汶川-映秀M_S8.0地震的地球物理场与动力过程
|
摘要
汶川-映秀M_S8.0大地震发生在当今构造、地震远不如相邻地带的龙门山断裂系上,震间和震后在地表形成了一条长300 km,宽近80 km,发生了70000多次余震的长廊地带,造成了严重的地表破坏和大量人员伤亡,而震前却未见到可视为与大地震发生与发展有因果关系的征兆现象,可是大地震就在这里发生了.多年的研究表明,这次M_S8.0大地震的发生乃是由于印度洋板块与欧亚板块碰撞、挤压,且东构造结向北"顶进"插入青藏高原东北缘力系作用下导致的该区构造、地震均强烈活动,在此背景下:(1)高原腹地壳、幔物质向东运移受阻、应力集中,深部物质重新分异、调整,物质与能量进行强烈交换;(2)震源深处介质属性与结构变异、破裂,且导致重力场的高度不均衡;(3)川西高原,相对低速壳、幔物质在坚硬的四川盆地壳、幔物质阻隔下,沿龙门山陡峭主断裂面相上逆冲,并在龙门山3条不同角度西倾断裂向下收敛处强烈碰撞;(4)震源深处汇聚断裂的形成构成了汶川-映秀M_S8.0大地震的发震断裂.
The Wenchuan-Yingxiu MS8.0 earthquake occurred along the Longmenshan fault system where the tectonic and seismic activities are relatively less inactive than its surroundings. After the great earthquake, a dynamic failure corridor zone was formed at the surface, which was about 300 km-long and 80 km-wide and more than 70000 aftershocks occurred. The earthquake caused serious surface damages and large numbers of casualties, but no confirmed precursor phenomena were reported. In the northeastern Tibetan Plateau, geophysicists had applied many kinds of geophysical methods, including the artificial seismic probing, the natural seismic imaging, the gravity probing, and the electric and magnetic methods. Many researchers believed that the crust or mantle shortening is the main dynamic of the MS8.0 Wenchuan-Yingxiu earthquake. However, the evidences were not enough, due to the disadvantage of the geophysical methods, such as the dubious resolution problem and the ambiguous interpretation from colorful results. Based on the previous results and our extensively study, we made a further study on the Wenchuan-Yingxiu MS8.0 earthquake which mainly concentrating on the three issues, including the highly isostatic equilibrium of the Longmenshan fault system, the fine structure and abrupt deep dynamics of the Longmenshan fault zone, and the force source system, the development and occurrence of the Wenchuan-Yingxiu MS8.0 great earthquake. First, we reviewed the gravity filed and response of the boundary in the northeastern margin of Tibetan Plateau. The free-space and Bouguer gravity anomaly were given. The distribution of the theoretical isostatic crustal thickness and the isostatic thickness difference were analyzed. Considering the topography and gravity field of eastern Tibetan Plateau, the Longmenshan zone was far from gravity isostasy. Second, the electrical structures and the S-wave velocity structures were reviewed. We reanalyzed the four artificial seismic sounding profiles. Third, we showed a diagram of the 15±5 km deep convergence and the columnar force source of the seismogenic fault. Fourth, we summarized the three flow locus of deep matter in the eastern margin of Tibetan Plateau. Meanwhile, a model about the Wenchuan-Yingxiu MS8.0 strong earthquake and deep material motion was proposed, illustrating the opposite motions of crust and upper mantle materials, and the strong collision between the crust of the Songpan-Gantze block and the Sichuan Basin. We believe that the Wenchuan-Yingxiu MS8.0 earthquake was caused by the collision and extrusion of the Indian plate and Eurasian plate which the east tectonic knot was extruding north under the Tibetan Plateau and the large force system intensified the tectonic and seismic activities in the east margin. In summary, we illustrated the processes as follows.(1) The crust and mantle material in the central Tibetan Plateau was blocked in the east which resulted a large-scale stress concentration and strong exchange of deep materials and energy. The variation of the crustal thickness between the northeastern Tibetan Plateau and the Sichuan Basin was large as 15–20 km.(2) The structures and properties of the material in the deep source mutated and leaded to a highly disequilibrium of gravity field.(3) Blocked by the hard crust of the Sichuan Basin, the low velocity crust and mantle materials beneath the western Sichuan Plateau thrusted upward along the steep fault plane of the Longmengshan fault and collided at the convergence spot of the three west-dipped fault planes.(4) The three surficial faults in the Longmenshan fault zone were not the seismogenic faults, but the convergence fault at the depth of 15±5 km. The convergence fault was a columnar focal volume, which had a radius of 5 km and a length of 300 km. The convergence of the fault planes in the deep focus induced the seismogenic fracture of the MS8.0 Wenchuan-Yingxiu earthquake.
The Wenchuan-Yingxiu MS8.0 earthquake occurred along the Longmenshan fault system where the tectonic and seismic activities are relatively less inactive than its surroundings. After the great earthquake, a dynamic failure corridor zone was formed at the surface, which was about 300 km-long and 80 km-wide and more than 70000 aftershocks occurred. The earthquake caused serious surface damages and large numbers of casualties, but no confirmed precursor phenomena were reported. In the northeastern Tibetan Plateau, geophysicists had applied many kinds of geophysical methods, including the artificial seismic probing, the natural seismic imaging, the gravity probing, and the electric and magnetic methods. Many researchers believed that the crust or mantle shortening is the main dynamic of the MS8.0 Wenchuan-Yingxiu earthquake. However, the evidences were not enough, due to the disadvantage of the geophysical methods, such as the dubious resolution problem and the ambiguous interpretation from colorful results. Based on the previous results and our extensively study, we made a further study on the Wenchuan-Yingxiu MS8.0 earthquake which mainly concentrating on the three issues, including the highly isostatic equilibrium of the Longmenshan fault system, the fine structure and abrupt deep dynamics of the Longmenshan fault zone, and the force source system, the development and occurrence of the Wenchuan-Yingxiu MS8.0 great earthquake. First, we reviewed the gravity filed and response of the boundary in the northeastern margin of Tibetan Plateau. The free-space and Bouguer gravity anomaly were given. The distribution of the theoretical isostatic crustal thickness and the isostatic thickness difference were analyzed. Considering the topography and gravity field of eastern Tibetan Plateau, the Longmenshan zone was far from gravity isostasy. Second, the electrical structures and the S-wave velocity structures were reviewed. We reanalyzed the four artificial seismic sounding profiles. Third, we showed a diagram of the 15±5 km deep convergence and the columnar force source of the seismogenic fault. Fourth, we summarized the three flow locus of deep matter in the eastern margin of Tibetan Plateau. Meanwhile, a model about the Wenchuan-Yingxiu MS8.0 strong earthquake and deep material motion was proposed, illustrating the opposite motions of crust and upper mantle materials, and the strong collision between the crust of the Songpan-Gantze block and the Sichuan Basin. We believe that the Wenchuan-Yingxiu MS8.0 earthquake was caused by the collision and extrusion of the Indian plate and Eurasian plate which the east tectonic knot was extruding north under the Tibetan Plateau and the large force system intensified the tectonic and seismic activities in the east margin. In summary, we illustrated the processes as follows.(1) The crust and mantle material in the central Tibetan Plateau was blocked in the east which resulted a large-scale stress concentration and strong exchange of deep materials and energy. The variation of the crustal thickness between the northeastern Tibetan Plateau and the Sichuan Basin was large as 15–20 km.(2) The structures and properties of the material in the deep source mutated and leaded to a highly disequilibrium of gravity field.(3) Blocked by the hard crust of the Sichuan Basin, the low velocity crust and mantle materials beneath the western Sichuan Plateau thrusted upward along the steep fault plane of the Longmengshan fault and collided at the convergence spot of the three west-dipped fault planes.(4) The three surficial faults in the Longmenshan fault zone were not the seismogenic faults, but the convergence fault at the depth of 15±5 km. The convergence fault was a columnar focal volume, which had a radius of 5 km and a length of 300 km. The convergence of the fault planes in the deep focus induced the seismogenic fracture of the MS8.0 Wenchuan-Yingxiu earthquake.
引文
1 Copley A,Dan M K.Models of crustal flow in the India-Asia collision zone.Geophys J Int,2007,169:683-698
2 Yang Z X,Waldhauser F,Chen Y T,et al.Double-difference relocation of earthquakes in central-western China,1992-1999.J Seismol,2005,9:241-264
3 Wen X Z,Zhang P Z,Du F,et al.The background of historical and modern seismic activities of the occurrence of the 2008 MS8.0 Wenchuan,Sichuan,earthquake(in Chinese).Chin J Geophys,2009,52:444-454[闻学泽,张培震,杜方,等.2008年汶川8.0级地震发生的历史与现今地震活动背景.地球物理学报,2009,52:444-454]
4 Hubbard J,Shaw J H,Klinger Y.Structural setting of the 2008 Mw 7.9 Wenchuan,China,earthquake.Bull Seismol Soc Am,2010,100:2713-2735
5 Zhang P Z.A review on active tectonics and deep crustal processes of the Western Sichuan region,eastern margin of the Tibetan Plateau.Tectonophysics,2013,584:7-22
6 Beaumont C,Jamieson R A,Mai H N,et al.Crustal channel flows:1.Numerical models with applications to the tectonics of the Himalayan-Tibetan orogen.J Geophys Res-Solid Earth,2004,109:1-29
7 Burchfiel B C,Royden L H,Hilst R D V D,et al.A geological and geophysical context for the Wenchuan earthquake of 12 May 2008,Sichuan,People’s Republic of China.GSA Today,2008,18:4-11
8 Richardson N J,Densmore A L,Seward D,et al.Extraordinary denudation in the Sichuan Basin:Insights from low-temperature thermochronology adjacent to the eastern margin of the Tibetan Plateau.J Geophys Res-Solid Earth,2008,113:1-23
9 Xu X W,Wen X Z,Ye J Q,et al.The MS8.0 Wenchuan earthquake surface reptures and its seismogenic structure(in Chinese).Seismol Geol,2008,30:597-629[徐锡伟,闻学泽,叶建青,等.汶川MS8.0地震地表破裂带及其发震构造.地震地质,2008,30:597-629]
10 Wang E C,Meng Q R.Mesozoic and Cenozoic tectonic evolution of the Longmenshan fault belt.Sci China Ser D-Earth Sci,2009,52:575-592[王二七,孟庆任.对龙门山中生代和新生代构造演化的讨论.中国科学D辑:地球科学,2008,38:1221-1233]
11 Zhang Y Q,Yang N,Shi W,et al.Neotectonics of eastern Tibet and its control on the Wenchuan earthquake(in Chinese).Acta Geol Sin,2008,82:1668-1678[张岳桥,杨农,施炜,等.青藏高原东缘新构造及其对汶川地震的控制作用.地质学报,2008,82:1668-1678]
12 Zhang P Z,Wen X Z,Xu X W,et al.Tectonic model of the great Wenchuan earthquake of May 12,2008,Sichuan,China(in Chinese).Chin Sci Bull,2009,54:944-953[张培震,闻学泽,徐锡伟,等.2008年汶川8.0级特大地震孕育和发生的多单元组合模式.科学通报,2009,54:944-953]
13 Zhang P Z,Xu X W,Wen X Z,et al.Slip rates and recurrence intervals of the Longmen Shan active fault zone and tectonic implications for the mechanism of the May 12 Wenchuan earthquake,2008,Sichuan,China(in Chinese).Chin J Geophys,2008,51:1066-1073[张培震,徐锡伟,闻学泽,等.2008年汶川8.0级地震发震断裂的滑动速率、复发周期和构造成因.地球物理学报,2008,51:1066-1073]
14 Chen L C,Ran Y K,Chen J,et al.Geological and geomorphic evidence for repeatedly occurring severe earthquakes on fronter-range fault of Longmenshan,China(in Chinese).Quat Sci,2009,29:472-483[陈立春,冉勇康,陈杰,等.龙门山前山断裂大地震原地重复发生的地质地貌证据.第四纪研究,2009,29:472-483]
15 Hubbard J,Shaw J H.Uplift of the Longmen Shan and Tibetan Plateau,and the 2008 Wenchuan(M=7.9)earthquake.Nature,2009,458:194-197
16 Li Y,Huang R Q,Zhou R J,et al.Geological background of Longmenshan seismic belt and surface ruptures in Wenchuan earthquake(in Chinese).J Eng Geol,2009,17:3-18[李勇,黄润秋,周荣军,等.龙门山地震带的地质背景与汶川地震的地表破裂.工程地质学报,2009,17:3-18]
17 Ma Y S,Long C X,Tan C X,et al.Co-seismic faults and geological hazards and incidence of active fault of Wenchuan MS8.0 earthquake,Sichuan,China.Acta Geol Sin,2009,83:713-723
18 Peng H,Ma X M,Jiang J J.Process analysis of in-situ strain during the MS8.0 Wenchuan earthquake-Data from the stress monitoring station at Shandan.Acta Geol Sin,2009,83:754-766
19 Zhou Y S,He C R.The rheological structures of crust and mechanics of high-angle reverse fault slip for Wenchuan MS8.0 earthquake(in Chinese).Chin J Geophys,2009,52:474-484[周永胜,何昌荣.汶川地震区的流变结构与发震高角度逆断层滑动的力学条件.地球物理学报,2009,52:474-484]
20 Li H B,Si J L,Pei J L,et al.Investigating the surface ruputre process of the Wenchuan earthquake(MS8.0)(in Chinese).Quat Sci,2010,30:677-698[李海兵,司家亮,裴军令,等.汶川地震(MS8.0)地表破裂过程探讨.第四纪研究,2010,30:677-698]
21 Deng Q D,Chen G H,Zhu A L.Discussion of rupture mechanisms on the seismogenic fault of the 2008 MS8.0 Wenchuan earthquake.Sci China Earth Sci,2011,54:1360-1377
22 Yan D P,Li S B,Cao W T,et al.Multi-layer detachment crustal structure in the Longmen Mountains:Evidences from neo-tectonic deformation and geophysical data(in Chinese).Earth Sci Front,2010,17:106-116[颜丹平,李书兵,曹文涛,等.龙门山多层分层拆离地壳结构:新构造变形与深部构造证据.地学前缘,2010,17:106-116]
23 Yin A.A special issue on the great 12 May 2008 Wenchuan earthquake(Mw 7.9):Observations and unanswered questions preface.Tectonophysics,2010,491:1-9
24 Zhang Z J,Yuan X H,Yun C,et al.Seismic signature of the collision between the east Tibetan escape flow and the Sichuan Basin.Earth Planet Sci Lett,2010,292:254-264
25 Fu B H,Shi P L,Wang P,et al.Geometry and kinematics of the 2008 Wenchuan earthquake surface ruptures around the Qushan Town of Beichuan County,Sichuan:Implications for mitigation of seismic and geologic disasters(in Chinese).Chin J Geophys,2009,52:485-495[付碧宏,时丕龙,王萍,等.2008年汶川地震断层北川段的几何学与运动学特征及地震地质灾害效应.地球物理学报,2009,52:485-495]
26 Wang Q,Yuan G.Rayleigh wave phase velocity tomography and strong earthquake activity on the southeastern front of the Tibetan Plateau.Sci China Earth Sci,2014,57:2532-2542
27 Teng J W,Bai D H,Yang H,et al.Deep processes and dynamic response associated with the Wenchuan MS8.0 earthquake of 2008(in Chinese).Chin J Geophys,2008,51:1385-1402[滕吉文,白登海,杨辉,等.2008汶川MS8.0地震发生的深层过程和动力学响应.地球物理学报,2008,51:1385-1402]
28 Wang Z,Wang X B,Huang R X,et al.Deep structure imaging of multi-geophysical parameters and seismogenesis in the Longmenshan fault zone(in Chinese).Chin J Geophys,2017,60:2068-2079[王志,王绪本,黄润秋,等.龙门山断裂带多参数深部结构成像与地震成因研究.地球物理学报,2017,60:2068-2079]
29 Wei W B,Unsworth M,Jones A,et al.Detection of widespread fluids in the Tibetan crust by magnetotelluric studies.Science,2001,292:716-718
30 Sun J,Jin G W,Bai D H,et al.Sounding of electrical structure of the crust and upper mantle along the eastern border of Qinghai-Tibet Plateau and its tectonic significance.Sci China Ser D-Earth Sci,2003,46:243-253[孙洁,晋光文,白登海,等.青藏高原东缘地壳、上地幔电性结构探测及其构造意义.中国科学D辑:地球科学,2003,33:173-180]
31 Clark M K,Royden L H.Topographic ooze:Building the eastern margin of Tibet by lower crustal flow.Geology,2000,28:703-706
32 Clark M K,Bush J W M,Royden L H.Dynamic topography produced by lower crustal flow against rheological strength heterogeneities bordering the Tibetan Plateau.Geophys J Roy Astron Soc,2005,162:575-590
33 Zhu S B,Shi Y L.Genetic algorithm-finite element inversion of drag forces exerted by the lower crust on the upper crust in the Sichuan-Yunnan area(in Chinese).Chin J Geophys,2004,47:232-239[朱守彪,石耀霖.用遗传有限单元法反演川滇下地壳流动对上地壳的拖曳作用.地球物理学报,2004,47:232-239]
34 Klemperer S L.Crustal flow in Tibet:Geophysical evidence for the physical state of Tibetan lithosphere,and inferred patterns of active flow.Geol Soc Lon Spec Publ,2006,268:265-308
35 Schoenbohm L M,Burchfiel B C,Liangzhong C.Propagation of surface uplift,lower crustal flow,and Cenozoic tectonics of the southeast margin of the Tibetan Plateau.Geology,2006,34:813-816
36 Royden L H.Coupling and decoupling of crust and mantle in convergent orogens:Implications for strain partitioning in the crust.JGeophys Res-Solid Earth,1996,101:17679-17705
37 Royden L H,Burchfiel B C,King R W,et al.Surface deformation and lower crustal flow in eastern Tibet.Science,1997,276:788-790
38 Zhao G Z,Chen X B,Wang L F,et al.Evidence of crustal‘channel flow’in the eastern margin of Tibetan Plateau from MT measurements.Chin Sci Bull,2008,53:1887-1893[赵国泽,陈小斌,王立凤,等.青藏高原东边缘地壳“管流”层的电磁探测证据.科学通报,2008,3:345-350]
39 Wang C Y,Lou H,LüZ Y,et al.S-wave crustal and upper mantle’s velocity structure in the eastern Tibetan Plateau-Deep environment of lower crustal flow.Sci China Ser D-Earth Sci,2008,51:263-274[王椿镛,楼海,吕智勇,等.青藏高原东部地壳上地幔S波速度结构-下地壳流的深部环境.中国科学D辑:地球科学,2008,38:22-32]
40 Zhu J S.The Wenchuan earthquake occurrence background in deep structure and dynamics of lithosphere(in Chinese).J Chengdu Univ Tech(Sci Tech Ver),2008,35:348-356[朱介寿.汶川地震的岩石圈深部结构与动力学背景.成都理工大学学报(自然科学版),2008,35:348-356]
41 Zhu J S,Wang X B,Yang Y H,et al.The crustal flow beneath the eastern margin of the Tibetan Plateau and its process of dynamics(in Chinese).Chin J Geophys,2017,60:2038-2057[朱介寿,王绪本,杨宜海,等.青藏高原东缘的地壳流及动力过程.地球物理学报,2017,60:2038-2057]
42 Jia S X,Liu B J,Xu Z F,et al.The crustal structures of the central Longmenshan along and its margins as related to the seismotectonics of the 2008 Wenchuan earthquake.Sci China Ser D-Earth Sci,2014,57:777-790[嘉世旭,刘保金,徐朝繁,等.龙门山中段及两侧地壳结构与汶川地震构造.中国科学:地球科学,2014,44:497-509]
43 Li J,Wang X B,Li D H,et al.Characteristics of the lithosphere physical structure in eastern margin of the Qinghai-Tibet Plateau and their deep tectonic implications(in Chinese).Chin J Geophys,2017,60:2500-2511[李军,王绪本,李大虎,等.青藏高原东缘岩石圈物性结构特征及深部构造涵义.地球物理学报,2017,60:2500-2511]
44 Chen Z,Burchfiel B C,Liu Y,et al.Global positioning system measurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation.J Geophys Res-Solid Earth,2000,105:16215-16227
45 Teng J W,Pi J L,Yang H,et al.Wenchuan-Yingxiu MS8.0 earthquake seismogenic faults and deep dynamic response(in Chinese).Chin J Geophys,2014,57:392-403[滕吉文,皮娇龙,杨辉,等.汶川-映秀MS8.0地震的发震断裂带和形成的深层动力学响应.地球物理学报,2014,57:392-403]
46 Teng J W,Yang H,Zhang H S,et al.Wenchuan MS8.0 earthquak,fine velocity structures lithoshpere and dynamical mechanism(in Chinese).Quat Sci,2010,30:637-651[滕吉文,杨辉,张洪双,等.汶川-映秀8.0级大地震的发生与岩石圈精细速度结构和动力机制.第四纪研究,2010,30:637-651]
47 Teng J W,Zhang Y Q,Yan Y F.Deep process of the rupture of strong earthquakes and exploration for the impending earthquake prediction(in Chinese).Chin J Geophys,2009,52:428-443[滕吉文,张永谦,闫雅芬.强烈地震震源破裂和深层过程与地震短临预测探索.地球物理学报,2009,52:428-443]
48 Zhang Y.Inversion of source rupture process(in Chinese).Doctor Dissertation.Beijing:Peking University,2008[张勇.震源破裂过程反演方法研究.博士学位论文.北京:北京大学,2008
49 Wang W M,Zhao L F,Li J,et al.Rupture process of the MS8.0 Wenchuan earthquake of Sichuan,China(in Chinese).Chin J Geophys,2008,51:1403-1410[王卫民,赵连锋,李娟,等.四川汶川8.0级地震震源过程.地球物理学报,2008,51:1403-1410]
50 He P C,Shen Z K.Rupture triggering process of Wenchuan earthquake seismogenic faults(in Chinese).Chin J Geophys,2014,57:3308-3317[贺鹏超,沈正康.汶川地震发震断层破裂触发过程.地球物理学报,2014,57:3308-3317]
51 Chen Q F,Hua C,Li L,et al.Viscoelastic simulation of deep tectonic deformation of the Longmenshan fault zone and its implication for strong earthquakes(in Chinese).Chin J Geophys,2015,58:4129-4137[陈棋福,华诚,李乐,等.龙门山断裂带深部构造变形的黏弹性模拟及其与强震活动的关联性探讨.地球物理学报,2015,58:4129-4137]
52 He F J,Liang C T,Yang Y H,et al.The crust structure of the unruptured segment between Wenchuan and Lushan earthquakes revealed by receiver functions(in Chinese).Chin J Geophys,2017,60:2130-2146[何富君,梁春涛,杨宜海,等.用接收函数方法研究汶川和芦山地震之间未破裂段的地壳结构.地球物理学报,2017,60:2130-2146]
53 Wang C Y,Li Y H,Lou H.Issues on crustal and upper-mantle structures associated with geodynamics in the northeastern Tibetan Plateau(in Chinese).Chin Sci Bull,2016,61:2239-2263[王椿镛,李永华,楼海.与青藏高原东北部地球动力学相关的深部构造问题.科学通报,2016,61:2239-2263]
54 Zhang X Y,Gao R,Bai Z M,et al.Crustal structure beneath the Longmenshan area in eastern Tibet:New constrains from reprocessing wide-angle seismic data of the Aba-Longmenshan-Suining profile(in Chinese).Chin J Geophys,2017,60:2200-2212[张新彦,高锐,白志明,等.阿坝-遂宁宽角地震剖面重建藏东缘龙门山地区地壳速度结构.地球物理学报,2017,60:2200-2212]
55 Chen X B,Wu Y Q,Du P S.The structural features of crustal velocity on both sides of Longmenshan tectonic belt(in Chinese).In:Research and Development of Deep Structure in Mainland China.Beijing:Geology Press,1988[陈学波,吴跃强,杜平山.龙门山构造带两侧地壳速度结构特征.见:中国大陆深部构造的研究与进展.北京:地质出版社,1988]
56 Li S L,Zhang X K,Zhang C K,et al.A preliminary study on the crustal velocity structure of Maqin-Lanzhou-Jingbian by means of deep seismic sounding profile(in Chinese).Chin J Geophys,2002,45:210-217[李松林,张先康,张成科,等.玛沁-兰州-靖边地震测深剖面地壳速度结构的初步研究.地球物理学报,2002,45:210-217]
57 Wang Y X,Mooney W D,Han G H.Crustal P-wave velocity structure from Altyn Tagh to Longmen mountains along the Taiwan-Altay geoscience transect(in Chinese).Chin J Geophys,2005,48:98-106[王有学,Mooney W D,韩果花,等.台湾-阿尔泰地学断面阿尔金-龙门山剖面的地壳纵波速度结构.地球物理学报,2005,48:98-106]
58 Zhou Y M,Zhang Y S,Shi Y M,et al.Three-dimensional crustal velocity structure in the northeastern margin of the Qinghai-Tibetan Plateau(in Chinese).Prog Geophys,2006,21:127-134[周民都,张元生,石雅鏐,等.青藏高原东北缘地壳三维速度结构.地球物理学进展,2006,21:127-134]
59 Jia S X,Zhang X K.Study on the crust phases of deep seismic sounding experiments and fine crust structures in the northeast margin of Tibetan Plateau(in Chinese).Chin J Geophys,2008,51:1431-1443[嘉世旭,张先康.青藏高原东北缘深地震测深震相研究与地壳细结构.地球物理学报,2008,51:1431-1443]
60 Guo W B,Jia S X,Duan Y H,et al.A study on the basement tectonic units in the northeast margin of Tibetan Plateau-The result of Maduo-Gonghe-Yabrai refraction profile(in Chinese).Chin J Geophys,2016,59:3627-3636[郭文斌,嘉世旭,段永红,等.青藏高原东北缘基底结构研究-玛多-共和-雅布赖剖面上地壳地震折射探测.地球物理学报,2016,59:3627-3636]
61 Lin J Y,Duan Y H.Upper crustal structure of Haiyuan tectonic zone and its surrounding areas(in Chinese).Acta Seismol Sin,2016,38:179-187[林吉焱,段永红.海原构造区及其周缘上部地壳结构研究.地震学报,2016,38:179-187]
62 Song W J,Zhu J S,Cheng X Q,et al.Deep crustal structure around the source area of the Wenchuan MS8.0 earthquake(in Chinese).Quat Sci,2010,30:670-676[宋文杰,朱介寿,程先琼,等.汶川MS8.0级地震震源区地壳深部结构研究.第四纪研究,2010,30:670-676]
63 Wang H Y,Gao R,Li Q S,et al.Deep seismic reflection profiling in the Songpan-west Qinling-Linxia basin of the Qinghai-Tibet Plateau:Data acquisition,data processing and preliminary interpretations(in Chinese).Chin J Geophys,2014,57:1451-1461[王海燕,高锐,李秋生,等.青藏高原松潘-西秦岭-临夏盆地深地震反射剖面-采集、处理与初步解释.地球物理学报,2014,57:1451-1461]
64 Liu Q Y,Hilst R D V D,Li Y,et al.Eastward expansion of the Tibetan Plateau by crustal flow and strain partitioning across faults.Nat Geosci,2014,7:361-365
65 Wang C Y,Flesch L M,Chang L J,et al.Evidence of active mantle flow beneath South China.Geophys Res Lett,2013,40:5137-5141
66 Chen J H,Liu Q Y,Li S C,et al.Crust and upper mantle S-wave velocity structure across Northeastern Tibetan Plateau and Ordos block(in Chinese).Chin J Geophys,2005,48:333-342[陈九辉,刘启元,李顺成,等.青藏高原东北缘-鄂尔多斯地块地壳上地幔S波速度结构.地球物理学报,2005,48:333-342]
67 Ding Z F,He Z Q,Sun W G,et al.3-D crust and upper mantle velocity structure in eastern Tibetan Plateau and its surrounding areas(in Chinese).Chin J Geophys,1999,42:197-205[丁志峰,何正勤,孙为国,等.青藏高原东部及其边缘地区的地壳上地幔三维速度结构.地球物理学报,1999,42:197-205]
68 Li Y H,Wu Q J,An Z H,et al.The Poisson ratio and crustal structure across the NE Tibetan Plateau determined from receiver functions(in Chinese).Chin J Geophys,2006,49:1359-1368[李永华,吴庆举,安张辉,等.青藏高原东北缘地壳S波速度结构与泊松比及其意义.地球物理学报,2006,49:1359-1368]
69 Liang C T,Song X D.A low velocity belt beneath northern and eastern Tibetan Plateau from Pn tomography.Geophys Res Lett,2006,33:121-132
70 Shen W S,Ritzwoller M H,Kang D,et al.A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion.Geophys J Int,2016,206:ggw175
71 Xu Y,Li Z,Huang R,et al.Seismic structure of the Longmen Shan region from S-wave tomography and its relationship with the Wenchuan MS8.0 earthquake on 12 May 2008,southwestern China.Geophys Res Lett,2010,37:211-228
72 Li S H,Wang Y B,Liang Z B,et al.Crustal structure in southeastern Gansu from regional seismic waveform inversion(in Chinese).Chin J Geophys,2012,55:1186-1197[李少华,王彦宾,梁子斌,等.甘肃东南部地壳速度结构的区域地震波形反演.地球物理学报,2012,55:1186-1197]
73 Wang C Y,Sandvol E,Zhu L,et al.Lateral variation of crustal structure in the Ordos block and surrounding regions,North China,and its tectonic implications.Earth Planet Sci Lett,2014,387:198-211
74 Yang Y J,Ritzwoller M H,Zheng Y,et al.A synoptic view of the distribution and connectivity of the mid-crustal low velocity zone beneath Tibet.J Geophys Res-Solid Earth,2012,117:B04303
75 Deng W Z,Chen J H,Guo B,et al.Fine velocity structure of the Longmenshan fault zone by double-difference tomography(in Chinese).Chin J Geophys,2014,57:1101-1110[邓文泽,陈九辉,郭飚,等.龙门山断裂带精细速度结构的双差层析成像研究.地球物理学报,2014,57:1101-1110]
76 Liu Q M,Zhao J M,Lu F,et al.Crustal structure of northeastern margin of the Tibetan Plateau by receiver function inversion.Sci China Earth Sci,2014,57:741-750[刘启民,赵俊猛,卢芳,等.用接收函数方法反演青藏高原东北缘地壳结构.中国科学:地球科学,2014,44:668-679]
77 Zhang Y,Cheng S Y,Zhao B K,et al.The feature of tectonics in the Tibet Plateau from new regional gravity signals(in Chinese).Chin JGeophys,2013,56:1369-1380[张燕,程顺有,赵炳坤,等.青藏高原构造结构特点:新重力异常成果的启示.地球物理学报,2013,56:1369-1380]
78 Li Y H,Pan J T,Wu Q J,et al.Crustal and uppermost mantle structure of SE Tibetan Plateau from Rayleigh-wave group-velocity measurements.Earthq Sci,2014,27:411-419
79 Yu D X,Li Y H,Wu Q J,et al.S-wave velocity structure of the northeastern Tibetan Plateau from joint inversion of Rayleigh wave phase and group velocities(in Chinese).Chin J Geophys,2014,57:800-811[余大新,李永华,吴庆举,等.利用Rayleigh波相速度和群速度联合反演青藏高原东北缘S波速度结构.地球物理学报,2014,57:800-811]
80 Deng Y F,Shen W S,Xu T,et al.Crustal layering in northeastern Tibet:A case study based on joint inversion of receiver functions and surface wave dispersion.Geophys J Int,2015,203:692-706
81 Pan J T,Li Y H,Wu Q J,et al.Phase velocity maps of Rayleigh waves in the southeast Tibetan Plateau(in Chinese).Chin J Geophys,2015,58:3993-4006[潘佳铁,李永华,吴庆举,等.青藏高原东南部地区瑞利波相速度层析成像.地球物理学报,2015,58:3993-4006]
82 Zhang H S,Gao R,Tian X B,et al.Crustal S-wave velocity beneath the northeastern Tibetan Plateau inferred from teleseismic P-wave receiver functions(in Chinese).Chin J Geophys,2015,58:3982-3992[张洪双,高锐,田小波,等.青藏高原东北缘地壳S波速度结构及其动力学含义-远震接收函数提供的证据.地球物理学报,2015,58:3982-3992]
83 Wang X B,Gao Y,Wang Z,et al.Research progress on deep geophysics and continental dynamics in Eastern Tibetan Plateau(in Chinese).Chin J Geophys,2017,60:2030-2037[王绪本,高原,王志,等.青藏高原东缘深部地球物理与大陆动力学研究进展.地球物理学报,2017,60:2030-2037]
84 Allam A A,Ben-Zion Y.Seismic velocity structures in the southern California plate-boundary environment from double-difference tomography.Geophys J Int,2012,190:1181-1196
85 Allen C R,Gillespie A R,Han Y,et al.Red River and associated faults,Yunnan Province,China:Quaternary geology,slip rates,and seismic hazard.Geol Soc Am Bull,1984,95:686-700
86 Pesicek J D,Thurber C H,Zhang H,et al.Teleseismic double-difference relocation of earthquakes along the Sumatra-Andaman subduction zone using a 3-D model.J Geophys Res-Solid Earth,2010,115:B10303
87 Waldhauser F,Ellsworth W L.A double-difference earthquake location algorithm:Method and application to the northern Hayward fault,California.Bull Seismol Soc Am,2000,90:1353-1368
88 Teng J W,Si X,Wang Q S,et al.Collation and stipulation of the core science problems and theoretical concept in the geoscience study on the Tibetan Plateau(in Chinese).Chin J Geophys,2015,58:103-124[滕吉文,司芗,王谦身,等.青藏高原地球科学研究中的核心问题与理念的厘定.地球物理学报,2015,58:103-124]
89 Hai L,Wang C Y,LüZ Y,et al.Deep tectonic setting of the 2008 Wenchuan MS8.0 earthquake in southwestern China―Joint analysis of teleseismic P-wave receiver functions and Bouguer gravity anomalies.Sci China Ser D-Earth Sci,2009,52:166-179[楼海,王椿镛,吕智勇,等.2008年汶川MS8.0级地震的深部构造环境-远震P波接收函数和布格重力异常的联合解释.中国科学D辑:地球科学,2008,38:1207-1220]
90 She Y W,Fu G Y,Wang Z H,et al.Vertical tectonic stress in eastern margin of Bayan Har block revealed by gravity and terrain data(in Chinese).Chin J Geophys,2017,60:2480-2492[佘雅文,付广裕,王灼华,等.重力与地形数据揭示的巴颜喀拉块体东缘垂向构造应力场.地球物理学报,2017,60:2480-2492]
91 Shen C Y,Li H,Sun S A,et al.Dynamic variations of gravity and the preparation process of the Wenchuan MS8.0 earthquake(in Chinese).Chin J Geophys,2009,52:2547-2557[申重阳,李辉,孙少安,等.重力场动态变化与汶川MS8.0地震孕育过程.地球物理学报,2009,52:2547-2557]
92 Wang Q S,Teng J W,Zhang Y Q,et al.The effect of crustal gravity isostasy and Wenchuan earthquake in Longmenshan faults and adjacent area(in Chinese).Chin J Geophys,2008,23:1664-1670[王谦身,滕吉文,张永谦,等.龙门山断裂系及邻区地壳重力均衡效应与汶川地震.地球物理学进展,2008,23:1664-1670]
93 Wang Q S,Teng J W,Zhang Y Q,et al.The crustal structure and gravity isostasy in the middle western Sichuan area(in Chinese).Chin JGeophys,2009,52:579-583[王谦身,滕吉文,张永谦,等.四川中西部地区地壳结构与重力均衡.地球物理学报,2009,52:579-583]
94 Zhang J S,Gao R,Zeng L S,et al.Relationship between characteristics of gravity and magnetic anomalies and the earthquakes in Longmenshan range and adjacent areas(in Chinese).Chin J Geophys,2009,52:572-578[张季生,高锐,曾令森,等.龙门山及邻区重、磁异常特征及与地震关系的研究.地球物理学报,2009,52:572-578]
95 Zhang J S,Gao R,Li Q S,et al.A study on geophysical characteristic and basement in the Songpan-Garze and Western Qinling Orogenic Belt(in Chinese).Geol Rev,2007,53:261-266[张季生,高锐,李秋生,等.松潘-甘孜和西秦岭造山带地球物理特征及基底构造研究.地质论评,2007,53:261-266]
96 Zhang Y Q,Wang Q S,Teng J W.The crustal isostatic anomaly beneath eastern Tibet and western Sichuan and its relationship with the distribution of earthquakes(in Chinese).Chin J Geophys,2010,53:2631-2638[张永谦,王谦身,滕吉文.川西藏东地区的地壳均衡异常及其与地震分布的关系.地球物理学报,2010,53:2631-2638]
97 Zhu Y Q,Liu F,Li T M,et al.Dynamic variation of the gravity field in the Sichuan-Yunnan region and its implication for seismic risk(in Chinese).Chin J Geophys,2015,58:4187-4196[祝意青,刘芳,李铁明,等.川滇地区重力场动态变化及其强震危险含义.地球物理学报,2015,58:4187-4196]
98 Bi B T,Hu X Y,Li L Q,et al.Multi-scale analysis to the gravity field of the northeastern Tibetan Plateau and its geodynamic implications(in Chinese).Chin J Geophys,2016,59:543-555[毕奔腾,胡祥云,李丽清,等.青藏高原东北部多尺度重力场及其地球动力学意义.地球物理学报,2016,59:543-555]
99 Meng X H,Shi L,Guo L H,et al.Multi-scale analyses of transverse structures based on gravity anomalies in the northeastern margin of the Tibetan Plateau(in Chinese).Chin J Geophys,2012,55:3933-3941[孟小红,石磊,郭良辉,等.青藏高原东北缘重力异常多尺度横向构造分析.地球物理学报,2012,55:3933-3941]
100 Zhang S M,Xie F R,Huang Z X,et al.Bending and thrusting of the upper crust in Longmenshan area and its deep dynamics(in Chinese).Quat Sci,2009,29:449-463[张世民,谢富仁,黄忠贤,等.龙门山地区上地壳的拱曲冲断作用及其深部动力学机制探讨.第四纪研究,2009,29:449-463]
101 Zhang Y Q,Wang Q S,Teng J W.Crustal isotatic state in western Sichuan and its dynamical mechanism(in Chinese).Quat Sci,2010,30:662-669[张永谦,王谦身,滕吉文.川西地区的地壳均衡状态及其动力学机制.第四纪研究,2010,30:662-669]
102 Li Y.Contiental Dynamic Process and Gelogical Response of the Eastern Margin of Tibetan Plateau(in Chinese).Beijing:Geological Press,2006[李勇.青藏高原东缘大陆动力学过程与地质响应.北京:地质出版社,2006]
103 Bai D H,Unsworth M J,Meju M A,et al.Crustal deformation of the eastern Tibetan Plateau revealed by magnetotelluric imaging.Nat Geosci,2010,3:358-362
104 Unsworth M J,Meju M A.Crustal deformation of the eastern Tibetan Plateau revealed by magnetotelluric imaging.Nat Geosci,2011,3:358-362
105 Zhao B,Shi Y,Gao Y.Seismic relocation,focal mechanism and crustal seismic anisotropy associated with the 2010 Yushu MS7.1earthquake and its aftershocks.Acta Seismol Sin,2012,25:111-119
106 Chen Y Z,Tang J,Cai J T,et al.Deep electrical structure beneath the Sichuan-Yunnan area in the eastern margin of the Tibetan Plateau(in Chinese).Chin J Geophys,2017,60:2425-2441[程远志,汤吉,蔡军涛,等.青藏高原东缘川滇构造区深部电性结构特征.地球物理学报,2017,60:2425-2441]
107 Chen Y Z,Tang J,Chen X B,et al.Electrical structure and seismogenic environment along the border region of Yunnan,Sichuan and Guizhou in the south of the North-South seismic belt(in Chinese).Chin J Geophys,2015,58:3965-3981[程远志,汤吉,陈小斌,等.南北地震带南段川滇黔接壤区电性结构特征和孕震环境.地球物理学报,2015,58:3965-3981]
108 Wang L F,Zhao G Z,Zhan Y,et al.Electric structure of crust beneath the southwestern segment of the Longmenshan fault zone(in Chinese).Seismol Geol,2014,36:302-311[王立凤,赵国泽,詹艳,等.龙门山断裂带西南端地壳电性结构.地震地质,2014,36:302-311]
109 Wang X B,Luo W,Zhang G,et al.Electrical resistivity structure of Longmenshan crust-mantle under sector boundary(in Chinese).Chin J Geophys,2013,56:2718-2727[王绪本,罗威,张刚,等.扇形边界条件下的龙门山壳、幔电性结构特征.地球物理学报,2013,56:2718-2727]
110 Wang X B,Yu N,Gao S,et al.Research progress in research on electrical structure of crust and upper mantle beneath the eastern margin of the Tibetan Plateau(in Chinese).Chin J Geophys,2017,60:2350-2370[王绪本,余年,高嵩,等.青藏高原东缘地壳上地幔电性结构研究进展.地球物理学报,2017,60:2350-2370]
111 Zhang L T,Jin S,Wei W B,et al.Electrical structure of crust and upper mantle beneath the eastern margin of the Tibetan Plateau and the Sichuan basin(in Chinese).Chin J Geophys,2012,55:4126-4137[张乐天,金胜,魏文博,等.青藏高原东缘及四川盆地的壳、幔导电性结构研究.地球物理学报,2012,55:4126-4137]
112 Bai D H,Teng J W,Ma X B,et al.Crustal flow beneath eastern Tibetan Plateau revealed by magnetotelluric measurements(in Chinese).Chin Basic Sci,2011,13:7-10[白登海,滕吉文,马晓冰,等.大地电磁观测揭示青藏高原东部存在两条地壳物质流.中国基础科学,2011,13:7-10]
113 Min G,Wang X B,Xia S B,et al.Electrical structure of middle and upper crust beneath the Minshan uplift zone and central section of the West Qinling orogenic zone(in Chinese).Chin J Geophys,2017,60:2397-2413[闵刚,王绪本,夏时斌,等.岷山隆起带与西秦岭构造带中段中上地壳电性结构特征.地球物理学报,2017,60:2397-2413]
114 Zhan Y,Yang H,Zhao G Z,et al.Deep electrical structure of crust beneath the Madongshan step area at the Haiyuan fault in the northeastern margin of the Tibetan Plateau and tectonic implications(in Chinese).Chin J Geophys,2017,60:2371-2384[詹艳,杨皓,赵国泽,等.青藏高原东北缘海原构造带马东山阶区深部电性结构特征及其构造意义.地球物理学报,2017,60:2371-2384]
115 Yan Y F,Teng J W,Ruan X M,et al.Aeromagnetic field characteristics and the Wenchuan earthquakes in the Longmenshan mountains and adjacent areas(in Chinese).Chin J Geophys,2016,59:197-214[闫亚芬,滕吉文,阮小敏,等.龙门山和相邻地域航磁场特征与汶川大地震.地球物理学报,2016,59:197-214]
116 Hu Y P,Wang Z,Liu G N,et al.Crustal structure imaging of multi-geophysical parameters and generating mechanisms of large earthquakes in North-South Seismic Zone(in Chinese).Chin J Geophys,2017,60:2113-2129[胡亚平,王志,刘冠男,等.南北地震带地壳结构多参数成像及强震触发机制研究.地球物理学报,2017,60:2113-2129]
117 Wang C Y,Chang L J,LüZ Y,et al.Seismic anisotropy of upper mantle in eastern Tibetan Plateau and related crust-mantle coupling pattern.Sci China Ser D-Earth Sci,2007,50:1150-1160[王椿镛,常利军,吕智勇,等.青藏高原东部上地幔各向异性及相关的壳、幔耦合型式.中国科学D辑:地球科学,2007,37:495-503]
118 Zhao P P,Chen J H,Campillo M,et al.Crustal velocity changes associated with the Wenchuan M8.0 earthquake by auto-correlation function analysis of seismic ambient noise(in Chinese).Chin J Geophys,2012,55:137-145[赵盼盼,陈九辉,Campillo M,等.汶川地震区地壳速度相对变化的环境噪声自相关研究.地球物理学报,2012,55:137-145]
119 Zhao P P,Chen J H,Liu Q Y,et al.Fine structure of middle and upper crust of the Longmenshan Fault zone from short period seismic ambient noise(in Chinese).Chin J Geophys,2015,58:4018-4030[赵盼盼,陈九辉,刘启元,等.龙门山断裂带中上地壳速度结构的短周期环境噪声成像.地球物理学报,2015,58:4018-4030]
120 Gouédard P,Yao H,Ernst F,et al.Surface wave eikonal tomography in heterogeneous media using exploration data.Geophys J Int,2012,191:781-788
121 Lin F C,Ritzwoller M H.Helmholtz surface wave tomography for isotropic and azimuthally anisotropic structure.Geophys J Int,2011,186:1104-1120
122 Lin F C,Ritzwoller M H,Snieder R.Eikonal tomography:Surface wave tomography by phase front tracking across a regional broad-band seismic array.Geophys J Roy Astron Soc,2010,177:1091-1110
123 Zhu J S,Zhao J M,Jiang X T,et al.Crustal flow beneath the eastern margin of the Tibetan Plateau.Earthq Sci,2012,25:469-483
124 Jin G,Gaherty J B.Surface wave phase-velocity tomography based on multichannel cross-correlation.Geophys J Int,2015,201:1383-1398
125 Zhong S J,Wu J P,Fang L H,et al.Surface wave eikonal tomography in and around the northeastern margin of the Tibetan Plateau(in Chinese).Chin J Geophys,2017,60:2304-2314[钟世军,吴建平,房立华,等.青藏高原东北缘及周边地区基于程函方程的面波层析成像.地球物理学报,2017,60:2304-2314]
126 Lei J S,Zhao D P.Structural heterogeneity of the Longmenshan fault zone and the mechanism of the 2008 Wenchuan earthquake(MS8.0).Geochem Geophys Geosyst,2009,10:1-17
127 Zheng T Y,Zhao L,Zhu R X.New evidence from seismic imaging for subduction during assembly of the North China Craton:REPLY.Geology,2010,38:395-398
128 Huang Z X,Li H Y,Xu Y.Lithospheric S-wave velocity structure of the North-South Seismic Belt of China from surface wave tomography(in Chinese).Chin J Geophys,2013,56:1121-1131[黄忠贤,李红谊,胥颐.南北地震带岩石圈S波速度结构面波层析成像.地球物理学报,2013,56:1121-1131]
129 Lei J S,Zhao D P,Su J R,et al.Fine seismic structure under the Longmenshan fault zone and the mechanism of the large Wenchuan earthquake(in Chinese).Chin J Geophys,2009,52:339-345[雷建设,赵大鹏,苏金蓉,等.龙门山断裂带地壳精细结构与汶川地震发震机理.地球物理学报,2009,52:339-345]
130 Liu Q Y,Li Y,Chen J H,et al.Wenchuan MS8.0 earthquake:Preliminary study of the S-wave velocity structure of the crust and upper mantle(in Chinese).Chin J Geophys,2009,52:309-319[刘启元,李昱,陈九辉,等.汶川MS8.0地震:地壳上地幔S波速度结构的初步研究.地球物理学报,2009,52:309-319]
131 Wang C Y,Yang W C,Wu J P,et al.Study on the lithospheric structure and earthquakes in North-South Tectonic Belt(in Chinese).Chin JGeophys,2015,58:3867-3901[王椿镛,杨文采,吴建平,等.南北构造带岩石圈结构与地震的研究.地球物理学报,2015,58:3867-3901]
132 Xu X M,Ding Z F,Zhang F X.The teleseismic tomography study by P-wave traveltime data beneath the southern South-north Seismic Zone(in Chinese).Chin J Geophys,2015,58:4041-4051[徐小明,丁志峰,张风雪.南北地震带南段远震P波走时层析成像研究.地球物理学报,2015,58:4041-4051]
133 He M X,Fang H,Wang X B,et al.Deep conductivity characteristics of the southern Xianshuihe fault zone(in Chinese).Chin J Geophys,2017,60:2414-2424[何梅兴,方慧,王绪本,等.鲜水河断裂带南段深部电性结构特征研究.地球物理学报,2017,60:2414-2424]
134 Wang C Y,Han W B,Wu J P,et al.Crustal structure beneath the eastern margin of the Tibetan Plateau and its tectonic implications.JGeophys Res-Solid Earth,2007,112:1-21
135 Yang H,Teng J W,Pi J L.Numerical simulation of the geodynamical condition about the channel flow model in Tibetan Plateau(in Chinese).Chin J Geophys,2013,56:2625-2635[杨辉,滕吉文,皮娇龙.青藏高原通道流模型动力环境的数值模拟.地球物理学报,2013,56:2625-2635]
136 Pi J L,Teng J W,Yang H.Geodynamic response of Moho relief modes to the channel flow below the Tibetan Plateau:Numerical simulation(in Chinese).Chin J Geophys,2014,57:2766-2776[皮娇龙,滕吉文,杨辉.青藏高原Moho界面起伏样式对通道流模型的动力学响应-基于数值模拟.地球物理学报,2014,57:2766-2776]
137 Jia S X,Lin J Y,Guo W B,et al.Investigation on diversity of crustal structures beneath the Bayan Har block(in Chinese).Chin J Geophys,2017,60:2226-2238[嘉世旭,林吉焱,郭文斌,等.巴颜喀拉块体地壳结构多样性探测.地球物理学报,2017,60:2226-2238]
138 Chen Y T.On the magnitude and the fault length of the great Wenchuan earthquake(in Chinese).Sci Tech Rev,2008,26:26-27[陈运泰.汶川特大地震的震级和断层长度.科技导报,2008,26:26-27]
139 Wu J P,Huang Y,Zhang T Z,et al.Aftershock distribution of the MS8.0 Wenchuan earthquake and three dimensional P-wave velocity structure in and around source region(in Chinese).Chin J Geophys,2009,52:320-328[吴建平,黄媛,张天中,等.汶川MS8.0级地震余震分布及周边区域P波三维速度结构研究.地球物理学报,2009,52:320-328]
140 Zhu A L,Xu X W,Diao G L,et al.Relocation of the MS8.0 Wenchuan earthquake sequence in part:Preliminary seismotectonic analysis(in Chinese).Seismol Geol,2008,30:759-767[朱艾斓,徐锡伟,刁桂苓,等.汶川MS8.0地震部分余震重新定位及地震构造初步分析.地震地质,2008,30:759-767]
141 Bai Y Z,Xu X W,Xu J,et al.A research on the distribution of deformation fields near the fault of 2008 Wenchuan earthquake(in Chinese).Chin J Geophys,2011,54:1798-1804[白玉柱,徐锡伟,徐杰,等.2008年汶川地震近断裂区域变形场的空间分布.地球物理学报,2011,54:1798-1804]
142 Guo X Y,Gao R,Keller G R,et al.Discussion on the mountain building process of the Longmenshan range(in Chinese).Chin J Geol,2014,49:1337-1345[郭晓玉,高锐,Keller G R,等.龙门山断裂带隆起造山独特性探讨.地质科学,2014,49:1337-1345]
143 Yang H,Teng J W,Wang Q S,et al.Numerical simulation on the special gravity fields and dynamic response in Longmenshan orogenic belt and adjacent area(in Chinese).Chin J Geophys,2013,56:106-116[杨辉,滕吉文,王谦身,等.龙门山造山带及邻区重力场特征与动力学响应数值模拟.地球物理学报,2013,56:106-116]
144 Royden L H,Burchfiel B C,Rd V D H.The geological evolution of the Tibetan Plateau.Science,2008,321:1054-1058
145 Chen G G,Ji F J,Zhou R J,et al.Primary research of activity segmentation of Longmenshan Fault zone since late-Quaternary(in Chinese).Seimol Geol,2007,29:657-673[陈国光,计凤桔,周荣军,等.龙门山断裂带晚第四纪活动性分段的初步研究.地震地质,2007,29:657-673]
146 Li H B,Si J L,Fu X F,et al.Co-seismic rupture and maximum displacement of the 2008 Wenchuan earthquake and its tectonic implications(in Chinese).Quat Sci,2009,29:387-402[李海兵,司家亮,付小方,等.2008年汶川地震同震滑移特征、最大滑移量及构造意义.第四纪研究,2009,29:387-402]
147 Wang H,Li H B,Pei J L,et al.Structural and lithologic characteristics of the Wenchuan earthquake fault zone and its relationship with the sesimic activities(in Chinese).Quat Sci,2010,30:768-778[王焕,李海兵,裴军令,等.汶川地震断裂带结构、岩性特征及其与地震活动的关系.第四纪研究,2010,30:768-778]
148 Xu J,Gao X L,Zhou B G,et al.The seismogenic structure of the 2008 Wenchuan MS8.0 earthquake:A newly generated deep fault in crust along the Longmen Mountains fault zone in the shallow subsurface(in Chinese).Earth Sci Front,2010,17:117-127[徐杰,高祥林,周本刚,等.2008年汶川8.0级地震的发震构造:沿龙门山断裂带新生的地壳深部断裂.地学前缘,2010,17:117-127]
149 Wang C Y,Flesch L M,Silver P G,et al.Evidence for mechanically coupled lithosphere in central Asia and resulting implications.Geology,2008,36:363-366
150 Shan J X,Song X G,Han Y F,et al.The characteristics of surface vertical deformation before the Wenchuan MS8.0 earthquake from In SAR(in Chinese).Chin J Geophys,2009,52:2739-2745[单新建,宋小刚,韩宇飞,等.汶川MS8.0地震前In SAR垂直形变场变化特征研究.地球物理学报,2009,52:2739-2745]
151 Shan J X,Zhang G H,Wang C S,et al.Joint inversion for the spatial fault slip distribution of the 2015 Nepal Mw 7.9 earthquake based on In SAR and GPS observations(in Chinese).Chin J Geophys,2015,58:4266-4276[单新建,张国宏,汪驰升,等.基于In SAR和GPS观测数据的尼泊尔地震发震断层特征参数联合反演研究.地球物理学报,2015,58:4266-4276]
152 Li Y H,Wang Q L,Cui D X,et al.Inversion of present-day fault slip,rate along Altyn Tagh Fault constrained by GPS data(in Chinese).Seismol Geol,2015,37:869-879[李煜航,王庆良,崔笃信,等.利用GPS数据反演阿尔金断裂现今滑动速率.地震地质,2015,37:869-879]
153 Liu X,Sun D Y,Ma J,et al.Present-day deformation and stress state of Longmenshan fault from GPS results-Comparative research on active faults in Sichuan-Yunnan region(in Chinese).Chin J Geophys,2014,57:1091-1100[刘峡,孙东颖,马瑾,等.GPS结果揭示的龙门山断裂带现今形变与受力-与川滇地区其他断裂带的对比研究.地球物理学报,2014,57:1091-1100]
154 Xu Z Q,Li H B,Wu Z L.Wenchuan earthquake and scientific drilling(in Chinese).Acta Geol Sin,2008,82:1613-1622[许志琴,李海兵,吴忠良.汶川地震和科学钻探.地质学报,2008,82:1613-1622]
155 Zhang P Z,Wang Q,Ma Z J.GPS velocity field and active crustal blocks of contemporary tectonic deformation in continental China(in Chinese).Earth Sci Front,2002,9:430-441[张培震,王琪,马宗晋.中国大陆现今构造运动的GPS速度场与活动地块.地学前缘,2002,9:430-441]
156 Xiao Z H,Xu C J,Jiang G Y,et al.Crustal strain in the Longmenshan region considering fault locking during ten years before the 2008Wenchuan earthquake(in Chinese).Chin J Geophys,2017,60:953-961[肖卓辉,许才军,江国焰,等.汶川地震前十年间龙门山区域顾及断层闭锁的地壳应变场.地球物理学报,2017,60:953-961]
157 Zhang Z J,Wang Y H,Chen Y,et al.Crustal structure across Longmenshan fault belt from passive source seismic profiling.Geophys Res Lett,2009,36:1397-1413
158 Zhang Y Q,Li H L.Late Quaternary active faulting along the SW segment of the Longmenshan Fault(in Chinese).Quat Sci,2010,30:699-710[张岳桥,李海龙.龙门山断裂带西南段晚第四纪活动性调查与分析.第四纪研究,2010,30:699-710]
159 Zhang Z Q,Zhang P Z,Wang Q L.The structure and seismogenic mechanism of Longmenshan high dip-angle reverse fault(in Chinese).Chin JGeophys,2010,53:2068-2082[张竹琪,张培震,王庆良.龙门山高倾角逆断层结构与孕震机制.地球物理学报,2010,53:2068-2082]
160 Tan K,Yang S M,Qiao X J,et al.Rupture of ramp-décollement faults in the 2008 Wenchuan earthquake-Geodetic evidence for the uplift of the Longmenshan driven by convergent deformation(in Chinese).Chin J Geophys,2013,56:1506-1516[谭凯,杨少敏,乔学军,等.2008年汶川地震中断坡-滑脱断层破裂:龙门山挤压隆升的大地测量证据.地球物理学报,2013,56:1506-1516]
161 Yang Y H,Chen Q,Liu G X,et al.Correction of coseismic deformation field associated with Wenchuan earthquake with GPS observables and In SAR adjacent track smoothing and fault slip inversion(in Chinese).Chin J Geophys,2014,57:1462-1476[杨莹辉,陈强,刘国祥,等.汶川地震同震形变场的GPS和In SAR邻轨平滑校正与断层滑移精化反演.地球物理学报,2014,57:1462-1476]
162 Liu Q X,Zhu J S,Cao J X,et al.Relocation of the Wenchuan MS8.0 earthquake sequence and its aftershocks and their spatial distribution characteristics(in Chinese).Quat Sci,2010,30:736-744[刘巧霞,朱介寿,曹俊兴,等.汶川MS8.0级地震余震重新定位及其空间分布特征研究.第四纪研究,2010,30:736-744]
163 Teng J W,Song P H,Zhang X M,et al.The driving force and movement of materials in the Earth’s interior(in Chinese).Chin Sci Bull,2016,61:1995-2019[滕吉文,宋鹏汉,张雪梅,等.地球内部物质的运动与动力.科学通报,2016,61:1995-2019]
164 Wang X C,Ding Z F,Wu Y,et al.Crustal thicknesses and Poisson’s ratios beneath the northern section of the North-South Seismic belt and surrounding areas in China(in Chinese).Chin J Geophys,2017,60:2080-2090[王兴臣,丁志峰,武岩,等.中国南北地震带北段及其周缘地壳厚度与泊松比研究.地球物理学报,2017,60:2080-2090]
165 Yue H,Lay T,Rivera L,et al.Rupture process of the 2010 Mw 7.8 Mentawai tsunami earthquake from joint inversion of nearfield GPSand teleseismic body wave recordings constrained by tsunami observations.J Geophys Res-Solid Earth,2015,119:5574-5593
166 Deng Q D,Cheng S P,Ma J,et al.Seismic activities and earthquake potential in the Tibetan Plateau(in Chinese).Chin J Geophys,2014,57:2025-2042[邓起东,程绍平,马冀,等.青藏高原地震活动特征及当前地震活动形势.地球物理学报,2014,57:2025-2042]
167 Ding L.Nepal earthquake leads the south extrustion of Himalyayas(in Chinese).Chin Nat Geogr,2015,8:156-163[丁林.尼泊尔大地震令喜马拉雅山向南摊开.中国国家地理,2015,8:156-163]
168 Teng J W.Ponder and research on the genesis and occurrence of strong earthquakes and the prediction of their place,time and intensity(in Chinese).Chin J Geophys,2010,53:1749-1766[滕吉文.强烈地震孕育与发生的地点、时间及强度预测的思考与探讨.地球物理学报,2010,53:1749-1766]
169 Teng J W,Ma X Y,Zhang X M,et al.Deep processes and dynamic responses of the generation and occurrence of the 2015 Nepal MS8.1earthquake(in Chinese).Chin J Geophys,2017,60:123-141[滕吉文,马学英,张雪梅,等.2015年尼泊尔MS8.1大地震孕育的深层过程与发生的动力学响应.地球物理学报,2017,60:123-141]
170 Teng J W,Ruan X M,Zhang Y Q,et al.The stratificational velocity structure of crust and covering strata of upper mantle and the orbit of deep interaquifer substance locus of movement for Tibetan Plateau(in Chinese).Chin J Geophys,2012,28:4077-4100[滕吉文,阮小敏,张永谦,等.青藏高原地壳与上地幔成层速度结构与深部层间物质的运移轨迹.岩石学报,2012,28:4077-4100]
171 Teng J W,Wang Q S,Wang G J,et al.Specific gravity field and deep crustal structure of the“Himalayas east structural knot”(in Chinese).Chin J Geophys,2006,49:1045-1052[滕吉文,王谦身,王光杰,等.喜马拉雅“东构造结”地区的特异重力场与深部地壳结构.地球物理学报,2006,49:1045-1052]
2 Yang Z X,Waldhauser F,Chen Y T,et al.Double-difference relocation of earthquakes in central-western China,1992-1999.J Seismol,2005,9:241-264
3 Wen X Z,Zhang P Z,Du F,et al.The background of historical and modern seismic activities of the occurrence of the 2008 MS8.0 Wenchuan,Sichuan,earthquake(in Chinese).Chin J Geophys,2009,52:444-454[闻学泽,张培震,杜方,等.2008年汶川8.0级地震发生的历史与现今地震活动背景.地球物理学报,2009,52:444-454]
4 Hubbard J,Shaw J H,Klinger Y.Structural setting of the 2008 Mw 7.9 Wenchuan,China,earthquake.Bull Seismol Soc Am,2010,100:2713-2735
5 Zhang P Z.A review on active tectonics and deep crustal processes of the Western Sichuan region,eastern margin of the Tibetan Plateau.Tectonophysics,2013,584:7-22
6 Beaumont C,Jamieson R A,Mai H N,et al.Crustal channel flows:1.Numerical models with applications to the tectonics of the Himalayan-Tibetan orogen.J Geophys Res-Solid Earth,2004,109:1-29
7 Burchfiel B C,Royden L H,Hilst R D V D,et al.A geological and geophysical context for the Wenchuan earthquake of 12 May 2008,Sichuan,People’s Republic of China.GSA Today,2008,18:4-11
8 Richardson N J,Densmore A L,Seward D,et al.Extraordinary denudation in the Sichuan Basin:Insights from low-temperature thermochronology adjacent to the eastern margin of the Tibetan Plateau.J Geophys Res-Solid Earth,2008,113:1-23
9 Xu X W,Wen X Z,Ye J Q,et al.The MS8.0 Wenchuan earthquake surface reptures and its seismogenic structure(in Chinese).Seismol Geol,2008,30:597-629[徐锡伟,闻学泽,叶建青,等.汶川MS8.0地震地表破裂带及其发震构造.地震地质,2008,30:597-629]
10 Wang E C,Meng Q R.Mesozoic and Cenozoic tectonic evolution of the Longmenshan fault belt.Sci China Ser D-Earth Sci,2009,52:575-592[王二七,孟庆任.对龙门山中生代和新生代构造演化的讨论.中国科学D辑:地球科学,2008,38:1221-1233]
11 Zhang Y Q,Yang N,Shi W,et al.Neotectonics of eastern Tibet and its control on the Wenchuan earthquake(in Chinese).Acta Geol Sin,2008,82:1668-1678[张岳桥,杨农,施炜,等.青藏高原东缘新构造及其对汶川地震的控制作用.地质学报,2008,82:1668-1678]
12 Zhang P Z,Wen X Z,Xu X W,et al.Tectonic model of the great Wenchuan earthquake of May 12,2008,Sichuan,China(in Chinese).Chin Sci Bull,2009,54:944-953[张培震,闻学泽,徐锡伟,等.2008年汶川8.0级特大地震孕育和发生的多单元组合模式.科学通报,2009,54:944-953]
13 Zhang P Z,Xu X W,Wen X Z,et al.Slip rates and recurrence intervals of the Longmen Shan active fault zone and tectonic implications for the mechanism of the May 12 Wenchuan earthquake,2008,Sichuan,China(in Chinese).Chin J Geophys,2008,51:1066-1073[张培震,徐锡伟,闻学泽,等.2008年汶川8.0级地震发震断裂的滑动速率、复发周期和构造成因.地球物理学报,2008,51:1066-1073]
14 Chen L C,Ran Y K,Chen J,et al.Geological and geomorphic evidence for repeatedly occurring severe earthquakes on fronter-range fault of Longmenshan,China(in Chinese).Quat Sci,2009,29:472-483[陈立春,冉勇康,陈杰,等.龙门山前山断裂大地震原地重复发生的地质地貌证据.第四纪研究,2009,29:472-483]
15 Hubbard J,Shaw J H.Uplift of the Longmen Shan and Tibetan Plateau,and the 2008 Wenchuan(M=7.9)earthquake.Nature,2009,458:194-197
16 Li Y,Huang R Q,Zhou R J,et al.Geological background of Longmenshan seismic belt and surface ruptures in Wenchuan earthquake(in Chinese).J Eng Geol,2009,17:3-18[李勇,黄润秋,周荣军,等.龙门山地震带的地质背景与汶川地震的地表破裂.工程地质学报,2009,17:3-18]
17 Ma Y S,Long C X,Tan C X,et al.Co-seismic faults and geological hazards and incidence of active fault of Wenchuan MS8.0 earthquake,Sichuan,China.Acta Geol Sin,2009,83:713-723
18 Peng H,Ma X M,Jiang J J.Process analysis of in-situ strain during the MS8.0 Wenchuan earthquake-Data from the stress monitoring station at Shandan.Acta Geol Sin,2009,83:754-766
19 Zhou Y S,He C R.The rheological structures of crust and mechanics of high-angle reverse fault slip for Wenchuan MS8.0 earthquake(in Chinese).Chin J Geophys,2009,52:474-484[周永胜,何昌荣.汶川地震区的流变结构与发震高角度逆断层滑动的力学条件.地球物理学报,2009,52:474-484]
20 Li H B,Si J L,Pei J L,et al.Investigating the surface ruputre process of the Wenchuan earthquake(MS8.0)(in Chinese).Quat Sci,2010,30:677-698[李海兵,司家亮,裴军令,等.汶川地震(MS8.0)地表破裂过程探讨.第四纪研究,2010,30:677-698]
21 Deng Q D,Chen G H,Zhu A L.Discussion of rupture mechanisms on the seismogenic fault of the 2008 MS8.0 Wenchuan earthquake.Sci China Earth Sci,2011,54:1360-1377
22 Yan D P,Li S B,Cao W T,et al.Multi-layer detachment crustal structure in the Longmen Mountains:Evidences from neo-tectonic deformation and geophysical data(in Chinese).Earth Sci Front,2010,17:106-116[颜丹平,李书兵,曹文涛,等.龙门山多层分层拆离地壳结构:新构造变形与深部构造证据.地学前缘,2010,17:106-116]
23 Yin A.A special issue on the great 12 May 2008 Wenchuan earthquake(Mw 7.9):Observations and unanswered questions preface.Tectonophysics,2010,491:1-9
24 Zhang Z J,Yuan X H,Yun C,et al.Seismic signature of the collision between the east Tibetan escape flow and the Sichuan Basin.Earth Planet Sci Lett,2010,292:254-264
25 Fu B H,Shi P L,Wang P,et al.Geometry and kinematics of the 2008 Wenchuan earthquake surface ruptures around the Qushan Town of Beichuan County,Sichuan:Implications for mitigation of seismic and geologic disasters(in Chinese).Chin J Geophys,2009,52:485-495[付碧宏,时丕龙,王萍,等.2008年汶川地震断层北川段的几何学与运动学特征及地震地质灾害效应.地球物理学报,2009,52:485-495]
26 Wang Q,Yuan G.Rayleigh wave phase velocity tomography and strong earthquake activity on the southeastern front of the Tibetan Plateau.Sci China Earth Sci,2014,57:2532-2542
27 Teng J W,Bai D H,Yang H,et al.Deep processes and dynamic response associated with the Wenchuan MS8.0 earthquake of 2008(in Chinese).Chin J Geophys,2008,51:1385-1402[滕吉文,白登海,杨辉,等.2008汶川MS8.0地震发生的深层过程和动力学响应.地球物理学报,2008,51:1385-1402]
28 Wang Z,Wang X B,Huang R X,et al.Deep structure imaging of multi-geophysical parameters and seismogenesis in the Longmenshan fault zone(in Chinese).Chin J Geophys,2017,60:2068-2079[王志,王绪本,黄润秋,等.龙门山断裂带多参数深部结构成像与地震成因研究.地球物理学报,2017,60:2068-2079]
29 Wei W B,Unsworth M,Jones A,et al.Detection of widespread fluids in the Tibetan crust by magnetotelluric studies.Science,2001,292:716-718
30 Sun J,Jin G W,Bai D H,et al.Sounding of electrical structure of the crust and upper mantle along the eastern border of Qinghai-Tibet Plateau and its tectonic significance.Sci China Ser D-Earth Sci,2003,46:243-253[孙洁,晋光文,白登海,等.青藏高原东缘地壳、上地幔电性结构探测及其构造意义.中国科学D辑:地球科学,2003,33:173-180]
31 Clark M K,Royden L H.Topographic ooze:Building the eastern margin of Tibet by lower crustal flow.Geology,2000,28:703-706
32 Clark M K,Bush J W M,Royden L H.Dynamic topography produced by lower crustal flow against rheological strength heterogeneities bordering the Tibetan Plateau.Geophys J Roy Astron Soc,2005,162:575-590
33 Zhu S B,Shi Y L.Genetic algorithm-finite element inversion of drag forces exerted by the lower crust on the upper crust in the Sichuan-Yunnan area(in Chinese).Chin J Geophys,2004,47:232-239[朱守彪,石耀霖.用遗传有限单元法反演川滇下地壳流动对上地壳的拖曳作用.地球物理学报,2004,47:232-239]
34 Klemperer S L.Crustal flow in Tibet:Geophysical evidence for the physical state of Tibetan lithosphere,and inferred patterns of active flow.Geol Soc Lon Spec Publ,2006,268:265-308
35 Schoenbohm L M,Burchfiel B C,Liangzhong C.Propagation of surface uplift,lower crustal flow,and Cenozoic tectonics of the southeast margin of the Tibetan Plateau.Geology,2006,34:813-816
36 Royden L H.Coupling and decoupling of crust and mantle in convergent orogens:Implications for strain partitioning in the crust.JGeophys Res-Solid Earth,1996,101:17679-17705
37 Royden L H,Burchfiel B C,King R W,et al.Surface deformation and lower crustal flow in eastern Tibet.Science,1997,276:788-790
38 Zhao G Z,Chen X B,Wang L F,et al.Evidence of crustal‘channel flow’in the eastern margin of Tibetan Plateau from MT measurements.Chin Sci Bull,2008,53:1887-1893[赵国泽,陈小斌,王立凤,等.青藏高原东边缘地壳“管流”层的电磁探测证据.科学通报,2008,3:345-350]
39 Wang C Y,Lou H,LüZ Y,et al.S-wave crustal and upper mantle’s velocity structure in the eastern Tibetan Plateau-Deep environment of lower crustal flow.Sci China Ser D-Earth Sci,2008,51:263-274[王椿镛,楼海,吕智勇,等.青藏高原东部地壳上地幔S波速度结构-下地壳流的深部环境.中国科学D辑:地球科学,2008,38:22-32]
40 Zhu J S.The Wenchuan earthquake occurrence background in deep structure and dynamics of lithosphere(in Chinese).J Chengdu Univ Tech(Sci Tech Ver),2008,35:348-356[朱介寿.汶川地震的岩石圈深部结构与动力学背景.成都理工大学学报(自然科学版),2008,35:348-356]
41 Zhu J S,Wang X B,Yang Y H,et al.The crustal flow beneath the eastern margin of the Tibetan Plateau and its process of dynamics(in Chinese).Chin J Geophys,2017,60:2038-2057[朱介寿,王绪本,杨宜海,等.青藏高原东缘的地壳流及动力过程.地球物理学报,2017,60:2038-2057]
42 Jia S X,Liu B J,Xu Z F,et al.The crustal structures of the central Longmenshan along and its margins as related to the seismotectonics of the 2008 Wenchuan earthquake.Sci China Ser D-Earth Sci,2014,57:777-790[嘉世旭,刘保金,徐朝繁,等.龙门山中段及两侧地壳结构与汶川地震构造.中国科学:地球科学,2014,44:497-509]
43 Li J,Wang X B,Li D H,et al.Characteristics of the lithosphere physical structure in eastern margin of the Qinghai-Tibet Plateau and their deep tectonic implications(in Chinese).Chin J Geophys,2017,60:2500-2511[李军,王绪本,李大虎,等.青藏高原东缘岩石圈物性结构特征及深部构造涵义.地球物理学报,2017,60:2500-2511]
44 Chen Z,Burchfiel B C,Liu Y,et al.Global positioning system measurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation.J Geophys Res-Solid Earth,2000,105:16215-16227
45 Teng J W,Pi J L,Yang H,et al.Wenchuan-Yingxiu MS8.0 earthquake seismogenic faults and deep dynamic response(in Chinese).Chin J Geophys,2014,57:392-403[滕吉文,皮娇龙,杨辉,等.汶川-映秀MS8.0地震的发震断裂带和形成的深层动力学响应.地球物理学报,2014,57:392-403]
46 Teng J W,Yang H,Zhang H S,et al.Wenchuan MS8.0 earthquak,fine velocity structures lithoshpere and dynamical mechanism(in Chinese).Quat Sci,2010,30:637-651[滕吉文,杨辉,张洪双,等.汶川-映秀8.0级大地震的发生与岩石圈精细速度结构和动力机制.第四纪研究,2010,30:637-651]
47 Teng J W,Zhang Y Q,Yan Y F.Deep process of the rupture of strong earthquakes and exploration for the impending earthquake prediction(in Chinese).Chin J Geophys,2009,52:428-443[滕吉文,张永谦,闫雅芬.强烈地震震源破裂和深层过程与地震短临预测探索.地球物理学报,2009,52:428-443]
48 Zhang Y.Inversion of source rupture process(in Chinese).Doctor Dissertation.Beijing:Peking University,2008[张勇.震源破裂过程反演方法研究.博士学位论文.北京:北京大学,2008
49 Wang W M,Zhao L F,Li J,et al.Rupture process of the MS8.0 Wenchuan earthquake of Sichuan,China(in Chinese).Chin J Geophys,2008,51:1403-1410[王卫民,赵连锋,李娟,等.四川汶川8.0级地震震源过程.地球物理学报,2008,51:1403-1410]
50 He P C,Shen Z K.Rupture triggering process of Wenchuan earthquake seismogenic faults(in Chinese).Chin J Geophys,2014,57:3308-3317[贺鹏超,沈正康.汶川地震发震断层破裂触发过程.地球物理学报,2014,57:3308-3317]
51 Chen Q F,Hua C,Li L,et al.Viscoelastic simulation of deep tectonic deformation of the Longmenshan fault zone and its implication for strong earthquakes(in Chinese).Chin J Geophys,2015,58:4129-4137[陈棋福,华诚,李乐,等.龙门山断裂带深部构造变形的黏弹性模拟及其与强震活动的关联性探讨.地球物理学报,2015,58:4129-4137]
52 He F J,Liang C T,Yang Y H,et al.The crust structure of the unruptured segment between Wenchuan and Lushan earthquakes revealed by receiver functions(in Chinese).Chin J Geophys,2017,60:2130-2146[何富君,梁春涛,杨宜海,等.用接收函数方法研究汶川和芦山地震之间未破裂段的地壳结构.地球物理学报,2017,60:2130-2146]
53 Wang C Y,Li Y H,Lou H.Issues on crustal and upper-mantle structures associated with geodynamics in the northeastern Tibetan Plateau(in Chinese).Chin Sci Bull,2016,61:2239-2263[王椿镛,李永华,楼海.与青藏高原东北部地球动力学相关的深部构造问题.科学通报,2016,61:2239-2263]
54 Zhang X Y,Gao R,Bai Z M,et al.Crustal structure beneath the Longmenshan area in eastern Tibet:New constrains from reprocessing wide-angle seismic data of the Aba-Longmenshan-Suining profile(in Chinese).Chin J Geophys,2017,60:2200-2212[张新彦,高锐,白志明,等.阿坝-遂宁宽角地震剖面重建藏东缘龙门山地区地壳速度结构.地球物理学报,2017,60:2200-2212]
55 Chen X B,Wu Y Q,Du P S.The structural features of crustal velocity on both sides of Longmenshan tectonic belt(in Chinese).In:Research and Development of Deep Structure in Mainland China.Beijing:Geology Press,1988[陈学波,吴跃强,杜平山.龙门山构造带两侧地壳速度结构特征.见:中国大陆深部构造的研究与进展.北京:地质出版社,1988]
56 Li S L,Zhang X K,Zhang C K,et al.A preliminary study on the crustal velocity structure of Maqin-Lanzhou-Jingbian by means of deep seismic sounding profile(in Chinese).Chin J Geophys,2002,45:210-217[李松林,张先康,张成科,等.玛沁-兰州-靖边地震测深剖面地壳速度结构的初步研究.地球物理学报,2002,45:210-217]
57 Wang Y X,Mooney W D,Han G H.Crustal P-wave velocity structure from Altyn Tagh to Longmen mountains along the Taiwan-Altay geoscience transect(in Chinese).Chin J Geophys,2005,48:98-106[王有学,Mooney W D,韩果花,等.台湾-阿尔泰地学断面阿尔金-龙门山剖面的地壳纵波速度结构.地球物理学报,2005,48:98-106]
58 Zhou Y M,Zhang Y S,Shi Y M,et al.Three-dimensional crustal velocity structure in the northeastern margin of the Qinghai-Tibetan Plateau(in Chinese).Prog Geophys,2006,21:127-134[周民都,张元生,石雅鏐,等.青藏高原东北缘地壳三维速度结构.地球物理学进展,2006,21:127-134]
59 Jia S X,Zhang X K.Study on the crust phases of deep seismic sounding experiments and fine crust structures in the northeast margin of Tibetan Plateau(in Chinese).Chin J Geophys,2008,51:1431-1443[嘉世旭,张先康.青藏高原东北缘深地震测深震相研究与地壳细结构.地球物理学报,2008,51:1431-1443]
60 Guo W B,Jia S X,Duan Y H,et al.A study on the basement tectonic units in the northeast margin of Tibetan Plateau-The result of Maduo-Gonghe-Yabrai refraction profile(in Chinese).Chin J Geophys,2016,59:3627-3636[郭文斌,嘉世旭,段永红,等.青藏高原东北缘基底结构研究-玛多-共和-雅布赖剖面上地壳地震折射探测.地球物理学报,2016,59:3627-3636]
61 Lin J Y,Duan Y H.Upper crustal structure of Haiyuan tectonic zone and its surrounding areas(in Chinese).Acta Seismol Sin,2016,38:179-187[林吉焱,段永红.海原构造区及其周缘上部地壳结构研究.地震学报,2016,38:179-187]
62 Song W J,Zhu J S,Cheng X Q,et al.Deep crustal structure around the source area of the Wenchuan MS8.0 earthquake(in Chinese).Quat Sci,2010,30:670-676[宋文杰,朱介寿,程先琼,等.汶川MS8.0级地震震源区地壳深部结构研究.第四纪研究,2010,30:670-676]
63 Wang H Y,Gao R,Li Q S,et al.Deep seismic reflection profiling in the Songpan-west Qinling-Linxia basin of the Qinghai-Tibet Plateau:Data acquisition,data processing and preliminary interpretations(in Chinese).Chin J Geophys,2014,57:1451-1461[王海燕,高锐,李秋生,等.青藏高原松潘-西秦岭-临夏盆地深地震反射剖面-采集、处理与初步解释.地球物理学报,2014,57:1451-1461]
64 Liu Q Y,Hilst R D V D,Li Y,et al.Eastward expansion of the Tibetan Plateau by crustal flow and strain partitioning across faults.Nat Geosci,2014,7:361-365
65 Wang C Y,Flesch L M,Chang L J,et al.Evidence of active mantle flow beneath South China.Geophys Res Lett,2013,40:5137-5141
66 Chen J H,Liu Q Y,Li S C,et al.Crust and upper mantle S-wave velocity structure across Northeastern Tibetan Plateau and Ordos block(in Chinese).Chin J Geophys,2005,48:333-342[陈九辉,刘启元,李顺成,等.青藏高原东北缘-鄂尔多斯地块地壳上地幔S波速度结构.地球物理学报,2005,48:333-342]
67 Ding Z F,He Z Q,Sun W G,et al.3-D crust and upper mantle velocity structure in eastern Tibetan Plateau and its surrounding areas(in Chinese).Chin J Geophys,1999,42:197-205[丁志峰,何正勤,孙为国,等.青藏高原东部及其边缘地区的地壳上地幔三维速度结构.地球物理学报,1999,42:197-205]
68 Li Y H,Wu Q J,An Z H,et al.The Poisson ratio and crustal structure across the NE Tibetan Plateau determined from receiver functions(in Chinese).Chin J Geophys,2006,49:1359-1368[李永华,吴庆举,安张辉,等.青藏高原东北缘地壳S波速度结构与泊松比及其意义.地球物理学报,2006,49:1359-1368]
69 Liang C T,Song X D.A low velocity belt beneath northern and eastern Tibetan Plateau from Pn tomography.Geophys Res Lett,2006,33:121-132
70 Shen W S,Ritzwoller M H,Kang D,et al.A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion.Geophys J Int,2016,206:ggw175
71 Xu Y,Li Z,Huang R,et al.Seismic structure of the Longmen Shan region from S-wave tomography and its relationship with the Wenchuan MS8.0 earthquake on 12 May 2008,southwestern China.Geophys Res Lett,2010,37:211-228
72 Li S H,Wang Y B,Liang Z B,et al.Crustal structure in southeastern Gansu from regional seismic waveform inversion(in Chinese).Chin J Geophys,2012,55:1186-1197[李少华,王彦宾,梁子斌,等.甘肃东南部地壳速度结构的区域地震波形反演.地球物理学报,2012,55:1186-1197]
73 Wang C Y,Sandvol E,Zhu L,et al.Lateral variation of crustal structure in the Ordos block and surrounding regions,North China,and its tectonic implications.Earth Planet Sci Lett,2014,387:198-211
74 Yang Y J,Ritzwoller M H,Zheng Y,et al.A synoptic view of the distribution and connectivity of the mid-crustal low velocity zone beneath Tibet.J Geophys Res-Solid Earth,2012,117:B04303
75 Deng W Z,Chen J H,Guo B,et al.Fine velocity structure of the Longmenshan fault zone by double-difference tomography(in Chinese).Chin J Geophys,2014,57:1101-1110[邓文泽,陈九辉,郭飚,等.龙门山断裂带精细速度结构的双差层析成像研究.地球物理学报,2014,57:1101-1110]
76 Liu Q M,Zhao J M,Lu F,et al.Crustal structure of northeastern margin of the Tibetan Plateau by receiver function inversion.Sci China Earth Sci,2014,57:741-750[刘启民,赵俊猛,卢芳,等.用接收函数方法反演青藏高原东北缘地壳结构.中国科学:地球科学,2014,44:668-679]
77 Zhang Y,Cheng S Y,Zhao B K,et al.The feature of tectonics in the Tibet Plateau from new regional gravity signals(in Chinese).Chin JGeophys,2013,56:1369-1380[张燕,程顺有,赵炳坤,等.青藏高原构造结构特点:新重力异常成果的启示.地球物理学报,2013,56:1369-1380]
78 Li Y H,Pan J T,Wu Q J,et al.Crustal and uppermost mantle structure of SE Tibetan Plateau from Rayleigh-wave group-velocity measurements.Earthq Sci,2014,27:411-419
79 Yu D X,Li Y H,Wu Q J,et al.S-wave velocity structure of the northeastern Tibetan Plateau from joint inversion of Rayleigh wave phase and group velocities(in Chinese).Chin J Geophys,2014,57:800-811[余大新,李永华,吴庆举,等.利用Rayleigh波相速度和群速度联合反演青藏高原东北缘S波速度结构.地球物理学报,2014,57:800-811]
80 Deng Y F,Shen W S,Xu T,et al.Crustal layering in northeastern Tibet:A case study based on joint inversion of receiver functions and surface wave dispersion.Geophys J Int,2015,203:692-706
81 Pan J T,Li Y H,Wu Q J,et al.Phase velocity maps of Rayleigh waves in the southeast Tibetan Plateau(in Chinese).Chin J Geophys,2015,58:3993-4006[潘佳铁,李永华,吴庆举,等.青藏高原东南部地区瑞利波相速度层析成像.地球物理学报,2015,58:3993-4006]
82 Zhang H S,Gao R,Tian X B,et al.Crustal S-wave velocity beneath the northeastern Tibetan Plateau inferred from teleseismic P-wave receiver functions(in Chinese).Chin J Geophys,2015,58:3982-3992[张洪双,高锐,田小波,等.青藏高原东北缘地壳S波速度结构及其动力学含义-远震接收函数提供的证据.地球物理学报,2015,58:3982-3992]
83 Wang X B,Gao Y,Wang Z,et al.Research progress on deep geophysics and continental dynamics in Eastern Tibetan Plateau(in Chinese).Chin J Geophys,2017,60:2030-2037[王绪本,高原,王志,等.青藏高原东缘深部地球物理与大陆动力学研究进展.地球物理学报,2017,60:2030-2037]
84 Allam A A,Ben-Zion Y.Seismic velocity structures in the southern California plate-boundary environment from double-difference tomography.Geophys J Int,2012,190:1181-1196
85 Allen C R,Gillespie A R,Han Y,et al.Red River and associated faults,Yunnan Province,China:Quaternary geology,slip rates,and seismic hazard.Geol Soc Am Bull,1984,95:686-700
86 Pesicek J D,Thurber C H,Zhang H,et al.Teleseismic double-difference relocation of earthquakes along the Sumatra-Andaman subduction zone using a 3-D model.J Geophys Res-Solid Earth,2010,115:B10303
87 Waldhauser F,Ellsworth W L.A double-difference earthquake location algorithm:Method and application to the northern Hayward fault,California.Bull Seismol Soc Am,2000,90:1353-1368
88 Teng J W,Si X,Wang Q S,et al.Collation and stipulation of the core science problems and theoretical concept in the geoscience study on the Tibetan Plateau(in Chinese).Chin J Geophys,2015,58:103-124[滕吉文,司芗,王谦身,等.青藏高原地球科学研究中的核心问题与理念的厘定.地球物理学报,2015,58:103-124]
89 Hai L,Wang C Y,LüZ Y,et al.Deep tectonic setting of the 2008 Wenchuan MS8.0 earthquake in southwestern China―Joint analysis of teleseismic P-wave receiver functions and Bouguer gravity anomalies.Sci China Ser D-Earth Sci,2009,52:166-179[楼海,王椿镛,吕智勇,等.2008年汶川MS8.0级地震的深部构造环境-远震P波接收函数和布格重力异常的联合解释.中国科学D辑:地球科学,2008,38:1207-1220]
90 She Y W,Fu G Y,Wang Z H,et al.Vertical tectonic stress in eastern margin of Bayan Har block revealed by gravity and terrain data(in Chinese).Chin J Geophys,2017,60:2480-2492[佘雅文,付广裕,王灼华,等.重力与地形数据揭示的巴颜喀拉块体东缘垂向构造应力场.地球物理学报,2017,60:2480-2492]
91 Shen C Y,Li H,Sun S A,et al.Dynamic variations of gravity and the preparation process of the Wenchuan MS8.0 earthquake(in Chinese).Chin J Geophys,2009,52:2547-2557[申重阳,李辉,孙少安,等.重力场动态变化与汶川MS8.0地震孕育过程.地球物理学报,2009,52:2547-2557]
92 Wang Q S,Teng J W,Zhang Y Q,et al.The effect of crustal gravity isostasy and Wenchuan earthquake in Longmenshan faults and adjacent area(in Chinese).Chin J Geophys,2008,23:1664-1670[王谦身,滕吉文,张永谦,等.龙门山断裂系及邻区地壳重力均衡效应与汶川地震.地球物理学进展,2008,23:1664-1670]
93 Wang Q S,Teng J W,Zhang Y Q,et al.The crustal structure and gravity isostasy in the middle western Sichuan area(in Chinese).Chin JGeophys,2009,52:579-583[王谦身,滕吉文,张永谦,等.四川中西部地区地壳结构与重力均衡.地球物理学报,2009,52:579-583]
94 Zhang J S,Gao R,Zeng L S,et al.Relationship between characteristics of gravity and magnetic anomalies and the earthquakes in Longmenshan range and adjacent areas(in Chinese).Chin J Geophys,2009,52:572-578[张季生,高锐,曾令森,等.龙门山及邻区重、磁异常特征及与地震关系的研究.地球物理学报,2009,52:572-578]
95 Zhang J S,Gao R,Li Q S,et al.A study on geophysical characteristic and basement in the Songpan-Garze and Western Qinling Orogenic Belt(in Chinese).Geol Rev,2007,53:261-266[张季生,高锐,李秋生,等.松潘-甘孜和西秦岭造山带地球物理特征及基底构造研究.地质论评,2007,53:261-266]
96 Zhang Y Q,Wang Q S,Teng J W.The crustal isostatic anomaly beneath eastern Tibet and western Sichuan and its relationship with the distribution of earthquakes(in Chinese).Chin J Geophys,2010,53:2631-2638[张永谦,王谦身,滕吉文.川西藏东地区的地壳均衡异常及其与地震分布的关系.地球物理学报,2010,53:2631-2638]
97 Zhu Y Q,Liu F,Li T M,et al.Dynamic variation of the gravity field in the Sichuan-Yunnan region and its implication for seismic risk(in Chinese).Chin J Geophys,2015,58:4187-4196[祝意青,刘芳,李铁明,等.川滇地区重力场动态变化及其强震危险含义.地球物理学报,2015,58:4187-4196]
98 Bi B T,Hu X Y,Li L Q,et al.Multi-scale analysis to the gravity field of the northeastern Tibetan Plateau and its geodynamic implications(in Chinese).Chin J Geophys,2016,59:543-555[毕奔腾,胡祥云,李丽清,等.青藏高原东北部多尺度重力场及其地球动力学意义.地球物理学报,2016,59:543-555]
99 Meng X H,Shi L,Guo L H,et al.Multi-scale analyses of transverse structures based on gravity anomalies in the northeastern margin of the Tibetan Plateau(in Chinese).Chin J Geophys,2012,55:3933-3941[孟小红,石磊,郭良辉,等.青藏高原东北缘重力异常多尺度横向构造分析.地球物理学报,2012,55:3933-3941]
100 Zhang S M,Xie F R,Huang Z X,et al.Bending and thrusting of the upper crust in Longmenshan area and its deep dynamics(in Chinese).Quat Sci,2009,29:449-463[张世民,谢富仁,黄忠贤,等.龙门山地区上地壳的拱曲冲断作用及其深部动力学机制探讨.第四纪研究,2009,29:449-463]
101 Zhang Y Q,Wang Q S,Teng J W.Crustal isotatic state in western Sichuan and its dynamical mechanism(in Chinese).Quat Sci,2010,30:662-669[张永谦,王谦身,滕吉文.川西地区的地壳均衡状态及其动力学机制.第四纪研究,2010,30:662-669]
102 Li Y.Contiental Dynamic Process and Gelogical Response of the Eastern Margin of Tibetan Plateau(in Chinese).Beijing:Geological Press,2006[李勇.青藏高原东缘大陆动力学过程与地质响应.北京:地质出版社,2006]
103 Bai D H,Unsworth M J,Meju M A,et al.Crustal deformation of the eastern Tibetan Plateau revealed by magnetotelluric imaging.Nat Geosci,2010,3:358-362
104 Unsworth M J,Meju M A.Crustal deformation of the eastern Tibetan Plateau revealed by magnetotelluric imaging.Nat Geosci,2011,3:358-362
105 Zhao B,Shi Y,Gao Y.Seismic relocation,focal mechanism and crustal seismic anisotropy associated with the 2010 Yushu MS7.1earthquake and its aftershocks.Acta Seismol Sin,2012,25:111-119
106 Chen Y Z,Tang J,Cai J T,et al.Deep electrical structure beneath the Sichuan-Yunnan area in the eastern margin of the Tibetan Plateau(in Chinese).Chin J Geophys,2017,60:2425-2441[程远志,汤吉,蔡军涛,等.青藏高原东缘川滇构造区深部电性结构特征.地球物理学报,2017,60:2425-2441]
107 Chen Y Z,Tang J,Chen X B,et al.Electrical structure and seismogenic environment along the border region of Yunnan,Sichuan and Guizhou in the south of the North-South seismic belt(in Chinese).Chin J Geophys,2015,58:3965-3981[程远志,汤吉,陈小斌,等.南北地震带南段川滇黔接壤区电性结构特征和孕震环境.地球物理学报,2015,58:3965-3981]
108 Wang L F,Zhao G Z,Zhan Y,et al.Electric structure of crust beneath the southwestern segment of the Longmenshan fault zone(in Chinese).Seismol Geol,2014,36:302-311[王立凤,赵国泽,詹艳,等.龙门山断裂带西南端地壳电性结构.地震地质,2014,36:302-311]
109 Wang X B,Luo W,Zhang G,et al.Electrical resistivity structure of Longmenshan crust-mantle under sector boundary(in Chinese).Chin J Geophys,2013,56:2718-2727[王绪本,罗威,张刚,等.扇形边界条件下的龙门山壳、幔电性结构特征.地球物理学报,2013,56:2718-2727]
110 Wang X B,Yu N,Gao S,et al.Research progress in research on electrical structure of crust and upper mantle beneath the eastern margin of the Tibetan Plateau(in Chinese).Chin J Geophys,2017,60:2350-2370[王绪本,余年,高嵩,等.青藏高原东缘地壳上地幔电性结构研究进展.地球物理学报,2017,60:2350-2370]
111 Zhang L T,Jin S,Wei W B,et al.Electrical structure of crust and upper mantle beneath the eastern margin of the Tibetan Plateau and the Sichuan basin(in Chinese).Chin J Geophys,2012,55:4126-4137[张乐天,金胜,魏文博,等.青藏高原东缘及四川盆地的壳、幔导电性结构研究.地球物理学报,2012,55:4126-4137]
112 Bai D H,Teng J W,Ma X B,et al.Crustal flow beneath eastern Tibetan Plateau revealed by magnetotelluric measurements(in Chinese).Chin Basic Sci,2011,13:7-10[白登海,滕吉文,马晓冰,等.大地电磁观测揭示青藏高原东部存在两条地壳物质流.中国基础科学,2011,13:7-10]
113 Min G,Wang X B,Xia S B,et al.Electrical structure of middle and upper crust beneath the Minshan uplift zone and central section of the West Qinling orogenic zone(in Chinese).Chin J Geophys,2017,60:2397-2413[闵刚,王绪本,夏时斌,等.岷山隆起带与西秦岭构造带中段中上地壳电性结构特征.地球物理学报,2017,60:2397-2413]
114 Zhan Y,Yang H,Zhao G Z,et al.Deep electrical structure of crust beneath the Madongshan step area at the Haiyuan fault in the northeastern margin of the Tibetan Plateau and tectonic implications(in Chinese).Chin J Geophys,2017,60:2371-2384[詹艳,杨皓,赵国泽,等.青藏高原东北缘海原构造带马东山阶区深部电性结构特征及其构造意义.地球物理学报,2017,60:2371-2384]
115 Yan Y F,Teng J W,Ruan X M,et al.Aeromagnetic field characteristics and the Wenchuan earthquakes in the Longmenshan mountains and adjacent areas(in Chinese).Chin J Geophys,2016,59:197-214[闫亚芬,滕吉文,阮小敏,等.龙门山和相邻地域航磁场特征与汶川大地震.地球物理学报,2016,59:197-214]
116 Hu Y P,Wang Z,Liu G N,et al.Crustal structure imaging of multi-geophysical parameters and generating mechanisms of large earthquakes in North-South Seismic Zone(in Chinese).Chin J Geophys,2017,60:2113-2129[胡亚平,王志,刘冠男,等.南北地震带地壳结构多参数成像及强震触发机制研究.地球物理学报,2017,60:2113-2129]
117 Wang C Y,Chang L J,LüZ Y,et al.Seismic anisotropy of upper mantle in eastern Tibetan Plateau and related crust-mantle coupling pattern.Sci China Ser D-Earth Sci,2007,50:1150-1160[王椿镛,常利军,吕智勇,等.青藏高原东部上地幔各向异性及相关的壳、幔耦合型式.中国科学D辑:地球科学,2007,37:495-503]
118 Zhao P P,Chen J H,Campillo M,et al.Crustal velocity changes associated with the Wenchuan M8.0 earthquake by auto-correlation function analysis of seismic ambient noise(in Chinese).Chin J Geophys,2012,55:137-145[赵盼盼,陈九辉,Campillo M,等.汶川地震区地壳速度相对变化的环境噪声自相关研究.地球物理学报,2012,55:137-145]
119 Zhao P P,Chen J H,Liu Q Y,et al.Fine structure of middle and upper crust of the Longmenshan Fault zone from short period seismic ambient noise(in Chinese).Chin J Geophys,2015,58:4018-4030[赵盼盼,陈九辉,刘启元,等.龙门山断裂带中上地壳速度结构的短周期环境噪声成像.地球物理学报,2015,58:4018-4030]
120 Gouédard P,Yao H,Ernst F,et al.Surface wave eikonal tomography in heterogeneous media using exploration data.Geophys J Int,2012,191:781-788
121 Lin F C,Ritzwoller M H.Helmholtz surface wave tomography for isotropic and azimuthally anisotropic structure.Geophys J Int,2011,186:1104-1120
122 Lin F C,Ritzwoller M H,Snieder R.Eikonal tomography:Surface wave tomography by phase front tracking across a regional broad-band seismic array.Geophys J Roy Astron Soc,2010,177:1091-1110
123 Zhu J S,Zhao J M,Jiang X T,et al.Crustal flow beneath the eastern margin of the Tibetan Plateau.Earthq Sci,2012,25:469-483
124 Jin G,Gaherty J B.Surface wave phase-velocity tomography based on multichannel cross-correlation.Geophys J Int,2015,201:1383-1398
125 Zhong S J,Wu J P,Fang L H,et al.Surface wave eikonal tomography in and around the northeastern margin of the Tibetan Plateau(in Chinese).Chin J Geophys,2017,60:2304-2314[钟世军,吴建平,房立华,等.青藏高原东北缘及周边地区基于程函方程的面波层析成像.地球物理学报,2017,60:2304-2314]
126 Lei J S,Zhao D P.Structural heterogeneity of the Longmenshan fault zone and the mechanism of the 2008 Wenchuan earthquake(MS8.0).Geochem Geophys Geosyst,2009,10:1-17
127 Zheng T Y,Zhao L,Zhu R X.New evidence from seismic imaging for subduction during assembly of the North China Craton:REPLY.Geology,2010,38:395-398
128 Huang Z X,Li H Y,Xu Y.Lithospheric S-wave velocity structure of the North-South Seismic Belt of China from surface wave tomography(in Chinese).Chin J Geophys,2013,56:1121-1131[黄忠贤,李红谊,胥颐.南北地震带岩石圈S波速度结构面波层析成像.地球物理学报,2013,56:1121-1131]
129 Lei J S,Zhao D P,Su J R,et al.Fine seismic structure under the Longmenshan fault zone and the mechanism of the large Wenchuan earthquake(in Chinese).Chin J Geophys,2009,52:339-345[雷建设,赵大鹏,苏金蓉,等.龙门山断裂带地壳精细结构与汶川地震发震机理.地球物理学报,2009,52:339-345]
130 Liu Q Y,Li Y,Chen J H,et al.Wenchuan MS8.0 earthquake:Preliminary study of the S-wave velocity structure of the crust and upper mantle(in Chinese).Chin J Geophys,2009,52:309-319[刘启元,李昱,陈九辉,等.汶川MS8.0地震:地壳上地幔S波速度结构的初步研究.地球物理学报,2009,52:309-319]
131 Wang C Y,Yang W C,Wu J P,et al.Study on the lithospheric structure and earthquakes in North-South Tectonic Belt(in Chinese).Chin JGeophys,2015,58:3867-3901[王椿镛,杨文采,吴建平,等.南北构造带岩石圈结构与地震的研究.地球物理学报,2015,58:3867-3901]
132 Xu X M,Ding Z F,Zhang F X.The teleseismic tomography study by P-wave traveltime data beneath the southern South-north Seismic Zone(in Chinese).Chin J Geophys,2015,58:4041-4051[徐小明,丁志峰,张风雪.南北地震带南段远震P波走时层析成像研究.地球物理学报,2015,58:4041-4051]
133 He M X,Fang H,Wang X B,et al.Deep conductivity characteristics of the southern Xianshuihe fault zone(in Chinese).Chin J Geophys,2017,60:2414-2424[何梅兴,方慧,王绪本,等.鲜水河断裂带南段深部电性结构特征研究.地球物理学报,2017,60:2414-2424]
134 Wang C Y,Han W B,Wu J P,et al.Crustal structure beneath the eastern margin of the Tibetan Plateau and its tectonic implications.JGeophys Res-Solid Earth,2007,112:1-21
135 Yang H,Teng J W,Pi J L.Numerical simulation of the geodynamical condition about the channel flow model in Tibetan Plateau(in Chinese).Chin J Geophys,2013,56:2625-2635[杨辉,滕吉文,皮娇龙.青藏高原通道流模型动力环境的数值模拟.地球物理学报,2013,56:2625-2635]
136 Pi J L,Teng J W,Yang H.Geodynamic response of Moho relief modes to the channel flow below the Tibetan Plateau:Numerical simulation(in Chinese).Chin J Geophys,2014,57:2766-2776[皮娇龙,滕吉文,杨辉.青藏高原Moho界面起伏样式对通道流模型的动力学响应-基于数值模拟.地球物理学报,2014,57:2766-2776]
137 Jia S X,Lin J Y,Guo W B,et al.Investigation on diversity of crustal structures beneath the Bayan Har block(in Chinese).Chin J Geophys,2017,60:2226-2238[嘉世旭,林吉焱,郭文斌,等.巴颜喀拉块体地壳结构多样性探测.地球物理学报,2017,60:2226-2238]
138 Chen Y T.On the magnitude and the fault length of the great Wenchuan earthquake(in Chinese).Sci Tech Rev,2008,26:26-27[陈运泰.汶川特大地震的震级和断层长度.科技导报,2008,26:26-27]
139 Wu J P,Huang Y,Zhang T Z,et al.Aftershock distribution of the MS8.0 Wenchuan earthquake and three dimensional P-wave velocity structure in and around source region(in Chinese).Chin J Geophys,2009,52:320-328[吴建平,黄媛,张天中,等.汶川MS8.0级地震余震分布及周边区域P波三维速度结构研究.地球物理学报,2009,52:320-328]
140 Zhu A L,Xu X W,Diao G L,et al.Relocation of the MS8.0 Wenchuan earthquake sequence in part:Preliminary seismotectonic analysis(in Chinese).Seismol Geol,2008,30:759-767[朱艾斓,徐锡伟,刁桂苓,等.汶川MS8.0地震部分余震重新定位及地震构造初步分析.地震地质,2008,30:759-767]
141 Bai Y Z,Xu X W,Xu J,et al.A research on the distribution of deformation fields near the fault of 2008 Wenchuan earthquake(in Chinese).Chin J Geophys,2011,54:1798-1804[白玉柱,徐锡伟,徐杰,等.2008年汶川地震近断裂区域变形场的空间分布.地球物理学报,2011,54:1798-1804]
142 Guo X Y,Gao R,Keller G R,et al.Discussion on the mountain building process of the Longmenshan range(in Chinese).Chin J Geol,2014,49:1337-1345[郭晓玉,高锐,Keller G R,等.龙门山断裂带隆起造山独特性探讨.地质科学,2014,49:1337-1345]
143 Yang H,Teng J W,Wang Q S,et al.Numerical simulation on the special gravity fields and dynamic response in Longmenshan orogenic belt and adjacent area(in Chinese).Chin J Geophys,2013,56:106-116[杨辉,滕吉文,王谦身,等.龙门山造山带及邻区重力场特征与动力学响应数值模拟.地球物理学报,2013,56:106-116]
144 Royden L H,Burchfiel B C,Rd V D H.The geological evolution of the Tibetan Plateau.Science,2008,321:1054-1058
145 Chen G G,Ji F J,Zhou R J,et al.Primary research of activity segmentation of Longmenshan Fault zone since late-Quaternary(in Chinese).Seimol Geol,2007,29:657-673[陈国光,计凤桔,周荣军,等.龙门山断裂带晚第四纪活动性分段的初步研究.地震地质,2007,29:657-673]
146 Li H B,Si J L,Fu X F,et al.Co-seismic rupture and maximum displacement of the 2008 Wenchuan earthquake and its tectonic implications(in Chinese).Quat Sci,2009,29:387-402[李海兵,司家亮,付小方,等.2008年汶川地震同震滑移特征、最大滑移量及构造意义.第四纪研究,2009,29:387-402]
147 Wang H,Li H B,Pei J L,et al.Structural and lithologic characteristics of the Wenchuan earthquake fault zone and its relationship with the sesimic activities(in Chinese).Quat Sci,2010,30:768-778[王焕,李海兵,裴军令,等.汶川地震断裂带结构、岩性特征及其与地震活动的关系.第四纪研究,2010,30:768-778]
148 Xu J,Gao X L,Zhou B G,et al.The seismogenic structure of the 2008 Wenchuan MS8.0 earthquake:A newly generated deep fault in crust along the Longmen Mountains fault zone in the shallow subsurface(in Chinese).Earth Sci Front,2010,17:117-127[徐杰,高祥林,周本刚,等.2008年汶川8.0级地震的发震构造:沿龙门山断裂带新生的地壳深部断裂.地学前缘,2010,17:117-127]
149 Wang C Y,Flesch L M,Silver P G,et al.Evidence for mechanically coupled lithosphere in central Asia and resulting implications.Geology,2008,36:363-366
150 Shan J X,Song X G,Han Y F,et al.The characteristics of surface vertical deformation before the Wenchuan MS8.0 earthquake from In SAR(in Chinese).Chin J Geophys,2009,52:2739-2745[单新建,宋小刚,韩宇飞,等.汶川MS8.0地震前In SAR垂直形变场变化特征研究.地球物理学报,2009,52:2739-2745]
151 Shan J X,Zhang G H,Wang C S,et al.Joint inversion for the spatial fault slip distribution of the 2015 Nepal Mw 7.9 earthquake based on In SAR and GPS observations(in Chinese).Chin J Geophys,2015,58:4266-4276[单新建,张国宏,汪驰升,等.基于In SAR和GPS观测数据的尼泊尔地震发震断层特征参数联合反演研究.地球物理学报,2015,58:4266-4276]
152 Li Y H,Wang Q L,Cui D X,et al.Inversion of present-day fault slip,rate along Altyn Tagh Fault constrained by GPS data(in Chinese).Seismol Geol,2015,37:869-879[李煜航,王庆良,崔笃信,等.利用GPS数据反演阿尔金断裂现今滑动速率.地震地质,2015,37:869-879]
153 Liu X,Sun D Y,Ma J,et al.Present-day deformation and stress state of Longmenshan fault from GPS results-Comparative research on active faults in Sichuan-Yunnan region(in Chinese).Chin J Geophys,2014,57:1091-1100[刘峡,孙东颖,马瑾,等.GPS结果揭示的龙门山断裂带现今形变与受力-与川滇地区其他断裂带的对比研究.地球物理学报,2014,57:1091-1100]
154 Xu Z Q,Li H B,Wu Z L.Wenchuan earthquake and scientific drilling(in Chinese).Acta Geol Sin,2008,82:1613-1622[许志琴,李海兵,吴忠良.汶川地震和科学钻探.地质学报,2008,82:1613-1622]
155 Zhang P Z,Wang Q,Ma Z J.GPS velocity field and active crustal blocks of contemporary tectonic deformation in continental China(in Chinese).Earth Sci Front,2002,9:430-441[张培震,王琪,马宗晋.中国大陆现今构造运动的GPS速度场与活动地块.地学前缘,2002,9:430-441]
156 Xiao Z H,Xu C J,Jiang G Y,et al.Crustal strain in the Longmenshan region considering fault locking during ten years before the 2008Wenchuan earthquake(in Chinese).Chin J Geophys,2017,60:953-961[肖卓辉,许才军,江国焰,等.汶川地震前十年间龙门山区域顾及断层闭锁的地壳应变场.地球物理学报,2017,60:953-961]
157 Zhang Z J,Wang Y H,Chen Y,et al.Crustal structure across Longmenshan fault belt from passive source seismic profiling.Geophys Res Lett,2009,36:1397-1413
158 Zhang Y Q,Li H L.Late Quaternary active faulting along the SW segment of the Longmenshan Fault(in Chinese).Quat Sci,2010,30:699-710[张岳桥,李海龙.龙门山断裂带西南段晚第四纪活动性调查与分析.第四纪研究,2010,30:699-710]
159 Zhang Z Q,Zhang P Z,Wang Q L.The structure and seismogenic mechanism of Longmenshan high dip-angle reverse fault(in Chinese).Chin JGeophys,2010,53:2068-2082[张竹琪,张培震,王庆良.龙门山高倾角逆断层结构与孕震机制.地球物理学报,2010,53:2068-2082]
160 Tan K,Yang S M,Qiao X J,et al.Rupture of ramp-décollement faults in the 2008 Wenchuan earthquake-Geodetic evidence for the uplift of the Longmenshan driven by convergent deformation(in Chinese).Chin J Geophys,2013,56:1506-1516[谭凯,杨少敏,乔学军,等.2008年汶川地震中断坡-滑脱断层破裂:龙门山挤压隆升的大地测量证据.地球物理学报,2013,56:1506-1516]
161 Yang Y H,Chen Q,Liu G X,et al.Correction of coseismic deformation field associated with Wenchuan earthquake with GPS observables and In SAR adjacent track smoothing and fault slip inversion(in Chinese).Chin J Geophys,2014,57:1462-1476[杨莹辉,陈强,刘国祥,等.汶川地震同震形变场的GPS和In SAR邻轨平滑校正与断层滑移精化反演.地球物理学报,2014,57:1462-1476]
162 Liu Q X,Zhu J S,Cao J X,et al.Relocation of the Wenchuan MS8.0 earthquake sequence and its aftershocks and their spatial distribution characteristics(in Chinese).Quat Sci,2010,30:736-744[刘巧霞,朱介寿,曹俊兴,等.汶川MS8.0级地震余震重新定位及其空间分布特征研究.第四纪研究,2010,30:736-744]
163 Teng J W,Song P H,Zhang X M,et al.The driving force and movement of materials in the Earth’s interior(in Chinese).Chin Sci Bull,2016,61:1995-2019[滕吉文,宋鹏汉,张雪梅,等.地球内部物质的运动与动力.科学通报,2016,61:1995-2019]
164 Wang X C,Ding Z F,Wu Y,et al.Crustal thicknesses and Poisson’s ratios beneath the northern section of the North-South Seismic belt and surrounding areas in China(in Chinese).Chin J Geophys,2017,60:2080-2090[王兴臣,丁志峰,武岩,等.中国南北地震带北段及其周缘地壳厚度与泊松比研究.地球物理学报,2017,60:2080-2090]
165 Yue H,Lay T,Rivera L,et al.Rupture process of the 2010 Mw 7.8 Mentawai tsunami earthquake from joint inversion of nearfield GPSand teleseismic body wave recordings constrained by tsunami observations.J Geophys Res-Solid Earth,2015,119:5574-5593
166 Deng Q D,Cheng S P,Ma J,et al.Seismic activities and earthquake potential in the Tibetan Plateau(in Chinese).Chin J Geophys,2014,57:2025-2042[邓起东,程绍平,马冀,等.青藏高原地震活动特征及当前地震活动形势.地球物理学报,2014,57:2025-2042]
167 Ding L.Nepal earthquake leads the south extrustion of Himalyayas(in Chinese).Chin Nat Geogr,2015,8:156-163[丁林.尼泊尔大地震令喜马拉雅山向南摊开.中国国家地理,2015,8:156-163]
168 Teng J W.Ponder and research on the genesis and occurrence of strong earthquakes and the prediction of their place,time and intensity(in Chinese).Chin J Geophys,2010,53:1749-1766[滕吉文.强烈地震孕育与发生的地点、时间及强度预测的思考与探讨.地球物理学报,2010,53:1749-1766]
169 Teng J W,Ma X Y,Zhang X M,et al.Deep processes and dynamic responses of the generation and occurrence of the 2015 Nepal MS8.1earthquake(in Chinese).Chin J Geophys,2017,60:123-141[滕吉文,马学英,张雪梅,等.2015年尼泊尔MS8.1大地震孕育的深层过程与发生的动力学响应.地球物理学报,2017,60:123-141]
170 Teng J W,Ruan X M,Zhang Y Q,et al.The stratificational velocity structure of crust and covering strata of upper mantle and the orbit of deep interaquifer substance locus of movement for Tibetan Plateau(in Chinese).Chin J Geophys,2012,28:4077-4100[滕吉文,阮小敏,张永谦,等.青藏高原地壳与上地幔成层速度结构与深部层间物质的运移轨迹.岩石学报,2012,28:4077-4100]
171 Teng J W,Wang Q S,Wang G J,et al.Specific gravity field and deep crustal structure of the“Himalayas east structural knot”(in Chinese).Chin J Geophys,2006,49:1045-1052[滕吉文,王谦身,王光杰,等.喜马拉雅“东构造结”地区的特异重力场与深部地壳结构.地球物理学报,2006,49:1045-1052]