引文
方盛明,赵成彬,柴炽章,等.2009.银川断陷盆地地壳结构与构造的地震学证据[J].地球物理学报,52(7):1768—1775.FANG Sheng-ming,ZHAO Cheng-bin,CHAI Chi-zhang,et al.2009.Seismic evidence of crustal structures in theYinchuan faulted basin[J].Chinese Journal of Geophysics,52(7):1768—1775(in Chinese).
国家地震局地质研究所,宁夏回族自治区地震局.1990.海原断裂带[M].北京:地震出版社.Institute of Geology,China Earthquake Administration,Earthquake Bureau of Ningxia Hui Autonomous Region.1990.The Haiyuan Fault Zone[M].Seismological Press,Beijing(in Chinese).
国家地震局“鄂尔多斯周缘断裂系”课题组.1988.鄂尔多斯周缘活动断裂系[M].北京:地震出版社.39—285.Research Group on Active Fault Systems around the Ordos Massif,State Seismological Bureau.1988.Active FaultSystems around the Ordos Massif[M].Seismological Press,Beijing.39—285(in Chinese).
李传友.2005.青藏高原东北部几条主要断裂带的定量研究[D]:[学位论文].北京:中国地震局地质研究所.76—101.LI Chuan-you.2005.Quantitative studies on major active fault zones in northeastern Qinghai-Tibet Plateau[D].Dissertation.Institute of Geology,China Earthquake Administration,Beijing.76—101(in Chinese).
李吉均,方小敏,马海洲,等.1996.晚新生代黄河上游地貌演化与青藏高原隆起[J].中国科学(D),26(4):316—322.LI Ji-jun,FANG Xaio-min,MA Hai-zhou,et al.1996.Geomorphological and environmental evolution in the upperreaches of the Yellow River during the late Cenozoic[J].Science in China(Ser D),39(4):380—390.
闵伟,柴炽章,王萍,等.1992.罗山东麓断裂全新世活动特征的初步研究[J].中国地震,8(4):49—54.MIN Wei,CHAI Chi-zhang,WANG Ping,et al.1992.Preliminary study on the Holocene active fault features at theeastern piedmont of the Luoshan Mountain[J].Earthquake Research in China,8(4):49—54(in Chinese).
宁夏回族自治区地质矿产局.1996.宁夏回族自治区岩石地层(全国地层多重划分对比研究64)[M].北京:中国地质大学出版社.Bureau of Geology and Mineral Resources of Ningxia Hui Autonomous Region.1996.Strata of the Ningxia HuiAutonomous Region(Strata Correlation of China64)[M].Geological Publishing House,Beijing(in Chinese).
任纪舜,姜春发,张正坤,等.1980.中国大地构造及其演化[M].北京:科学出版社.10—65.REN Ji-shun,JIANG Chun-fa,ZHANG Zheng-kun,et al.1980.Geotectonic Evolution of China[M].Science Press,Beijing.10—65(in Chinese).
任文军,张庆龙,张进,等.1999.鄂尔多斯盆地中央古隆起板块构造成因初步研究[J].大气构造与成矿,23(2):191—196.REN Wen-jun,ZHANG Qing-long,ZHANG Jin,et al.1999.The plate tectonic formation of the central paleouplift in theOrdos Basin[J].Geotectonica et Metallogenia,23(2):191—196.
汤锡元,郭忠铭.1992.陕甘宁盆地西缘逆冲推覆构造及油气勘探[M].西安:西北大学出版社.TANG Xi-yuan,GUO Zhong-ming.1992.The Thrusting Tectonics in the West Margin of Shanganning Basin and thePetroleum Exploration[M].Northeast University Press,Xi'an(in Chinese).
田勤俭,丁国瑜,申旭辉.2002.青藏高原东北隅强震构造模型[J].地震,22(1):9—16.TIAN Qin-jian,DING Guo-yu,SHEN Xu-hui,et al.2002.Seismic tectonic model of the northeastern corner of the TibetPlateau[J].Earthquake,22(1):9—16(in Chinese).
王伟涛,张培震,张广良,等.2010.青藏高原东北缘寺口子盆地新生代沉积演化及其构造意义[J].地质科学,45(2):440—452.WANG Wei-tao,ZHANG Pei-zhen,ZHANG Guang-liang,et al.2010.Cenozoic sedimentary evolution of the SikouziBasin on the northeastern margin of the Qinghai-Tibetan plateau and its tectonic significance[J].Chinese Journalof Geology,45(2):440—452(in Chinese).
王志才,张培震,张广良,等.2006.西秦岭北缘构造带的新生代构造活动:兼论对青藏高原东北缘形成过程的指示意义[J].地学前缘,13(4):119—135.WANG Zhi-cai,ZHANG Pei-zhen,ZHANG Guang-liang,et al.2006.Tertiary tectonic activities of the north frontal faultzone of the west Qinling Mountains:Implications for the growth of the northeastern margin of the Qinghai-Tibetanplateau[J].Earth Science Frontiers,13(4):119—135(in Chinese).
徐锡伟,Tapponnier P,Van Der Woerd J,等.2003.阿尔金断裂带晚第四纪左旋走滑速率及其构造运动转换模式讨论[J].中国科学(D),33(10):967—974.XU Xi-wei,Tapponnier P,Van Der Woerd J,et al.2003.Pattern of latest tectonic motion and its dynamics for activeblocks in Sichuan-Yunnan region,China[J].Science in China(Ser D),33(10):967—974(in Chinese).
袁道阳,张培震,刘百篪,等.2004.青藏高原东北缘晚第四纪活动构造的几何图像与构造转换[J].地质学报,78(2):270—278.YUAN Dao-yang,ZHANG Pei-zhen,LIU Bai-chi,et al.2004.Geometrical imagery and tectonic transformation of lateQuaternary active tectonics in northeastern margin of Qinghai-Xizang Plateau[J].Acta Geologica Sinica,78(2):270—278(in Chinese).
袁道阳,张培震,雷中生,等.2005.青海拉脊山断裂带新活动特征的初步研究[J].中国地震,21(1):93—102.YUAN Dao-yang,ZHANG Pei-zhen,LEI Zhong-sheng,et al.2005.A preliminary study on the new activity features ofthe Lajishan Mountain Fault zone in Qinghai Province[J].Earthquake Research in China,21(1):93—102(inChinese).
袁道阳,张培震,方小敏,等.2007.青藏高原东北缘临夏盆地晚新生代构造变形及过程[J].地学前缘,14(1):243—250.YUAN Dao-yang,ZHANG Pei-zhen,FANG Xiao-min,et al.2007.Late Cenozoic tectonic deformation of the LinxiaBasin,northeastern margin of the Qinghai-Tibet Plateau[J].Earth Science Frontiers,14(1):243—250(inChinese).
詹艳.2008.青藏高原东北缘地区深部电性结构特征及构造涵义[D]:[学位论文].北京:中国地震局地质研究所.76—101.ZHAN Yan.2008.Deep electric structures beneath the northeastern margin of the Tibetan plateau and its tectonicimplications[D].Dissertation.Institute of Geology,China Earthquake Administration,Beijing,76—101(inChinese).
张进,马宗晋,任文军.2005.宁夏中南部新生界沉积特征及其与青藏高原演化的关系[J].地质学报,79(6):757—773.ZHANG Jin,MA Zong-jin,REN Wen-jun.2005.The sedimentary characteristics of Cenozoic strata in central andsouthern Ningxia and their relationships with the development of the Qinghai-Tibetan plateau[J].Acta GeologicaSinica,79(6):757—773(in Chinese).
张进,马宗晋,任文军.2006.试论宁夏地区始新统寺口子组沉积的构造背景[J].地质论评,52(2):207—214.ZHANG Jin,MA Zong-jin,REN Wen-jun.2006.Discussion on the tectonic setting of deposition of the Eocene SikouziFormation in Ningxia region[J].Geological Review,52(2):207—214(in Chinese).
郑德文,张培震,万景林,等.2003.青藏高原东北边缘晚新生代构造变形的时序:临夏盆地碎屑颗粒磷灰石裂变径迹记录[J].中国科学(D),33(B04):190—198.ZHENG De-wen,ZHANG Pei-zhen,WAN Jin-lin,et al.2003.Late Cenozoic deformation subsequence in northeasternmargin of Tibet:Detrital AFT records from Linxia Basin[J].Science in China(Ser D),33(B04):190—198(inChinese).
郑德文,张培震,万景林,等.2005.六盘山盆地热历史的裂变径迹证据[J].地球物理学报,48(1):157—164.ZHENG De-wen,ZHANG Pei-zhen,WAN Jin-lin,et al.2005.Apatite fission track evidence for the thermal history ofthe Liupanshan Basin[J].Chinese Journal of Geophysics,48(1):157—164(in Chinese).
Burchfiel B C,Deng Q D,Molnar P,et al.1989.Intracrustal detachment within zones of continental deformation[J].Geology,17(8):748—752.
Burchfiel B C,Zhang P,Wang Y,et al.1991.Geology of the Haiyuan Fault zone,Ningxia Hui Autonomous Region,China,and its relation to the evolution of the northeastern margin of the Tibetan plateau[J].Tectonics,10(6):1091—1110.
Fang X,Garzione C,Van der Voo R,et al.2003.Flexural subsidence by29Ma on the NE edge of Tibet from themagnetostratigraphy of Linxia Basin,China[J].Earth and Planetary Science Letters,210:545—560.
Fang X,Yan M,Van der Voo R,et al.2005.Late Cenozoic deformation and uplift of the NE Tibetan plateau:Evidencefrom high-resolution magnetostratigraphy of the Guide Basin,Qinghai Province,China[J].Geological Society ofAmerica Bulletin,117(9-10):1208—1225.
Fang X,Zhang W,Meng Q,et al.2007.High-resolution magnetostratigraphy of the Neogene Huaitoutala section in theeastern Qaidam Basin on the NE Tibetan plateau,Qinghai Province,China and its implication on tectonic uplift ofthe NE Tibetan plateau[J].Earth and Planetary Science Letters,258:293—306.
Lease R O,Burbank D W,Gehrels G E,et al.2007.Signatures of mountain building:Detrital zircon U/Pb ages fromnortheastern Tibet[J].Geology,35(3):239—242.
Lease R O,Burbank D W,Hough B,et al.2012.Pulsed Miocene range growth in northeastern Tibet:Insights from Xunhua Basin magnetostratigraphy and provenance[J].Geological Society of America Bulletin,124:657—677.
Li C,Zhang P Z,Yin J,et al.2009.Late Quaternary left-lateral slip rate of the Haiyuan Fault,northeastern margin of theTibetan plateau[J].Tectonics,28(TC5010):1—26.
Métivier F,Gaudemer Y,Tapponnier P,et al.1998.Northeastward growth of the Tibet Plateau deduced from balancedreconstruction of two depositional areas:The Qaidam and Hexi Corridor Basins,China[J].Tectonics,17:823—842.
Meyer B,Tapponnier P,Bourjot L,et al.1998.Crustal thickening in Gansu-Qinghai,lithospheric mantle subduction,andoblique,strike-slip controlled growth of the Tibet Plateau[J].Geophysical Journal International,135:1—47.
Molnar P.2005.Mio-Pliocene growth of the Tibetan plateau and evolution of East Asian climate[J].PalaeontologiaElectronica,8:1—23.
Molnar P,Boos W R,Battisti D S.2010.Orographic controls on climate and paleoclimate of Asia:Thermal andmechanical roles for the Tibetan plateau[J].Annual Review of Earth and Planetary Sciences,38:77—102.
Tapponnier P,Xu Z Q,Roger F,et al.2001.Oblique stepwise rise and growth of the Tibet Plateau[J].Science,2(5547):1671—1677.
Wang Q,Zhang P Z,Freymueller J F,et al.2001.Present-day crustal deformation in China constrained by globalpositioning system measurements[J].Science,294:574—577.
Wang W,Kirby E,Zhang P,et al.2013.Tertiary basin evolution along the northeastern margin of the Tibetan plateauEvidence for basin formation during Oligocene transtension[J].Geological Society of America Bulletin,1421113—1137.
Wang W T,Zhang P Z,Kirby E,et al.2011.A revised chronology for Tertiary sedimentation in the Sikouzi Basin:Implications for the tectonic evolution of the northeastern corner of the Tibetan plateau[J].Tectonophysics,505:100—114.
Zhang J,Cunningham D,Chen H Y,et al.2010.Sedimentary characteristics of Cenozoic strata in central-southernNingxia,NW China:Implications for the evolution of the NE Qinghai-Tibetan plateau[J].Journal of Asian EarthSciences,39:740—749.
Zhang P Z,Burchfiel B C,Molnar P,et al.1990.Late Cenozoic tectonic evolution of the Ningxia-Hui AutonomousRegion,China[J].Geological Society of America Bulletin,102:1484—1498.
Zhang P Z,Burchfel B C,Molnar P,et al.1991.Amount and style of late Cenozoic deformation in the Liupan Shanarea,Ningxia Autonomous Region,China[J].Tectonics,10(6):1111—1129.
Zhang P Z,Molnar P,Burchfiel B C,et al.1988.Bounds on the Holocene slip rate along the Haiyuan Fault,north-central China[J].Quaternary Research,30:151—164.
Zhang P Z,Molnar P,Xu X.2007.Late Quaternary and present-day rates of slip along the Altyn Tagh Fault,northernmargin of the Tibetan plateau[J].Tectonics,26(TC5010):1—24.
Zhang P Z,Shen Z K,Wang M,et al.2004.Continuous deformation of the Tibetan plateau from global positioning systemdata[J].Geology,32(9):809—812.
Zheng D,Zhang P,Wan J L,et al.2006.Rapid exhumation at~8Ma on the Liupan Shan thrust fault from apatitefission-track thermochronology:Implications for growth of the northeastern Tibetan plateau margin[J].Earth andPlanetary Science Letters,248:198—208.