西秦岭北缘断裂带漳县—车厂断层的结构及构造演化
|
摘要
西秦岭北缘断裂带是青藏高原东北缘主要构造边界断裂带之一,其构造变形历史和运动学特征研究可以为西秦岭中新生代构造过程和印度—亚洲板块碰撞动力学的远程构造响应提供约束。漳县—车厂断层是西秦岭北缘断裂带的重要组成部分,通过对工程开挖所揭露的断层带内丰富构造现象的观测与分析,至少可以辨别出3期性质、规模、运动学特征各异的构造变形事件。第一期为向北北东陡倾的伸展正断层作用;第二期为向南南西倾的由南向北的逆冲断层作用;第三期为沿近直立断面左旋走滑作用。尽管每期变形的时代尚缺乏构造物质测年的约束,但根据其与白垩系、新近系的空间关系以及已有第四纪以来沿断层地貌位错和相关沉积物测年以及地震活动历史研究对断层左旋走滑作用的时代约束,认为第一期伸展正断层作用起始于早白垩纪,可能持续到渐新世;第二期向北逆冲断层作用起始于渐新世初,可能持续到早第四纪;第三期左旋走滑断层作用起始于晚第四纪,持续至今。漳县—车厂断层是一条典型的多期变形的脆性断层,其变形特征与历史,如果代表了西秦岭北缘断裂带特征与构造变形过程,那么现今西秦岭北缘断裂带仅是起始于早白垩纪、新生的脆性断裂带,并非是印支主造山期大规模韧性逆冲推覆作用的边界断层。
The north margin fault zone of West Qinling is one of the tectonic boundary faults and earthquake faults in the northeast margin of Tibetan plateau. Its structural characteristics and deformation history can provide important constraints on the Mesozoic-Cenozoic tectonic processes of West Qinling and the remote tectonic responses to the Indian-Europe plate collisions. Based upon the tectonic observation and analysis of Zhangxian-Chechang fault zone which was uncovered by engineering construction and is located in the central segment of the north margin faults of West Qinling, the authors identified three phases of deformation events with different properties, scales, and kinematics. The first event is characterized by steep NNE-dipping extensional normal faulting. According to the relationship between Cretaceous red bed basin and the fault, it is suggested that this normal faulting event documented the Cretaceous regional crustal extension and development of the red bed basin. The fault gouge with a lot of grinding gravels and well-developed faulting foliations indicates its longduration, probably lasting to the Late Oligocene, i.e., 29 Ma when Linxia basin began developing. The second event is characterized by south-dipping inverse faulting, which led to the folding and thrusting of the Cretaceous red bed strata, possibly indicating the transition from crustal extension to contraction. This tectonic transition probably suggests that the India-Europe plate collision might have been spread to West Qinling, and strong thrusting should have occurred at 3.6 Ma when Jishishan and Wuquanshan conglomerates occurred. The third event is characterized by sinistral strike-slipping along the nearly vertical NNW-striking fault plane, which began in Late Quaternary and has continued up till now. Zhangxian-Chechang fault as one of the north margin faults of West Qinling is a typical brittle fault, which failed to document the large-scale ductile shearing in Indochina orogeny. Therefore it is held that the north margin fault zone of West Qinling, which has been generally believed to be the tectonic boundary fault between the Central Qinling and North Qinling or Central Qilian Block, is a newly generated fault from the Cretaceous instead of the boundary fault in the Indochina orogeny.
The north margin fault zone of West Qinling is one of the tectonic boundary faults and earthquake faults in the northeast margin of Tibetan plateau. Its structural characteristics and deformation history can provide important constraints on the Mesozoic-Cenozoic tectonic processes of West Qinling and the remote tectonic responses to the Indian-Europe plate collisions. Based upon the tectonic observation and analysis of Zhangxian-Chechang fault zone which was uncovered by engineering construction and is located in the central segment of the north margin faults of West Qinling, the authors identified three phases of deformation events with different properties, scales, and kinematics. The first event is characterized by steep NNE-dipping extensional normal faulting. According to the relationship between Cretaceous red bed basin and the fault, it is suggested that this normal faulting event documented the Cretaceous regional crustal extension and development of the red bed basin. The fault gouge with a lot of grinding gravels and well-developed faulting foliations indicates its longduration, probably lasting to the Late Oligocene, i.e., 29 Ma when Linxia basin began developing. The second event is characterized by south-dipping inverse faulting, which led to the folding and thrusting of the Cretaceous red bed strata, possibly indicating the transition from crustal extension to contraction. This tectonic transition probably suggests that the India-Europe plate collision might have been spread to West Qinling, and strong thrusting should have occurred at 3.6 Ma when Jishishan and Wuquanshan conglomerates occurred. The third event is characterized by sinistral strike-slipping along the nearly vertical NNW-striking fault plane, which began in Late Quaternary and has continued up till now. Zhangxian-Chechang fault as one of the north margin faults of West Qinling is a typical brittle fault, which failed to document the large-scale ductile shearing in Indochina orogeny. Therefore it is held that the north margin fault zone of West Qinling, which has been generally believed to be the tectonic boundary fault between the Central Qinling and North Qinling or Central Qilian Block, is a newly generated fault from the Cretaceous instead of the boundary fault in the Indochina orogeny.
引文
曹娟娟,刘百篪,闻学泽.2003.西秦岭北缘断裂带特征地震平均复发间隔的确定和地震危险性评价[J].地震研究,26(4):372-381.
方小敏,李吉均,朱俊杰,陈怀录,曹继秀.1997.甘肃临夏盆地新生代地层绝对年代测定与划分[J].科学通报,42(14):1457-1471.
甘肃省地质调查院.2007.岷县幅1:250000区域地质调查报告[R].兰州:甘肃省地质调查院.
高锐,王海燕,马永生,朱铉,李秋生,李鹏武,匡朝阳,卢占武.2006.松潘地块若尔盖盆地与西秦岭造山带岩石圈尺度的构造关系——深地震反射剖面探测成果[J].地球学报,27(5):411-418.
郭进京,韩文峰,李雪峰,刘寒鹏.2011.汶川8.0级地震断层同震位移的构造意义与运动学模型[J].地质学报,85(3):309-322.
郭进京,韩文峰,李雪峰.2009.西秦岭新生代以来地质构造过程对青藏高原隆升和变形的约束[J].地学前缘,16(6):215-225.
何永年,林传勇,史兰斌.1988.构造岩石学基础[M].北京:地质出版社.
姜晓玮,王江海,张会化.2003.西秦岭断裂走滑与盆地的耦合——西秦岭—松甘块体新生代向东走滑挤出的证据[J].地学前缘,10(2):201-207.
康来迅,张新基,黄杏珍,李立武.1999.西秦岭北缘断裂带排气活动的比较研究[J].地震学报,21(6):657-664.
李传友,张培震,袁道阳,王志才,张剑玺.2006.西秦岭北缘断裂带黄香沟段晚第四纪水平位移特征及其微地貌响应[J].地震地质,28(3):391-404.
李传友,张培震,袁道阳,王志才,郑德文.2010.活动走滑断裂上断塞塘沉积特征及其构造含义——以西秦岭北缘断裂带断塞塘为例[J].地质学报,84(1):90-104.
李传友,张培震,张剑玺,袁道阳,王志才.2007.西秦岭北缘断裂带黄香沟段晚第四纪活动表现与滑动速率[J].第四纪研究,27(1):54-63.
李吉均,方小敏,马海洲,朱俊杰,潘保田,陈怀录.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辑),26(4):316-322.
林爱明.1996.断层岩与断层模式[J].高校地质学报,2(3):295-306.
林爱明.2008.地震化石:假熔岩的形成与保存[M].北京:高等教育出版社.
陕西省地质矿产勘查开发局.1996.秦岭北缘活动断裂带[M].北京:地质出版社.
施炜,张岳桥,董树文.2003.郯庐断裂带中段第四纪活动及其分段特征[J].地球学报,24(1):11-18.
孙岩,韩克从.1985.断裂构造岩带划分[M].北京:科学出版社.
王修喜,李吉均,宋春晖,张军,赵志军,高军平,潘美慧.2006.青藏高原东北缘西秦岭新生代抬升——天水盆地碎屑颗粒磷灰石裂变径迹记录[J].沉积学报,24(6):783-789.
王志才,张培震,张广良,李传友,郑德文,袁道阳.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.
王宗起,闫臻,王涛,高联达,闫全人,陈隽璐,李秋根,姜春发,刘平,张英利,谢春林,向忠金.2009.秦岭造山带主要疑难地层时代研究的新进展[J].地球学报,30(5):561-570.
袁道阳,杨明.1999.西秦岭北缘断裂带的位移累计滑动亏损特征及其破裂分段性研究[J].地震研究,22(4):382-389.
袁道阳,张培震,方小敏,王志才,宋春晖,郑德文.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.
张国伟,郭安林,姚安平.2004.中国大陆构造中西秦岭-松潘大陆构造结[J].地学前缘,11(3):23-32.
张国伟,张本仁,袁学诚,肖庆辉.2001.秦岭造山带与大陆动力学[M].北京:科学出版社.
张秋文,张培震,王乘,ELLIS M A.2004.断层间相互作用的触震与缓震效应定量评价[J].地球学报,25(4):483-488.
张岳桥,马寅生,杨农,张会平,施炜.2005.西秦岭地区东昆仑一秦岭断裂系晚新生代左旋走滑历史及其向东扩展[J].地球学报,26(1):1-8.
郑德文,张培震,万景林,李传友,曹继秀.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),46(S1):266-275.
ALPAR B,YALTTIRAK C.2002.Characteristic features of the North Anatolian Fault in the eastern Marmara region and its tectonic evolution[J].Marine Geology,190(1-2):329-350.
Bureau of Geology and Mineral Recourses Exploration and Devel-opment of Shannxi Province.1996.The north frontal active fault zone of Qinling mountains[M].Beijing:Geological Pub-lishing House(in Chinese).
CAO Juan-juan,LIU Bai-chi,WEN Xue-ze.2003.Determination of the Average Recurrence Intervals of Characteristic Earth-quakes and Estimate of Earthquake Risk on Northern Xiqinling Faults[J].Journal of Seismological Research,26(4):372-381(in Chinese with English abstract).
FANG Xiao-min,LI Ji-jun,ZHU Jun-jie,CHEN Huai-lu,CAO Ji-xiu.1997.Absolute age determination and division of the Cenozoic stratigraphy in the Linxia Basin,Gansu Province,China[J].Chinese Science Bulletin,42(14):1457-1471(in Chi-nese).
Geological Survey of Gansu Province.2007.1:250000Minxian Gregional Gological Surveying Report[R].Lanzhou:Geologi-cal Survey of Gansu Province(in Chinese).
GAO Rui,WANG Hai-yan,MA Yong-sheng,ZHU Xuan,LI Qiu-sheng,LI Peng-wu,KUANG Zhao-yang,LU Zhan-wu.2006.Tectonic Relationships between the ZoigêBasin of the Song-Pan Block and the West Qinling Orogen at Lithosphere Scale:Results of Deep Seismic Reflection Profiling[J].Acta Geoscientica Sinica,27(5):411-418(in Chinese with English abstract).
GUO Jin-jing,HAN Wen-feng,LI Xue-feng,LIU Han-peng.2011.Tectonic Implication of Co-seismic Displacement of Ms8.0Wenchuan Earthquake Fault and Its Kinematic Model[J].Acta Geologica Sinica,85(3):309-322(in Chinese with English ab-stract).
GUO Jin-jing,HAN Wen-feng,LI Xue-feng.2009.The Cenozoic Tectonic Evolution of the West Qinling:Constraints on the Uplift and Deformation of the Tibetan Plateau[J].Earth Sci-ence Frontiers,16(6):215-225(in Chinese with English ab-stract).
HE Yong-nian,LIN Chuan-yong,SHI Lan-bin.1988.Basis of Tec-tonic Petrology[M].Beijing:Geological Publishing House(in Chinese).
JIANG Xiao-wei,WANG Jiang-hai,ZHANG Hui-hua.2003.Cou-pling between strike-slip faults and basins:the evidence for Cenozoic eastward extrusion of the West Qinling-Songgan Block[J].Earth Science Frontiers,10(2):201-207(in Chinese with English abstract).
KANG Lai-xun,ZHANG Xin-ji,HUANG Xing-zhen,LI Li-wu.1999.Comparative study on degassing activities along the north fault zone of western Qinling[J].Acta Seismologica Sinica,12(6):716-723.
KOYIGIT A,BEYHAN A.1998.A new intracontinental transcurrent structure:the Central Anatolian Fault Zone,Tur-key[J].Tectonophysics,284(3-4):317-336.
KOYIGIT A,YILMAS A,ADAMIA S,KULOSGVILI S.2001.Neotectonics of East Anatolian Plateau(Turkey)and Lesser Caucasus:Implication for Transition from Thrusting to Strike-Slip Faulting[J].Geodinamica Acta,14(1-3):177-195.
LI Chuan-you,ZHANG Pei-zhen,YUAN Dao-yang,WANG Zhi-cai,ZHANG Jian-xi.2006.Late-Quaternary horizontal displacement and its associated microgeomorphology of the western Qinling Fault Zone at Huangxianggou[J].Seismology and Geology,28(3):391-404(in Chinese with English ab-stract).
LI Chuan-you,ZHANG Pei-zhen,YUAN Dao-yang,WANG Zhi-cai,ZHENG De-wen.2010.Sedimentary characteristics of sag-pond on the active strike slip fault and its tectonic impli-cations:An example from sag pond along the West Qinling Fault[J].Acta Geologica Sinica,84(2):90-104(in Chinese with English abstract).
LI Chuan-you,ZHANG Pei-zhen,ZHANG Jian-xi,YUANDao-yang,WANG Zhi-cai.2007.Late-Quaternary activity and slip rate of the Western Qinling Fault zone at Huangxiang-gou[J].Quaternary Sciences,27(1):54-63(in Chinese with English abstract).
LI Ji-jun,FANG Xiao-min,MA Hai-zhou,ZHU Jun-jie,PAN Bao-tian,CHEN Huai-lu.1996.Geomorphological and envi-ronmental evolution in the upper reaches of the Yellow River during the Late Cenozoic[J].Science in China(Series D),39(4):380-390.
LIN Ai-ming.1996.Fault rocks and faulting model[J].Geological Journal of China Universities,2(3):295-306(in Chinese with English abstract).
LIN Ai-ming.2001.S-C fabrics developed in cataclastic rocks from the Nojima fault zone,Japan and their implications for tec-tonic history[J].Journal of Structural Geology,23(6-7):1167-1178.
LIN Ai-ming.2008.Earthquake fossils pseudotachylytes:genera-tion and preservation[M].Beijing:High Education Press(in Chinese).
PICHA F J.2002.Late orogenic strike-slip faulting and escape tectonics in frontal Dinarides-Hellenides,Croatia,Yugoslavia,Albania,and Greece[J].American Association of Petroleum Geologists Bulletin,86(9):1659-1671.
REID L F,SIMONY P S,ROSS G M.2002.Dextral strike-slip faulting in the Cariboo Mountains,British Columbia:A natural example of wrench tectonics in relation to Cordilleran tecton-ics[J].Canadian Journal of Earth Sciences,39(6):953-970.
SHI Wei,ZHANG Yue-qiao,DONG Shu-wen.2003.Quaternary Activity and Segmentation Behavior of the Middle Portion of the Tan-Lu Fault Zone[J].Acta Geoscientica Sinica,24(1):11-18(in Chinese with English abstract).
SIBSON R H.1977.Fault rocks and fault mechanism[J].Journal of the Geological Society,133(3):191-213.
SNOKE A W,TULLIS J,TODD V R.1998.Fault-related rocks:a photographic atlas[M].New Jersey:Princeton University Press.
SUN Yan,HAN Ke-cong.1985.Division of Fault Rock Zone[M].Beijing:Science Press(in Chinese).
TSUTSUMI H,YEATS R S,HUFTILE G J.2001.Late Cenozoic tectonics of the Northern Los Angeles fault system,Califor-nia[J].Geological Society of America Bulletin,113(4):454-468.
WANG Xiu-xi,LI Ji-jun,SONG Chun-hui,ZHANG Jun,ZHAO Zhi-jun,GAO Jun-ping,PAN Mei-hui.2006.Cenozoic Uplift of West Qinling,Northeast Margin of Tibetan Plateau:The record of detrital apatite fission track data in Tianshui Basin[J].Acta Sedimentologica Sinica,24(6):783-789(in Chinese with English abstract).
WANG Zhi-cai,ZHANG Pei-zhen,ZHANG Guang-liang,LI Chuan-you,ZHENG De-wen,YUAN Dao-yang.2006.Tertiary tectonic activities of the north frontal fault zone of the west Qinling mountains:implications for the growth of the north-eastern margin of the Qinghai-Tibetan Plateau[J].Earth Sci-ence Frontiers,13(4):119-135(in Chinese with English ab-stract).
WANG Zong-qi,YAN Zhen,WANG Tao,GAO Lian-da,YAN Quan-ren,CHEN Jun-lu,LI Qiu-gen,JIANG Chun-fa,LIU Ping,ZHANG Ying-li,XIE Chun-lin,XIANG Zhong-jin.2009.New Advances in the Study on Ages of Metamorphic Strata in the Qinling Orogenic Belt[J].Acta Geoscientica Sinica,30(5):561-570(in Chinese with English abstract).
YUAN Dao-yang,YANG Ming.1999.Research on the features of displacement cumulative slip deficits and segmentation in the northern margin fault zone of the western Qinling[J].Journal of Seismological Research,22(4):382-389(in Chinese with English abstract).
YUAN Dao-yang,ZHANG Pei-zhen,FANG Xiao-min,WANG Zhi-cai,SONG Chun-hui,ZHENG De-wen.2007.Late Ceno-zoic tectonic deformation of the Linxia Basin,northeastern margin of the Qinghai-Tibet Plateau[J].Earth Science Fron-tiers,14(1):243-250(in Chinese with English abstract).
ZHANG Guo-wei,GUO An-lin,YAO An-ping.2004.Western Qinling-Songpan continental tectonic node in China’s conti-nental tectonics[J].Earth Science Frontiers,11(3):23-32(in Chinese with English abstract).
ZHANG Guo-wei,ZHANG Ben-ren,YUAN Xue-cheng,XIAO Qing-hui.2001.Qinling Continental Orogenic Belt and Continen-tal Dynamics[M].Beijing:Science Press(in Chinese).
ZHANG Qiu-wen,ZHANG Pei-zhen,WANG Cheng,ELLIS M A.2004.Interaction of Active Faults and Its effect on Earthquake Triggering and Delaying[J].Acta Geoscientica Sinica,25(4):483-488(in Chinese with English abstract).
ZHANG Yue-qiao,MA Yin-sheng,YANG Nong,ZHANG Hui-ping,SHI Wei.2005.Late Cenozoic Left-slip Faulting Process of the East Kunlun-Qinling Fault System in West Qinling Region and Its Eastward Propagation[J].Acta Geoscientica Sinica,26(1):1-8(in Chinese with English abstract).
ZHENG De-wen,ZHANG Pei-zhen,WAN Jing-lin,LI Chuan-you,CAO Ji-xiu.2003.Late Cenozoic deformation subsequence in northeastern margin of Tibet-Detrital AFT records from Linxia Basin[J].Science in China(Series D),46(S1):266-275(in Chinese).
方小敏,李吉均,朱俊杰,陈怀录,曹继秀.1997.甘肃临夏盆地新生代地层绝对年代测定与划分[J].科学通报,42(14):1457-1471.
甘肃省地质调查院.2007.岷县幅1:250000区域地质调查报告[R].兰州:甘肃省地质调查院.
高锐,王海燕,马永生,朱铉,李秋生,李鹏武,匡朝阳,卢占武.2006.松潘地块若尔盖盆地与西秦岭造山带岩石圈尺度的构造关系——深地震反射剖面探测成果[J].地球学报,27(5):411-418.
郭进京,韩文峰,李雪峰,刘寒鹏.2011.汶川8.0级地震断层同震位移的构造意义与运动学模型[J].地质学报,85(3):309-322.
郭进京,韩文峰,李雪峰.2009.西秦岭新生代以来地质构造过程对青藏高原隆升和变形的约束[J].地学前缘,16(6):215-225.
何永年,林传勇,史兰斌.1988.构造岩石学基础[M].北京:地质出版社.
姜晓玮,王江海,张会化.2003.西秦岭断裂走滑与盆地的耦合——西秦岭—松甘块体新生代向东走滑挤出的证据[J].地学前缘,10(2):201-207.
康来迅,张新基,黄杏珍,李立武.1999.西秦岭北缘断裂带排气活动的比较研究[J].地震学报,21(6):657-664.
李传友,张培震,袁道阳,王志才,张剑玺.2006.西秦岭北缘断裂带黄香沟段晚第四纪水平位移特征及其微地貌响应[J].地震地质,28(3):391-404.
李传友,张培震,袁道阳,王志才,郑德文.2010.活动走滑断裂上断塞塘沉积特征及其构造含义——以西秦岭北缘断裂带断塞塘为例[J].地质学报,84(1):90-104.
李传友,张培震,张剑玺,袁道阳,王志才.2007.西秦岭北缘断裂带黄香沟段晚第四纪活动表现与滑动速率[J].第四纪研究,27(1):54-63.
李吉均,方小敏,马海洲,朱俊杰,潘保田,陈怀录.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辑),26(4):316-322.
林爱明.1996.断层岩与断层模式[J].高校地质学报,2(3):295-306.
林爱明.2008.地震化石:假熔岩的形成与保存[M].北京:高等教育出版社.
陕西省地质矿产勘查开发局.1996.秦岭北缘活动断裂带[M].北京:地质出版社.
施炜,张岳桥,董树文.2003.郯庐断裂带中段第四纪活动及其分段特征[J].地球学报,24(1):11-18.
孙岩,韩克从.1985.断裂构造岩带划分[M].北京:科学出版社.
王修喜,李吉均,宋春晖,张军,赵志军,高军平,潘美慧.2006.青藏高原东北缘西秦岭新生代抬升——天水盆地碎屑颗粒磷灰石裂变径迹记录[J].沉积学报,24(6):783-789.
王志才,张培震,张广良,李传友,郑德文,袁道阳.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.
王宗起,闫臻,王涛,高联达,闫全人,陈隽璐,李秋根,姜春发,刘平,张英利,谢春林,向忠金.2009.秦岭造山带主要疑难地层时代研究的新进展[J].地球学报,30(5):561-570.
袁道阳,杨明.1999.西秦岭北缘断裂带的位移累计滑动亏损特征及其破裂分段性研究[J].地震研究,22(4):382-389.
袁道阳,张培震,方小敏,王志才,宋春晖,郑德文.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.
张国伟,郭安林,姚安平.2004.中国大陆构造中西秦岭-松潘大陆构造结[J].地学前缘,11(3):23-32.
张国伟,张本仁,袁学诚,肖庆辉.2001.秦岭造山带与大陆动力学[M].北京:科学出版社.
张秋文,张培震,王乘,ELLIS M A.2004.断层间相互作用的触震与缓震效应定量评价[J].地球学报,25(4):483-488.
张岳桥,马寅生,杨农,张会平,施炜.2005.西秦岭地区东昆仑一秦岭断裂系晚新生代左旋走滑历史及其向东扩展[J].地球学报,26(1):1-8.
郑德文,张培震,万景林,李传友,曹继秀.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),46(S1):266-275.
ALPAR B,YALTTIRAK C.2002.Characteristic features of the North Anatolian Fault in the eastern Marmara region and its tectonic evolution[J].Marine Geology,190(1-2):329-350.
Bureau of Geology and Mineral Recourses Exploration and Devel-opment of Shannxi Province.1996.The north frontal active fault zone of Qinling mountains[M].Beijing:Geological Pub-lishing House(in Chinese).
CAO Juan-juan,LIU Bai-chi,WEN Xue-ze.2003.Determination of the Average Recurrence Intervals of Characteristic Earth-quakes and Estimate of Earthquake Risk on Northern Xiqinling Faults[J].Journal of Seismological Research,26(4):372-381(in Chinese with English abstract).
FANG Xiao-min,LI Ji-jun,ZHU Jun-jie,CHEN Huai-lu,CAO Ji-xiu.1997.Absolute age determination and division of the Cenozoic stratigraphy in the Linxia Basin,Gansu Province,China[J].Chinese Science Bulletin,42(14):1457-1471(in Chi-nese).
Geological Survey of Gansu Province.2007.1:250000Minxian Gregional Gological Surveying Report[R].Lanzhou:Geologi-cal Survey of Gansu Province(in Chinese).
GAO Rui,WANG Hai-yan,MA Yong-sheng,ZHU Xuan,LI Qiu-sheng,LI Peng-wu,KUANG Zhao-yang,LU Zhan-wu.2006.Tectonic Relationships between the ZoigêBasin of the Song-Pan Block and the West Qinling Orogen at Lithosphere Scale:Results of Deep Seismic Reflection Profiling[J].Acta Geoscientica Sinica,27(5):411-418(in Chinese with English abstract).
GUO Jin-jing,HAN Wen-feng,LI Xue-feng,LIU Han-peng.2011.Tectonic Implication of Co-seismic Displacement of Ms8.0Wenchuan Earthquake Fault and Its Kinematic Model[J].Acta Geologica Sinica,85(3):309-322(in Chinese with English ab-stract).
GUO Jin-jing,HAN Wen-feng,LI Xue-feng.2009.The Cenozoic Tectonic Evolution of the West Qinling:Constraints on the Uplift and Deformation of the Tibetan Plateau[J].Earth Sci-ence Frontiers,16(6):215-225(in Chinese with English ab-stract).
HE Yong-nian,LIN Chuan-yong,SHI Lan-bin.1988.Basis of Tec-tonic Petrology[M].Beijing:Geological Publishing House(in Chinese).
JIANG Xiao-wei,WANG Jiang-hai,ZHANG Hui-hua.2003.Cou-pling between strike-slip faults and basins:the evidence for Cenozoic eastward extrusion of the West Qinling-Songgan Block[J].Earth Science Frontiers,10(2):201-207(in Chinese with English abstract).
KANG Lai-xun,ZHANG Xin-ji,HUANG Xing-zhen,LI Li-wu.1999.Comparative study on degassing activities along the north fault zone of western Qinling[J].Acta Seismologica Sinica,12(6):716-723.
KOYIGIT A,BEYHAN A.1998.A new intracontinental transcurrent structure:the Central Anatolian Fault Zone,Tur-key[J].Tectonophysics,284(3-4):317-336.
KOYIGIT A,YILMAS A,ADAMIA S,KULOSGVILI S.2001.Neotectonics of East Anatolian Plateau(Turkey)and Lesser Caucasus:Implication for Transition from Thrusting to Strike-Slip Faulting[J].Geodinamica Acta,14(1-3):177-195.
LI Chuan-you,ZHANG Pei-zhen,YUAN Dao-yang,WANG Zhi-cai,ZHANG Jian-xi.2006.Late-Quaternary horizontal displacement and its associated microgeomorphology of the western Qinling Fault Zone at Huangxianggou[J].Seismology and Geology,28(3):391-404(in Chinese with English ab-stract).
LI Chuan-you,ZHANG Pei-zhen,YUAN Dao-yang,WANG Zhi-cai,ZHENG De-wen.2010.Sedimentary characteristics of sag-pond on the active strike slip fault and its tectonic impli-cations:An example from sag pond along the West Qinling Fault[J].Acta Geologica Sinica,84(2):90-104(in Chinese with English abstract).
LI Chuan-you,ZHANG Pei-zhen,ZHANG Jian-xi,YUANDao-yang,WANG Zhi-cai.2007.Late-Quaternary activity and slip rate of the Western Qinling Fault zone at Huangxiang-gou[J].Quaternary Sciences,27(1):54-63(in Chinese with English abstract).
LI Ji-jun,FANG Xiao-min,MA Hai-zhou,ZHU Jun-jie,PAN Bao-tian,CHEN Huai-lu.1996.Geomorphological and envi-ronmental evolution in the upper reaches of the Yellow River during the Late Cenozoic[J].Science in China(Series D),39(4):380-390.
LIN Ai-ming.1996.Fault rocks and faulting model[J].Geological Journal of China Universities,2(3):295-306(in Chinese with English abstract).
LIN Ai-ming.2001.S-C fabrics developed in cataclastic rocks from the Nojima fault zone,Japan and their implications for tec-tonic history[J].Journal of Structural Geology,23(6-7):1167-1178.
LIN Ai-ming.2008.Earthquake fossils pseudotachylytes:genera-tion and preservation[M].Beijing:High Education Press(in Chinese).
PICHA F J.2002.Late orogenic strike-slip faulting and escape tectonics in frontal Dinarides-Hellenides,Croatia,Yugoslavia,Albania,and Greece[J].American Association of Petroleum Geologists Bulletin,86(9):1659-1671.
REID L F,SIMONY P S,ROSS G M.2002.Dextral strike-slip faulting in the Cariboo Mountains,British Columbia:A natural example of wrench tectonics in relation to Cordilleran tecton-ics[J].Canadian Journal of Earth Sciences,39(6):953-970.
SHI Wei,ZHANG Yue-qiao,DONG Shu-wen.2003.Quaternary Activity and Segmentation Behavior of the Middle Portion of the Tan-Lu Fault Zone[J].Acta Geoscientica Sinica,24(1):11-18(in Chinese with English abstract).
SIBSON R H.1977.Fault rocks and fault mechanism[J].Journal of the Geological Society,133(3):191-213.
SNOKE A W,TULLIS J,TODD V R.1998.Fault-related rocks:a photographic atlas[M].New Jersey:Princeton University Press.
SUN Yan,HAN Ke-cong.1985.Division of Fault Rock Zone[M].Beijing:Science Press(in Chinese).
TSUTSUMI H,YEATS R S,HUFTILE G J.2001.Late Cenozoic tectonics of the Northern Los Angeles fault system,Califor-nia[J].Geological Society of America Bulletin,113(4):454-468.
WANG Xiu-xi,LI Ji-jun,SONG Chun-hui,ZHANG Jun,ZHAO Zhi-jun,GAO Jun-ping,PAN Mei-hui.2006.Cenozoic Uplift of West Qinling,Northeast Margin of Tibetan Plateau:The record of detrital apatite fission track data in Tianshui Basin[J].Acta Sedimentologica Sinica,24(6):783-789(in Chinese with English abstract).
WANG Zhi-cai,ZHANG Pei-zhen,ZHANG Guang-liang,LI Chuan-you,ZHENG De-wen,YUAN Dao-yang.2006.Tertiary tectonic activities of the north frontal fault zone of the west Qinling mountains:implications for the growth of the north-eastern margin of the Qinghai-Tibetan Plateau[J].Earth Sci-ence Frontiers,13(4):119-135(in Chinese with English ab-stract).
WANG Zong-qi,YAN Zhen,WANG Tao,GAO Lian-da,YAN Quan-ren,CHEN Jun-lu,LI Qiu-gen,JIANG Chun-fa,LIU Ping,ZHANG Ying-li,XIE Chun-lin,XIANG Zhong-jin.2009.New Advances in the Study on Ages of Metamorphic Strata in the Qinling Orogenic Belt[J].Acta Geoscientica Sinica,30(5):561-570(in Chinese with English abstract).
YUAN Dao-yang,YANG Ming.1999.Research on the features of displacement cumulative slip deficits and segmentation in the northern margin fault zone of the western Qinling[J].Journal of Seismological Research,22(4):382-389(in Chinese with English abstract).
YUAN Dao-yang,ZHANG Pei-zhen,FANG Xiao-min,WANG Zhi-cai,SONG Chun-hui,ZHENG De-wen.2007.Late Ceno-zoic tectonic deformation of the Linxia Basin,northeastern margin of the Qinghai-Tibet Plateau[J].Earth Science Fron-tiers,14(1):243-250(in Chinese with English abstract).
ZHANG Guo-wei,GUO An-lin,YAO An-ping.2004.Western Qinling-Songpan continental tectonic node in China’s conti-nental tectonics[J].Earth Science Frontiers,11(3):23-32(in Chinese with English abstract).
ZHANG Guo-wei,ZHANG Ben-ren,YUAN Xue-cheng,XIAO Qing-hui.2001.Qinling Continental Orogenic Belt and Continen-tal Dynamics[M].Beijing:Science Press(in Chinese).
ZHANG Qiu-wen,ZHANG Pei-zhen,WANG Cheng,ELLIS M A.2004.Interaction of Active Faults and Its effect on Earthquake Triggering and Delaying[J].Acta Geoscientica Sinica,25(4):483-488(in Chinese with English abstract).
ZHANG Yue-qiao,MA Yin-sheng,YANG Nong,ZHANG Hui-ping,SHI Wei.2005.Late Cenozoic Left-slip Faulting Process of the East Kunlun-Qinling Fault System in West Qinling Region and Its Eastward Propagation[J].Acta Geoscientica Sinica,26(1):1-8(in Chinese with English abstract).
ZHENG De-wen,ZHANG Pei-zhen,WAN Jing-lin,LI Chuan-you,CAO Ji-xiu.2003.Late Cenozoic deformation subsequence in northeastern margin of Tibet-Detrital AFT records from Linxia Basin[J].Science in China(Series D),46(S1):266-275(in Chinese).
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心