引文
刘国栋主编.临汾地区地壳构造及其动力学研究.国家地震局地质所,1991.
[1] MA Xingyuan.TheLithosphereGeodynamicsCompendiuminChina[M].Beijing:GeologicalPublishingHouse,1987:76(inChinese).
[2] MA Xingyuan,SU Jian.Taphrogenesis through the geolog ical history ofChina[A].Research onRecentCrustalMove ment(I)—ContinentalRifts andDeepInternalProcesses[M].Beijing:SeismologicalPress,1985:516(inChinese).
[3] XING Jishan,YAO Dianqun,LI Ming, et al.The structurefeatures ofShanxi rift valley resulted from geophysical data[J].ShanxiGeology,1989,14(2):95109(inChinese).
[4] XING Jishan,YE Zhiguang,SUN Zhenguo, et al.Shanxi in nerplate structure and its evolvement[J].ShanxiGeology,1991,6(1):315(inChinese).
[5] YANG Weiran,SUN Jiyuan,JI Kecheng, et al.ComparisonofContinentalRiftValley[M].Wuhan:ChinaUniversityofGeosciencesPress,1996(inChinese).
[6] WERNICKE B.Low angle normal faults in theBasin andRange province:Nappe tectonics in an extending oregon[J].Nature,1981,291:65648.
[7] WERNICKE B,BURCHFIEL B.Models of extensional tec tonics[J].JournalStructural ofGeology,1982,4:105115.
[8] WERNICKE B.Uniform sense normal simple shear of thethe continental lithosphere[J].CanJ EarthSci,1985,22:108125.
[9] LIU Hefu,LIANG Huishe,LI Xiaoqing, et al.The couplingmechanisms ofMesozoic cenozoic rift basins and extensionalmountain system inEasternChina[J].EarthScienceFron tiers,2000,7(4):477486(inChinese).
[10] LIU Hefu.Geodynamic scenario of coupled basin and moun tain system[J].EarthScience—Journal ofChinaUniversityofGeosciences,2001,26(6):581596(inChinese).
[11] ZHONG Dalai,DING Lin,JI Jianqing, et al.Coupling of thelithosphere convergence ofWestChina and dispersion ofEastChina inCenozoic:Link with paleoenvironmental changes[J].QuaternarySciences,2001,21(4):302312( inChi nese).
[12] MCKENZIE D P.Some remarks on the development of sedi mentary basins[J].Earth andPlanetarySciLett,1978,40:2532
[13] ROYDEN L.A simple method for analyzing subsidence andheat flow in extensional basins[A].BURRUS JeanTher malModeling inSedimentaryBasins[M].Paris:Technip,1986:4973
[14] SHANG Yuequan,LI Kewu,XU Jin.Problems of mechanicsonWeihe fault basin[J].TheChineseJournal ofGeologicalHazard andControl,1994,5(2):6570.
[15] GREEN P F,DUDDY I K,GLEADOW A J W, et al.Ther mal annealing of fission tracks in apatite,1, a qualitative de scription[J].ChemGeol,1986,59:237253
[16] WAN Jinglin,LI Qi,WANG Yu.The fission track evidenceofHuashan batholith uplifting inMesozoicCenozoic[J ].Seismology andGeology,2000,22(1):5358(inChinese)
[17] YIN Gongming,LU Yanzhou,ZHAO Hua, et al.The tec tonic uplift of theHuaShan in theCenozoic[J].ChineseBul letin,2001,46(13):11211123(inChinese).
[18] LIU Hujun.Tectonic uplift of theCenozoic era in theQinlingrange[J].Journal ofShanxiNormalUniversity,2002,30(1):121124(inChinese).
[19] TENG Zhihong,WANG Xiaohong.Studies of tectonic upliftat theCenozoic era and the regionally environmental effects intheQinling orogenic belt[J].Geology ofShanxi,1996,14(2):3342(inChinese).
[20] WU Chen.Changes of river system and new tectonic move ment in northChina mountainous area[J ].NorthChinaEarthquakeSciences,2001,19(4):16(inChinese).
[21] FEI Qi.A preliminary research into the plate collision, rota tion and divergence pattern ofChina and its periphery sinceMesozoic[J].EarthScience,1987,12(5):463475(inChi nese).
[22] ZHANG Jian,SHI Yaolin.Thermodynamics mechanism ofthe marginal extensional belt ofEastAsia[J].Geotectonic etMetallogenia,2003,27(3):222227(inChinese).
[23] WAN Tianfeng.TheTectonicsCompendium inChina[M].Beijing:GeologicalPublishingHouse,2004:387( inChi nese).
[24] AN Meijian,LI Fangquan.Present structure stress field ofShanxi rift valley system[J].ActaSeismologicaSina,1998,20(5):461465(inChinese).
[25] YANG Guohua,HAN Yueping,ZHOU Xiaoyan.New fea tures ofCrustal motion inNorthChina[J].Journal ofGeod esy andGeodynamics,2002,22(3):2833(inChinese).
[26] WANG Xiuwen,GUO Yuehong,FAN Xuefang.Analysis ofrecent vertical deformation inShanxi area[J].CrustalDe form andEarthquake,2001,1(2):6469(inChinese).
[27] LIU Futian,QU Kexin,WU Hua, et al.ST image ofNorthChina[J]Journal ofGeophys,1986,5:442(inChinese).
[28] HE Yongnian,LIN Chuanyong,SHI Lanbin.The rheologi cal features of mantle derived xenoliths:Evidence for the riftnature ofNorthChina region[A].Research onRecentCrus talMovement(I)—ContinentalRifts andDeepInternalProcesses[M].Beijing:SeismologicalPress,1985:4149(inChinese).
[29] LIU Ruoxin,MA Baolin.The sequence of rocks and physicalproperties in uppermost mantle beneathNorthChina[A].Proceeding ofChinaUpperMantleFeatures andItsDy namic[C].Beijing:SeismologicalPress,1990:17( inChi nese).
[30] CHEN Xiaode,LIN Chuanyong,ZHANG Xiao ou, et al.Deformation features of mantle xenoliths fromQuarter narybasalts inDatong,ShanxiProvince and their rheological im plication[J].Seismology andGeology,1997,19(4):313319(inChinese).
[31] LIN Chuanyong,SHI Lanbin,CHEN Xiaode, et al.Deform ation features of mantle xenoliths from paleogene basalts inEasternChina and their implication of upper mantle rheology[J].ActaPetrologica etMineralogica,1995,14(4):302312(inChinese).
[32] ZHANG Shuliang,LI Dongmei,MA ZhaohuiThe influenceof hydrothermal body on strong earthquake activity along theShanxi seismic belt[J]Earthquake,2002,22(1):8490(inChinese)
[33] ZHAO Yonggui,WANG Sijing,LIU Jianhua, et al.Struc ture characteristics of crust and lower lithosphere inDabieorogen[A].Geotectonic andResource[M]Beijing:OceanPress,1993:3240(inChinese)
[34] WANG Jiyang.Compilation of theChinese continental geo thermal value data[J].Seismology andGeology,1990,12(4):351(inChinese).
[35] XING Jishan,LIU Jianhua,ZHAO Jinquan.Deep seatedtectonics in theNorth intraplate[J].EarthquakeResearch inShanxi,2002,111(4):312(inChinese).
[1] 马杏垣.中国岩石圈动力学纲要[M]北京:地质出版社,1987:76.
[2] 马杏垣,宿俭中国地质历史过程中的裂陷作用[A].现代地壳运动研究(I)———大陆裂谷与深部过程[M]北京:地震出版社,1985:516.
[3] 邢集善,姚典群,黎明,等试从地球物理资料论山西地堑系的构造特征[J]山西地质,1989,4(2):95109
[4] 邢集善,叶志光,孙振国,等山西板内构造及其演化特征初探[J]山西地质,1991,6(1):315
[5] 杨巍然,孙继源,纪克诚,等大陆裂谷对比[M]武汉:中国地质大学出版社,1996.
[9] 刘和甫,梁慧社,李晓清,等中国东部中新生代裂陷盆地与伸展山岭耦合机制[J]地学前缘,2000,7(4):477486.
[10] 刘和甫盆地山岭耦合体系与地球动力学机制[J]地球科学,2001,26(6):581596.
[11] 钟大赉,丁林,季建清,等中国西部新生代岩石圈汇聚和东部岩石圈离散的耦合关系与古环境格局演变的探讨[J]第四纪研究,2001,21(4):302312.
[14] 尚岳全,黎克武,徐进渭河断陷盆地形成过程中的力学问题[J]中国地质灾害与防治学报,1994,5(2):6570
[16] 万景林,李齐,王瑜.华山岩体中、新生代抬升的裂变径迹证明[J]地震地质,2000,22(1):5358.
[17] 尹功明,卢演俦,赵华,等.华山新生代构造抬升[J].科学通报,2001,46(13):11211123.
[18] 刘护军.秦岭新生代构造隆升研究[J]陕西师大学报(自然科学),2002,30(1):121124.
[19] 藤志宏,王晓红.秦岭造山带新生代构造隆升与区域环境效应研究[J]陕西地质,1996,14(2):3342.
[20] 吴忱.华北山地的水系变迁与新构造运动[J]华北地震科学,2001,19(4):16.
[21] 费琪.中新生代中国及邻区板块碰撞、旋转及离散模式初探[J]地球科学,1987,12(5):463475.
[22] 张建,石耀霖.东亚陆缘带构造扩张的深部热力学机制[J]大地构造与成矿学,2003,27(3):222227.
[23] 万天丰.中国大地构造学纲要[M]北京:地质出版社,2004:387.
[24] 安美建,李方全.山西地堑系现今构造应力场[J]地震学报,1998,20(5):461465.
[25] 杨国华,韩月萍,周晓燕.华北地壳运动新特征[J]大地测量与地球动力学,2002,22(3):2833.
[26] 王秀文,郭跃宏,范雪芳.山西地区近期垂直形变场分析[J]地壳形变与地震荡,2001,1(2):6469.
[27] 刘福田,曲克信,吴华,等.华北地区的地震层析成像[J]地球物理学报,1986,5:442.
[28] 何永年,林传勇,史兰斌从幔源包体的流变学特征看我国华北地区裂谷性质[A]现代地壳运动研究(I)———大陆裂谷与深部过程[M]北京:地震出版社,1985:4149.
[29] 刘若新,马宝林.华北地区地幔最上部岩石物性分层[A]中国上地幔特征及动力学论文集[C]北京:地震出版社,1990:17.
[30] 陈孝德,林传勇,张小鸥,等.山西大同第四纪火山岩中幔源包体的变形特征及其上地幔流变学意义[J]地震地质,1997,19(4):313319.
[31] 林传勇,史兰斌,陈孝德,等.中国东部早第三纪玄武岩中幔源包体的变形特征及其上地幔流变学意义[J]岩石矿物学杂志,1995,14(4):302312.
[32] 张淑亮,李冬梅,马朝晖山西地震带热流体对强震活动影响[J]地震,2002,22(1):8490
[33] 赵永贵,王思敬,刘建华,等.大别造山带的地壳和下岩石圈构造特征[A]大地构造与资源[M]北京:海洋出版社,1993:3240
[34] 汪集.中国大陆地区大地热流值数据汇编[J]地震地质,1990,12(4):351
[35] 邢集善,刘建华,赵晋泉.华北板内深部构造[J]山西地震,2002,111(4):312.