引文
[1]Tapponnier P,Molnar P.Active faulting and tectonics inChina.J.Geophys.Res.,1977,82(20):2905-2930.
[2]Allen C R,Gillespie A R,Han Y,et al.Red River andassociated faults,Yunnan Province,China:Quaternarygeology,slip rates,and seismic hazard.Geological Societyof America Bulletin,1984,95(6):686-700.
[3]许志琴,杨经绥,李海兵等.印度—亚洲碰撞大地构造.地质学报,2011,85(1):1-33.Xu Z Q,Yang J S,Li H B,et al.On the tectonics of theIndian-Asia collision.Acta Geolocia Sinica(in Chinese),2011,85(1):1-33.
[4]King R W,Shen F,Burchfiel B C,et al.Geodeticmeasurement of crustal motion in southwest China.Geology,1997,25(2):179-182.
[5]王刚,王二七.挤压造山带中的伸展构造及其成因-以滇中地区晚新生代构造为例.地震地质,2005,27(2):188-199.Wang G,Wang E Q.Extensional structures within thecompressional orogenic belt and its mechanism:A case studyfor the late Cenozoic deformation in central Yunnan.Seismology and Geology(in Chinese),2005,27(2):188-199.
[6]崔作舟,卢德源,陈纪平等.攀西地区的深部地壳结构与构造.地球物理学报,1987,30(6):566-58.Cui Z Z,Lu D Y,Chen J P,et al.The deep structural andtectonic features of the crust in Panxi area.Chinese J.Geophys.(in Chinese),1987,30(6):566-580.
[7]熊绍柏,郑哗,尹周勋等.丽江—攀枝花—者海地带二维地壳结构及其构造意义.地球物理学报,1993,36(4):434-444.Xiong S B,Zheng Y,Yin Z X,et al.The 2-D structure andit′s tectonic implications of the crust in the Lijiang-Panzhihua-Zhehai Region.Chinese J.Geophys.(in Chinese),36(4):434-444.
[8]张中杰,白志明,王椿镛等.冈瓦纳型和杨子型地块地壳结构:以滇西孟连—马龙宽角反射剖面为例.中国科学(D辑),2005,34(5):387-392.Zhang Z J,Bai Z M,Wang C Y,et al.Crustal structure ofGondwana-and Yangtze-typed blocks:An example by wide-angle seismic profile from Menglian to Malong in westernYunnan.Science in China(Series D)(in Chinese),2005,34(5):387-392.
[9]刘建华,刘福田,吴华等.中国南北带地壳和上地幔的三维速度图像.地球物理学报,1989,32(2):143-151.Liu J H,Liu F T,Wu H,et al.3-D velocity images of thecrust and upper mantle beneath North-South zone in China.Chinese J.Geophys.(in Chinese),1989,32(2):143-151.
[10]刘福田,刘建华,何建坤等.滇西特提斯造山带下扬子地块的俯冲板片.科学通报,2000,45(1):79-84.Liu F T,Liu J H,He J K,et al.The subducted slab ofYangtz continental block beneath the Tethyan orogen inwestern Yunnan.Chinese Science Bulletin(in Chinese),2000,45(1):79-84.
[11]Huang J,Zhao D,Zheng S.Lithospheric structure and itsrelationship to seismic and volcanic activity in southwestChina.J.Geophys.Res.,2002,107(B10),2255,doi:10.1029/2000JB000137.
[12]吴建平,明跃红,王椿镛.云南数字地震台站下方的S波速度结构研究.地球物理学报,2001,44(2):228-230.Wu J P,Ming Y H,Wang C Y.The S wave velocitystructure beneath digital seismic stations of Yunnan provinceinferred from teleseimci receiver function modeling.ChineseJ.Geophys.(in Chinese),2001,44(2):228-230.
[13]吴建平,黄媛,张天中等.汶川8.0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(2):320-328.Wu J P,Huang Y,Zhang T Z,et al.Aftershock distributionof the Ms8.0 Wenchuan earthquake and 3-D P-wave velocitystructure in and around source region.Chinese J Geophys.(in Chinese),2009,52(2):320-328.
[14]王椿镛,Mooney W D,王溪莉等.川滇地区地壳上地幔三维速度结构研究.地震学报,2002,24(1):1-16.Wang C Y,Mooney W D,Wang X L,et al.Study on 3-Dvelocity structure of crust and upper mantle in Sichuan-Yunnan region.China.Acta Seismologica Sinica(in Chinese),2002,24(1):1-16.
[15]韦伟,孙若昧,石耀霖.青藏高原东南缘地震层析成像及汶川地震成因探讨.中国科学(D辑),2010,40(7):831-839.Wei W,Sun R M,Shi Y L.P-wave tomographic imagesbeneath southeastern Tibet:Investigating the mechanism ofthe 2008 Wenchuan earthquake.Sci.China Earth Sci.,2010,53(9):1252-1259,doi:10.1007/sl1430-010.4037-5.
[16]Lei J,Zhao D,Su Y.Insight into the origin of the Tengchongintraplate volcano and seismotectonics in southwest China fromlocal and teleseismic data.J.Geophys.Res.,2009,114,B05302,doi:10.1029/2008JB005881.
[17]何正勤,叶太兰,苏伟.云南地区地壳中上部横波速度结构研究.地球物理学报,2004,47(5):838-844.He Z Q,Ye T L,Su W.S-wave velocity structure of themiddle and upper crust in the Yunnan region.Chinese J.Geophys(in Chinese),2004,47(5):838-844.
[18]Yao H,van der Hilst R D,Montagner J P.Heterogeneityand anisotropy of the lithosphere of SE Tibet from surfacewave array tomography.J.Geophys.Res.,2010,115,B12307,doi:10.1029/2009JB007142.
[19]胡家富,苏有锦,朱雄关等.云南的地壳S波速度与泊松比结构及其意义.中国科学(D辑),2003,33(8):714-722.Hu J F,Su Y J,Zhou X G,et al.S wave velocity of thecrust and the structure of Possion ratio in Yunnan andmeanings.Science in China(Series D)(in Chinese),2003,33(8):714-722.
[20]李永华,吴庆举,田小波等.用接收函数方法研究云南及其邻区地壳上地幔结构.地球物理学报,2009,52(1):67-80.Li Y H,Wu Q J,Tian X B,et al.Crustal structure in theYunnan region determined by modeling receiver functions.Chinese J.Geophys.(in Chinese),2009,52(1):67-80.
[21]徐震,徐鸣洁,王良书等.用接收函数Ps转换波研究地壳各向异性:以哀牢山—红河断裂带为例.地球物理学报,2006,49(2):438-448.Xu Z,Xu M J,Wang L S,et al.A study on crustalanisotropy using P to S converted phase of the receiverfunction:Application to Ailaoshan-Red River fault.ChineseJ.Geophys.(in Chinese),2006,49(2):438-448.
[22]Zhao D,Hasegawa A,Horiuchi S.Tomographic imaging ofP and S wave velocity structure beneath northeastern Japan.J.Geophys.Res.,1992,97(B13):19909-19928.
[23]Zhao D P,Hasegawa A,Kanamori H.Deep structure ofJapan subduction zone as derived from local,regional,andteleseismic events.J.Geophys.Res.,1994,99(B11):22313-22329.
[24]张云湘,骆耀南,杨崇喜.攀西裂谷.北京:地质出版社,1988.Zhang Y X,Luo Y N,Yang C X.The Panxi Rift(inChinese).Beijing:Geological Press,1988.
[25]Chung S L,Jahn B M.Plume-lithosphere interaction ingeneration of the Emeishan flood basalts at the Permian-Triassic boundary.Geology,1995,23(10):889-892.
[26]Xu Y G,Chung S L,Jahn B M,et al.Petrologic andgeochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwestern China.Lithos,2001,58(3-4):145-168.
[27]Xu Y G,He B,Chung S L,et al.Geologic,geochemical,and geophysical consequences of plume involvement in theEmeishan flood-basalt province.Geology,2004,32(10):917-920.
[28]Lo C H,Chung S L,Lee T Y,et al.Age of the Emeishanflood magmatism and relations to Permian-Triassic boundaryevents.Earth P1anet.Sci.Lett.,2002,198(3-4):449-458.
[29]He B,Xu Y G,Chung S L,et al.Sedimentary evidence for arapid Kilometer-scale crustal doming prior to the eruption ofthe Emeishan flood basalts.Earth and Planetary ScienceLetters,2003,213(3-4):391-405.
[30]张招崇,Mahoney J J,王福生等.蛾眉山大火成岩省西部苦橄岩及其共生玄武岩的地球化学:地幔柱头部熔融的证据.岩石学报,2006,22(6):1538-1552.Zhang Z C,Mahoney J J,Wang F S,et al.Geochemistry ofpicritic an d associated basalt flows of the western Emeishanflood basalt province,Chin8:evidence for a plume-headorigin.Acta Petrologica Sinica(in Chinese),2006,22(6):1538-1552.
[31]Li J,Xu J F,Suzuki K,et al.Os,Nd and Sr isotope andtrace element geochemistry of the Muli picrites:Insights intothe mantle source of the Emeishan Large Igneous Province.Lithos,2010,119(1-2):108-122.
[32]Zhou M F,Robinson P T,Michaellesher C,et al.Geochemistry,Petrogenesis and metallogenesis of the Panzhihuagabbroic layered intrusion and associated Fe-Ti-V oxide deposits,Sichuan Province,SW China.Journal of Petrology,2005,46(11):2253-2280.
[33]Christensen N I,Mooney W D.Seismic velocity structureand composition of the continental crust:A global view.J.Geophys.Res.,1995,100(B6):9761-9788.
[34]Stadtlander R,Mechie J,Schulze A.Deep structure of thesouthern Ural mountains as derived fromwide-angle seismicdata.Geophys.J.Int.,1999,137(2):501-515.
[35]徐锡伟,程国良,于贵华等.川滇菱形块体顺时针转动的构造学与古地磁学证据.地震地质,2003,25(1):61-70.Xu X W,Cheng G L,Yu G H,et al.Tectonic andpaleomagnetic evidence for the clockwise rotation of theSichuan-Yunnan rhombic block.SeismologyandGeology(inChinese),2003,25(1):61-70.
[36]何宏林,方仲景,李坪.小江断裂带西支断裂南段新活动初探.地震研究,1993,6(3):291-298.He H L,Fang Z J,Li P.A preliminary approach to the faultactivity of southern segment on Xiaojiang west branch fault.J.Seism.Res.(in Chinese),6(3):291-298.
[37]闻学泽,杜方,龙锋等.小江和曲江-石屏两断裂系统的构造动力学与强震序列的关联性.中国科学(D辑),2011,41(5):713-724.Wen X Z,Du F,Long F,et al.Tectonic dynamics andcorrelation of major earthquake sequences of the Xiaojiangand Qujiang-Shiping fault systems,Yunnan,China.Sci.China Earth Sci.,2011,54(10):1563-1575,doi:10.1007/s11430-011-4231-0.
[38]Shen Z K,Zhao C K,Yin A,et al.Contemporary crustaldeformation in east Asia constrained by Global PositioningSystem measurements.J.Geophys.Res.,2000,105(B3):5721-5734.
[39]Wang E,Burchfiel B C,Royden L H,et al.Late CenozoicXianshuihe-Xiaojiang,Red River,and Dali Fault Systems ofsouthwestern Sichuan and central Yunnan,China.Geol.Soc.Amer.,1998,327:1-108.
[40]常利军,王椿镛,丁志峰.云南地区SKS波分裂研究.地球物理学报,2006,49(1):197-204.Chang L J,Wang C Y,Ding Z F.A study on SKS splittingbeneath the Yunnan region.Chinese J.Geophys.(in Chinese),2006,49(1):197-204.
[41]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),2007,37(4):495-503.Wang C Y,Chang L J,LüZ Y,et al.Seismic anisotropy ofupper mantle in eastern Tibetan Plateau and related crust-mantle coupling pattern.Science in China(Series D),2007,50(8):1150-1160.
[42]吴建平,明跃红,王椿镛.云南地区中小地震震源机制及构造应力场研究.地震学报,2004,26(5):457-465.Wu J P,Ming Y H,Wang C Y.Source mechanism of smallto moderate earthquakes and tectonic stress field in YunnanProvince.Acta Seismologica Sinica(in Chinese),2004,26(5):457-465.
[43]汪集旸,黄少鹏.中国大陆地区大地热流数据汇编.地质科学,1988,(2):196-204.Wang J Y,Huang S P.Compilation of heat flow data in theChina continental area.Scientia Geologica Sinica(in Chinese),1988,(2):196-204.
[44]汪集旸,黄少鹏.中国大陆地区大地热流数据汇编(第二版).地震地质,1990,12(4):351-366.Wang J Y,Huang S P.Compilation of heat flow data in theChina continental area(2nd Edition).Seismology and Geology(in Chinese),1990,12(4):351-366.
[45]徐青,汪缉安,汪集旸等.云南大地热流及其大地构造意义.大地构造与成矿学,1992,16(3):285-299.Xu Q,Wang J A,Wang J Y,et al.Terrestrial heat flow andits tectonic significance in Yunnan,China.Geotectonica etMetallogenia(in Chinese),1992,16(3):285-299.
[46]周真恒,韩新民,周瑞琦.云南腾冲地区的岩石圈热结构.地震地磁观测与研究,1996,17(4):34-41.Zhou Z H,Han X M,Zhou R Q.Geothermal structure oflithosphere in Tengchong region,Yunnan province.Seismologicaland Geomagnetic Observation and Research(in Chinese),1996,17(4):34-41.
[47]胡圣标,何丽娟,汪集旸.中国大陆地区大地热流数据汇编(第三版).地球物理学报,2001,44(5):611-626.Hu S B,He L J,Wang J Y.Compilation of heat flow data inthe China continental area(3rd edition).Chinese J.Geophys.(in Chinese),2001,44(5):611-626.
[48]袁玉松,马永生,胡圣标等.中国南方现今地热特征.地球物理学报,2006,49(4):1118-1126.Yuan Y S,Ma Y S,Hu S B,et al.Present-day geothermalcharacteristics in South China.Chinese J.Geophys.(in Chinese),2006,49(4):1118-1126.