塔东南隆起沉积-构造特征及其演化历史
|
摘要
基于地震剖面、岩心、测井和露头剖面等资料分析,运用平衡剖面复原技术,论述了塔里木盆地塔东南隆起带古生代以来的沉积-构造特征及其演化历史。在地震剖面上识别出6个地层不整合界面,划分了5个主要地层构造层序。指出塔东南隆起形成于晚奥陶世加里东运动,经历了加里东、海西、印支、燕山和喜山多次构造运动,在中生代以陆内变形为主,受到南北两条主边界断裂的控制,于中生代早期发生伸展断陷,并遭受晚新生代喜山运动的强烈挤压改造,形成了现今两凹两凸的构造格局。
Based on an analysis of data obtained from seismic profiles,cores,loggings and outcrops,and using the balanced section technology,this paper deals with structural-sedimentary characteristics and tectonic evolution history of the Tadongnan uplift belt in Tarim basin since Paleozoic.Six unconformities were identified on seismic profiles and,on such a basis,five major tectonic sequences were recognized.The Tadongnan Uplift was initially formed in Late Ordovician and experienced Caledonian,Hercynian,Indosinian,Yanshanian and Himalayan movements.Intra-continental deformation took place predominantly during the Mesozoic,with the extensional faulting controlled by two principal boundary faults respectively on the south and on the north.In Early Mesozoic and later,the Tadongnan Uplift experienced serious compressional reformation,thus forming the tectonic framework characterized by two depressions and two uplifts as seen at present.
Based on an analysis of data obtained from seismic profiles,cores,loggings and outcrops,and using the balanced section technology,this paper deals with structural-sedimentary characteristics and tectonic evolution history of the Tadongnan uplift belt in Tarim basin since Paleozoic.Six unconformities were identified on seismic profiles and,on such a basis,five major tectonic sequences were recognized.The Tadongnan Uplift was initially formed in Late Ordovician and experienced Caledonian,Hercynian,Indosinian,Yanshanian and Himalayan movements.Intra-continental deformation took place predominantly during the Mesozoic,with the extensional faulting controlled by two principal boundary faults respectively on the south and on the north.In Early Mesozoic and later,the Tadongnan Uplift experienced serious compressional reformation,thus forming the tectonic framework characterized by two depressions and two uplifts as seen at present.
引文
[1]潘正中,郭群英,王步清,等.塔东南地区构造单元划分新方案[J].新疆石油地质,2007,28(6):781-783.Pan Zhengzhong,Guo Qunying,Wang Buqing,et al.A discussion on division of tectonic units of southeastern Tarim basin[J].Xinjiang Petroleum Geology,2007,28(6):781-783(in Chinese with English abstract).
[2]张斌,肖中尧,吴英,等.塔里木盆地东南地区若参1井天然气成因初探[J].天然气地球化学,2006,17(4):586-589.Zhang Bin,Xiao Zhongyao,Wu Ying,et al.Elementary research of natural gas origin in Ruocan1well,southeast of Tarim basin[J].Natural Gas Geoscience,2006,17(4):586-589(in Chinese with English abstract).
[3]蒲仁海.塔东南拗陷侏罗系沉积相的确定[J].西北大学学报(自然科学版),1994,24(6):547-550.Pu Renhai.The defining of Jurassic depositional facies of the southeast Tarim Basin[J].Journal of Northwest University(Natural Science Edition),1994,24(6):547-550(in Chinese with English abstract).
[4]蒲仁海,车自成,任战利.塔里木盆地东南部构造特征与油气远景[J].石油实验地质,1995,17(3):249-258,264.Pu Renhai,Che Zicheng,Ren Zhanli.Tectonic characteristics and hydrocarbon prospects of southeast Tarim basin[J].Experimental Petroleum Geology,1995,17(3):249-258,264(in Chinese with English abstract).
[5]陈荣林,胡民.塔里木盆地东南断陷区侏罗系含油砂岩的发现及油源研究[J].科学通报,1996,41(18):1685-1688.Chen Ronglin,Hu Min.Findings of Jurassic oil-bearing sandstone and study on oil source in the Dongnan rift zone of Tarim basin[J].Chinese Science Bulletin,1996,41(18):1685-1688(in Chinese).
[6]李文厚.塔里木东南断陷区侏罗系沉积体系及油田意义[J].石油与天然气地质,1998,19(2):110-115.Li Wenhou.Jurassic sedimentary system of fault depression in southeast Tarim and its hydrocarbon significance[J].Oil&Gas Geology,1998,19(2):110-115(in Chinese with English abstract).
[7]周琦,王建国,杜鸿烈.塔东南坳陷侏罗系层序地层分析与油气前景[J].沉积学报,2000,18(4):580-584.Zhou Qi,Wang Jianguo,Du Honglie.Study of sequencestratigraphy in Mesozoic southeast Tarim foreland basin[J].Acta Sedimentologica Sinica,2000,18(4):580-584(in Chinese with English abstract).
[8]王建国,王林风,周琦.塔里木盆地东南地区侏罗系油气勘探前景[J].石油与天然气地质,2000,21(3):259-263,267Wang Jianguo,Wang linfeng,Zhou Qi.Prospects of Jurassic hydrcarbon exploration in southeast Tarim basin[J].Oil&Gas Geology,2000,21(3):259-263,267(in Chinese with English abstract).
[9]温声明,丁长辉,刘兴晓,等.塔里木盆地塔东南地区构造特征[J].石油地球物理勘探,2005,40(增刊):l9-24.Wen Shengming,Ding Changhui,Liu Xingxiao,et al.Structural characteristics of Tadongnan zone of Tarim basin[J].Oil Geophysical Prospecting,2005,40(supplement):l9-24(in Chinese).
[10]丁长辉,单玄龙,王凤俊,等.塔里木盆地东南侏罗纪断陷盆地形成机理及演化分析[J].新疆地质,2007,25(1):81-86.Ding Changhui,Shan Xuanlong,Wang fengjun,et al.The analysis on the mechanism of the formation of Jurassic faulted basin and its evolution in the Southeast region of Tarim basin[J].Xinjiang Geology,2007,25(1):81-86(in Chinese with English abstract).
[11]程晓敢,廖林,陈新安,等.塔里木盆地东南缘侏罗纪沉积相特征与古环境再造[J].中国矿业大学学报,2008,37(4):519-525.Cheng Xiaogan,Liao Lin,Chen Xinan,et al.Jurassic sedimentary facies and paleoenvironmental reconstruction of southeastern Tarim basin,Northwestern China[J].Journal of China University of Mining&Technology,2008,37(4):519-525(in Chinese with English abstract).
[12]王步清,潘正中,郭群英,等.塔东南构造演化和上新世以来的构造格架[J].新疆石油地质,2007,28(6):704-706.Wang Buqing,Pan Zhengzhong,Guo Qunying,et al.Structural evolution and structural framework since Pliocene in Southeast Tarim basin[J].Xinjiang Petroleum Geology,2007,28(6):704-706(in Chinese with English abstract).
[13]伍跃中,王战,陈守建,等.阿尔金山南缘断裂带的分段特征及其构造演化[J].地质学报,2008,82(9):1195-1209.Wu Yuezhong,Wang Zhan,Chen Shoujian,et al.Segmentation and zonation characteristics of South Altun border fault and its tectonic evolution[J].Acta Geologica Sinica,2008,82(9):1195-1209(in Chinese with English abstract).
[14]周勇,潘裕生.茫崖-肃北段阿尔金断裂右旋走滑运动的确定[J].地质科学,1998,33(1):9-16.Zhou Yong,Pan Yusheng.Determination of the dextral slip of Mangya-Subei degment of Altun fault[J].Chinese Jour.Geol.(formerly,Scientia Geologica Sinica),1998,33(1):9-16(in Chinese with English abstract).
[15]周勇,潘裕生.阿尔金断裂早期走滑运动方向及其活动时问探讨[J].地质论评,1999,45(1):1-9.Zhou Yong,Pan Yusheng.The initial shear sense of the Altun fault and its timing[J].Geological Review,1999,45(1):1-9(in Chinese with English abstract).
[16]于海峰,陆松年,赵风清,等.古阿尔金断裂的岩石构造依据及意义[J].前寒武纪研究进展,1998,21(4):10-15.Yu Haifeng,Lu Songnian,Zhao Fengqing,et al.Litho-structural evidences of ancient Altun Tagh and its significance[J].Progress in Precambrian Research,1998,21(4):10-15(in Chinese with English abstract).
[17]刘永江,葛肖虹,叶慧文,等.晚中生代以来阿尔金断裂的走滑模式[J].地球学报,2001,22(1):23-28.Liu Yongjiang,Ge Xiaohong,Ye Huiwen,et al.Strike-slip model for Altun Tagh Fault developed since Late Mesozoic[J].Acta Geoscientia Sinica,2001,22(1):23-28(in Chinese with English abstract).
[18]刘永江,葛肖虹,Genser J,等.阿尔金断裂带构造活动的40Ar-39Ar年龄证据[J].科学通报,2003,48(12):1335-1341.Liu Yongjiang,Ge Xiaohong,Genser J,et al.40Ar-39Ar age evidence for Altun fault tectonic activities in western China[J].Chinese Sci.Bull.,2003,48(18):2024-2030(in Chinese).
[19]刘永江,Franz Neubauer,袁四化,等.阿尔金断裂带年代学和阿尔金山隆升[J].地质科学,2007,42(1):134-146.Liu Yongjiang,Franz Neubauer,Ge Xiaohong,et al.Geochronology of the Altun fault zone and rising of the Altun Mountains[J].Chinese Journal of Geology,2007,42(1):134-146(in Chinese with English abstract).
[20]张岳桥,陈正乐,杨农.阿尔金断裂晚新生代左旋走滑位错的地质新证据[J].现代地质,2001,15(1):8-12.Zhang Yueqiao,Chen Zhengle,Yang Nong.New geological evidence for Late Cenozoic left-lateral displacement along the Altun Tagh Fault[J].Geology,2001,15(1):8-12(in Chinese with English abstract).
[21]陈正乐,张岳桥,王小凤,等.新生代阿尔金山脉隆升历史的裂变径迹证据[J].地球学报,2001,22(5):413-418.Chen Zhengle,Zhang Yueqiao,Wang Xiaofeng,et al.Fission track dating of Apatite constrains on Cenozoic uplift of the Altun Tagh Mountain[J].Acta Geoscientia Sinica,2001,22(5):413-418(in Chinese with English abstract).
[22]陈宣华,尹安,Gehrels G E,等.青藏高原北缘中生代伸展构造40Ar-39Ar测年和MDD模拟[J].地球学报,2002,23(4):305-310.Chen Xuanhua,Yin An,Gehrels G E,et al.Mesozoic extension in northern Tibetan plateau:40Ar-39Ar analyses and MDD modeling[J].Acta Geoscientia Sinica,2002,23(4):305-310(in Chinese with English abstract).
[23]虢顺民,向宏发.阿尔金构造系渐新世-中新世以来断裂左旋位错时空分布规律研究[J].地震地质,1998,20(1):9-18.Guo Shunmin,Xiang Hongfa.A study on spatial-temporal distribution of the fault sinistral displacement in the Altun structure system since Oligocene-Miocene[J].Seismology and Geology,1998,20(1):9-18(in Chinese with English abstract).
[24]葛肖虹,刘永江,任收麦.青藏高原隆升动力学与阿尔金断裂[J].中国地质,2002,29(4):346-350.Ge Xiaohong,Liu Yongjiang,Ren Shoumai.Uplift dynamics ofthe Qinghai-Tibet Plateau and Altun fault[J].Geology in China,2002,29(4):346-350(in Chinese with English abstract).
[25]车自成,刘良,刘洪福,等.阿尔金断裂系的组成及相关中新生代含油气盆地的成因特征[J].中国区域地质,1998,17(4):377-384.Che Zicheng,Liu Liang,Liu Hongfu,et al.The constituents of the Altun fault system and genetic characteristics of related Meso-Cenozoic petroleum-bearing basin[J].Regional Geology of China,1998,17(4):377-384(in Chinese with English abstract).
[26]Zhang J,Zhang Z,Xu Z,et al.Petrology and geochronology of eclogites from the western segment of the Altun Tagh,Northwestern China[J].Lithos,2001,56(2/3):187-206.
[27]Gehrels G E,Yin A,Wang X F.Detrital-Zircon Geochronology of the Northeastern Tibetan Plateau[J].Geol.Soc.Amer.Bull,2003,115(7):881-896.
[28]Sobel E R,Arnaud N,Jolivet M,et a1.Jurassic to Cenozoic Exhumation history of the Altun Tagh Range,Northwest China,constrained by40Ar-39Ar and apatite fission track thermochronology.in:Paleozoic and Mesozoic Tectonic Evolution of Central Asia:from Continental Assembly to Intracontinental Deformation[J].Geological Society of America Memoir,2001,194:247-267.
[29]Ritts B D,Biffi U.Magnitude of Post-Middle Jurassic(Bajocian)displacement on the central Altun Tagh fault system,Northwest China[J].Geol.Soc.Amer.Bull,2000,112(1):61-74.
[30]Meng Q R,Hu J M,Yang F Z.Timing and magnitude of displacement on the Altun Tagh fault:constraints from stratigraphic correlation of adjoining Tarim and Qaidam Basins,NW China[J].Terra Nova,2001,13(2):86-91.
[31]贾承造,张师本,吴绍祖,等.塔里木盆地及周边地层[M].北京:科学出版社,2004:340-342.Jia Chengzhao,Zhang Shiben,Wu Shaozu,et al.Stratigraphy of the Tarim Basin and Adjacent Areas[M].Beijing:Science Press,2004:340-342(in Chinese with English abstract).
[32]张传林,陆松年,于海锋,等.青藏高原北缘西昆仑造山带构造演化:来自锆石SHRIMP及LA-ICP-MS测年的证据[J].中国科学(D辑),2007,37(2):145-154.Zhang Chuanlin,Lu Songnian,Yu Haifeng,et al.Tectonic evolution of structural zone in the northern mergin of Tibetan plateau:evidence of dating from SHRIMP and LA-ICP-MS[J].Science in China(Series D),2007,37(2):145-154(in Chinese).
[33]覃小锋,李江,陆济璞,等.阿尔金碰撞造山带西段的构造特征[J].地质通报,2006,25(1/2):104-112.Qin Xiaofeng,Li Jiang,Lu Jipu,et al.Tectonic evolution of the western segment of the Altun Tagh collisional orogen,Northwest China[J].Geological Bulletin of China,2006,25(1/2):104-112(in Chinese with English abstract).
[34]许志琴,戚学祥,刘福来,等.西昆仑康西瓦加里东期孔兹岩系及地质意义[J].地质学报,2004,78(6):733-743.Xu Zhiqin,Qi Xuexiang,Liu Fulai,et al.The Kangxiwa Caledoniankhondalite series in West Kunlun,China,and its geological significance[J].Acta Geologica Sinica,2004,78(6):733-743(in Chinese with English abstract).
[35]高俊,龙灵利,钱青,等.南天山:晚古生代还是三叠纪碰撞造山带-[J].岩石学报,2006,22(5):1049-1061.Gao Jun,Long Lingli,Qian Qing,et al.South Tianshan:a Late Paleozoie or a Triassic orogen-[J].Acta Petrologica Sinica,2006,22(5):1049-1061(in Chinese with English abstract).
[36]杨品,丁跃潮.塔里木盆地杜瓦剖面二叠-三叠系界限及其特征[J].新疆石油地质,1996,17(3):255-259.Yang Pin,Ding Yuechao.Boundary of Permian-Triassic on Duwa section and its characteristics in the Tarim basin[J].Xinjiang Petroleum Geology,1996,17(3):255-259(in Chinese).
[37]赵冬冬,陈汉林,杨树锋,等.西昆仑甜水海地区前陆褶皱冲断带的构造样式及其演化[J].地质学报,2000,74(2):134-141.Zhao Dongdong,Chen Hanling,Yang Shufeng,et al.Structural styles of the foreland fold and thrust belt in the Tianshuihai area,western Kunlun,and its tectonic evolution[J].Acta Geologica Sinica,2000,134-141(in Chinese with English abstract).
[38]贾承造,杨树锋,陈汉林,等.特提斯北缘盆地群构造地质与天然气[M].北京:石油工业出版社,2001:1-16,136-143.Jia Chengzao,Yang Shufeng,Chen Hanlin,et al.Structural Geology and Natural Gas in the Northern Magin Basin Group[M].Beijing:Petroleum Industry Press,2001:1-16,136-143(in Chinese).
[39]杨树锋,贾承造,陈汉林,等.特提斯构造带的演化和北缘盆地群形成及塔里木天然气勘探远景[J].科学通报,2002,47(增刊):36-43.Yang Shufeng,Jia Chengzao,Chen Hanlin,et al.Evolution of the Tethys tectonic zone,formation of the northern margin basin group and exploration prospect of natural gas in the Tarim basin[J].Chinese Science Bulletin,2002,47(supp.):36-43(in Chinese).
[40]Xiao W J,Windley B F,Hao J,et al.Arc-ophiolite obduction in the western of Kunlun range(China):implications for the palaeozoic evolution of central Asia[J].Jour Geol.Soc,London,2002,159:517-528.
[41]刘训,肖序常,等.中国新疆南部(青藏高原北缘)盆山构造格局的演化[M].北京:地质出版社,2006:273-282.Liu Xun,Xiao Xuchang,et al.Evolution of Basin-Mountain Tectonic Framework in Southern Xinjiang,China(Northern Margin of Qinghai-Tibet Plateau)[M].Beijing:Geological Publishing House,2006:273-282(in Chinese with English abstract).
[42]贾承造,魏国齐,李本亮.中国中西部燕山期构造特征及其油气地质意义[J].石油与天然气地质,2005,26(1):9-15.Jia Chengzao,Wei Guoqi,Li Benliang.Yanshanian tectonic features in West-Central China and their petroleum geological significance[J].Oil&Gas Geology,2005,26(1):9-15(in Chinese with English abstract).
[43]中国地质调查局.阿尔金-昆仑山地区区域地质调查成果与进展[J].地质通报,2004,23(1):28-96.China Geology Survey.Survey results and progress of regional geology in the Altun-Kunlun mountains areas[J].Geological Bulletin of China,2004,23(1):28-96(in Chinese).
[44]McKenzie D P,Sclater J G.The evolution of the Indian Ocean since the Late Cretaceous[J].Geophys.Jour.R.Soc.,1971,24:437-528.
[45]Patriat P,Achache J.The chronology of the India-Eurasia collision:implications for crustal shortening and the driving mechanism of plates[J].Nature,1984,311:615-621.
[46]Rowley D B.Age of initiation of collision between India and Asia:a review of stratigraphic data[J].Earth and Planetary Science Letters.1996,145:1-13.
[47]丁道桂,罗月明.帕米尔地区碰撞构造与塔里木盆地的改造[J].石油与天然气地质,2005,26(1):57-64,77.Ding Daogui,Luo Yueming.Collision structures in Pamir region and reformation of Tarim basin[J].Oil&Gas Geology,2005,26(1):57-64,77(in Chinese with English abstract).
[48]肖序常,刘训,高锐,等.西昆仑及邻区岩石圈结构构造演化-塔里木南-西昆仑多学科地学断面简要报道[J].地质通报,2002,21(2):63-68.Xiao Xuchang,Liu Xun,Gao Rui,et al.Lithospheric structure and tectonic evolution of the west Kunlun and its adjacent areas-brief report on the south Tarim-west Kunlun multidisciplinary geoscience transect[J].Geological Bulletin of China,2002,21(2):63-68(in Chinese with English abstract).
[49]潘桂棠,王培生,徐耀荣,等.中华人民共和国地质矿产部·地质专报(五)构造地质·地质力学·第9号青藏高原新生代构造演化[M].北京:地质出版社,1990:1-190.Pan Guitang,Wang Peisheng,Xu Yaorong,et al.People's Republic of China Ministry of Geology and Mineral Resources Geological Memoirs Series5Number9Cenozoic Tectonic Evolution of Qinghai-Tibet Plateau[M].Beijing:Geological Publishing House,1990:1-190(in Chinese with English abstract).
[2]张斌,肖中尧,吴英,等.塔里木盆地东南地区若参1井天然气成因初探[J].天然气地球化学,2006,17(4):586-589.Zhang Bin,Xiao Zhongyao,Wu Ying,et al.Elementary research of natural gas origin in Ruocan1well,southeast of Tarim basin[J].Natural Gas Geoscience,2006,17(4):586-589(in Chinese with English abstract).
[3]蒲仁海.塔东南拗陷侏罗系沉积相的确定[J].西北大学学报(自然科学版),1994,24(6):547-550.Pu Renhai.The defining of Jurassic depositional facies of the southeast Tarim Basin[J].Journal of Northwest University(Natural Science Edition),1994,24(6):547-550(in Chinese with English abstract).
[4]蒲仁海,车自成,任战利.塔里木盆地东南部构造特征与油气远景[J].石油实验地质,1995,17(3):249-258,264.Pu Renhai,Che Zicheng,Ren Zhanli.Tectonic characteristics and hydrocarbon prospects of southeast Tarim basin[J].Experimental Petroleum Geology,1995,17(3):249-258,264(in Chinese with English abstract).
[5]陈荣林,胡民.塔里木盆地东南断陷区侏罗系含油砂岩的发现及油源研究[J].科学通报,1996,41(18):1685-1688.Chen Ronglin,Hu Min.Findings of Jurassic oil-bearing sandstone and study on oil source in the Dongnan rift zone of Tarim basin[J].Chinese Science Bulletin,1996,41(18):1685-1688(in Chinese).
[6]李文厚.塔里木东南断陷区侏罗系沉积体系及油田意义[J].石油与天然气地质,1998,19(2):110-115.Li Wenhou.Jurassic sedimentary system of fault depression in southeast Tarim and its hydrocarbon significance[J].Oil&Gas Geology,1998,19(2):110-115(in Chinese with English abstract).
[7]周琦,王建国,杜鸿烈.塔东南坳陷侏罗系层序地层分析与油气前景[J].沉积学报,2000,18(4):580-584.Zhou Qi,Wang Jianguo,Du Honglie.Study of sequencestratigraphy in Mesozoic southeast Tarim foreland basin[J].Acta Sedimentologica Sinica,2000,18(4):580-584(in Chinese with English abstract).
[8]王建国,王林风,周琦.塔里木盆地东南地区侏罗系油气勘探前景[J].石油与天然气地质,2000,21(3):259-263,267Wang Jianguo,Wang linfeng,Zhou Qi.Prospects of Jurassic hydrcarbon exploration in southeast Tarim basin[J].Oil&Gas Geology,2000,21(3):259-263,267(in Chinese with English abstract).
[9]温声明,丁长辉,刘兴晓,等.塔里木盆地塔东南地区构造特征[J].石油地球物理勘探,2005,40(增刊):l9-24.Wen Shengming,Ding Changhui,Liu Xingxiao,et al.Structural characteristics of Tadongnan zone of Tarim basin[J].Oil Geophysical Prospecting,2005,40(supplement):l9-24(in Chinese).
[10]丁长辉,单玄龙,王凤俊,等.塔里木盆地东南侏罗纪断陷盆地形成机理及演化分析[J].新疆地质,2007,25(1):81-86.Ding Changhui,Shan Xuanlong,Wang fengjun,et al.The analysis on the mechanism of the formation of Jurassic faulted basin and its evolution in the Southeast region of Tarim basin[J].Xinjiang Geology,2007,25(1):81-86(in Chinese with English abstract).
[11]程晓敢,廖林,陈新安,等.塔里木盆地东南缘侏罗纪沉积相特征与古环境再造[J].中国矿业大学学报,2008,37(4):519-525.Cheng Xiaogan,Liao Lin,Chen Xinan,et al.Jurassic sedimentary facies and paleoenvironmental reconstruction of southeastern Tarim basin,Northwestern China[J].Journal of China University of Mining&Technology,2008,37(4):519-525(in Chinese with English abstract).
[12]王步清,潘正中,郭群英,等.塔东南构造演化和上新世以来的构造格架[J].新疆石油地质,2007,28(6):704-706.Wang Buqing,Pan Zhengzhong,Guo Qunying,et al.Structural evolution and structural framework since Pliocene in Southeast Tarim basin[J].Xinjiang Petroleum Geology,2007,28(6):704-706(in Chinese with English abstract).
[13]伍跃中,王战,陈守建,等.阿尔金山南缘断裂带的分段特征及其构造演化[J].地质学报,2008,82(9):1195-1209.Wu Yuezhong,Wang Zhan,Chen Shoujian,et al.Segmentation and zonation characteristics of South Altun border fault and its tectonic evolution[J].Acta Geologica Sinica,2008,82(9):1195-1209(in Chinese with English abstract).
[14]周勇,潘裕生.茫崖-肃北段阿尔金断裂右旋走滑运动的确定[J].地质科学,1998,33(1):9-16.Zhou Yong,Pan Yusheng.Determination of the dextral slip of Mangya-Subei degment of Altun fault[J].Chinese Jour.Geol.(formerly,Scientia Geologica Sinica),1998,33(1):9-16(in Chinese with English abstract).
[15]周勇,潘裕生.阿尔金断裂早期走滑运动方向及其活动时问探讨[J].地质论评,1999,45(1):1-9.Zhou Yong,Pan Yusheng.The initial shear sense of the Altun fault and its timing[J].Geological Review,1999,45(1):1-9(in Chinese with English abstract).
[16]于海峰,陆松年,赵风清,等.古阿尔金断裂的岩石构造依据及意义[J].前寒武纪研究进展,1998,21(4):10-15.Yu Haifeng,Lu Songnian,Zhao Fengqing,et al.Litho-structural evidences of ancient Altun Tagh and its significance[J].Progress in Precambrian Research,1998,21(4):10-15(in Chinese with English abstract).
[17]刘永江,葛肖虹,叶慧文,等.晚中生代以来阿尔金断裂的走滑模式[J].地球学报,2001,22(1):23-28.Liu Yongjiang,Ge Xiaohong,Ye Huiwen,et al.Strike-slip model for Altun Tagh Fault developed since Late Mesozoic[J].Acta Geoscientia Sinica,2001,22(1):23-28(in Chinese with English abstract).
[18]刘永江,葛肖虹,Genser J,等.阿尔金断裂带构造活动的40Ar-39Ar年龄证据[J].科学通报,2003,48(12):1335-1341.Liu Yongjiang,Ge Xiaohong,Genser J,et al.40Ar-39Ar age evidence for Altun fault tectonic activities in western China[J].Chinese Sci.Bull.,2003,48(18):2024-2030(in Chinese).
[19]刘永江,Franz Neubauer,袁四化,等.阿尔金断裂带年代学和阿尔金山隆升[J].地质科学,2007,42(1):134-146.Liu Yongjiang,Franz Neubauer,Ge Xiaohong,et al.Geochronology of the Altun fault zone and rising of the Altun Mountains[J].Chinese Journal of Geology,2007,42(1):134-146(in Chinese with English abstract).
[20]张岳桥,陈正乐,杨农.阿尔金断裂晚新生代左旋走滑位错的地质新证据[J].现代地质,2001,15(1):8-12.Zhang Yueqiao,Chen Zhengle,Yang Nong.New geological evidence for Late Cenozoic left-lateral displacement along the Altun Tagh Fault[J].Geology,2001,15(1):8-12(in Chinese with English abstract).
[21]陈正乐,张岳桥,王小凤,等.新生代阿尔金山脉隆升历史的裂变径迹证据[J].地球学报,2001,22(5):413-418.Chen Zhengle,Zhang Yueqiao,Wang Xiaofeng,et al.Fission track dating of Apatite constrains on Cenozoic uplift of the Altun Tagh Mountain[J].Acta Geoscientia Sinica,2001,22(5):413-418(in Chinese with English abstract).
[22]陈宣华,尹安,Gehrels G E,等.青藏高原北缘中生代伸展构造40Ar-39Ar测年和MDD模拟[J].地球学报,2002,23(4):305-310.Chen Xuanhua,Yin An,Gehrels G E,et al.Mesozoic extension in northern Tibetan plateau:40Ar-39Ar analyses and MDD modeling[J].Acta Geoscientia Sinica,2002,23(4):305-310(in Chinese with English abstract).
[23]虢顺民,向宏发.阿尔金构造系渐新世-中新世以来断裂左旋位错时空分布规律研究[J].地震地质,1998,20(1):9-18.Guo Shunmin,Xiang Hongfa.A study on spatial-temporal distribution of the fault sinistral displacement in the Altun structure system since Oligocene-Miocene[J].Seismology and Geology,1998,20(1):9-18(in Chinese with English abstract).
[24]葛肖虹,刘永江,任收麦.青藏高原隆升动力学与阿尔金断裂[J].中国地质,2002,29(4):346-350.Ge Xiaohong,Liu Yongjiang,Ren Shoumai.Uplift dynamics ofthe Qinghai-Tibet Plateau and Altun fault[J].Geology in China,2002,29(4):346-350(in Chinese with English abstract).
[25]车自成,刘良,刘洪福,等.阿尔金断裂系的组成及相关中新生代含油气盆地的成因特征[J].中国区域地质,1998,17(4):377-384.Che Zicheng,Liu Liang,Liu Hongfu,et al.The constituents of the Altun fault system and genetic characteristics of related Meso-Cenozoic petroleum-bearing basin[J].Regional Geology of China,1998,17(4):377-384(in Chinese with English abstract).
[26]Zhang J,Zhang Z,Xu Z,et al.Petrology and geochronology of eclogites from the western segment of the Altun Tagh,Northwestern China[J].Lithos,2001,56(2/3):187-206.
[27]Gehrels G E,Yin A,Wang X F.Detrital-Zircon Geochronology of the Northeastern Tibetan Plateau[J].Geol.Soc.Amer.Bull,2003,115(7):881-896.
[28]Sobel E R,Arnaud N,Jolivet M,et a1.Jurassic to Cenozoic Exhumation history of the Altun Tagh Range,Northwest China,constrained by40Ar-39Ar and apatite fission track thermochronology.in:Paleozoic and Mesozoic Tectonic Evolution of Central Asia:from Continental Assembly to Intracontinental Deformation[J].Geological Society of America Memoir,2001,194:247-267.
[29]Ritts B D,Biffi U.Magnitude of Post-Middle Jurassic(Bajocian)displacement on the central Altun Tagh fault system,Northwest China[J].Geol.Soc.Amer.Bull,2000,112(1):61-74.
[30]Meng Q R,Hu J M,Yang F Z.Timing and magnitude of displacement on the Altun Tagh fault:constraints from stratigraphic correlation of adjoining Tarim and Qaidam Basins,NW China[J].Terra Nova,2001,13(2):86-91.
[31]贾承造,张师本,吴绍祖,等.塔里木盆地及周边地层[M].北京:科学出版社,2004:340-342.Jia Chengzhao,Zhang Shiben,Wu Shaozu,et al.Stratigraphy of the Tarim Basin and Adjacent Areas[M].Beijing:Science Press,2004:340-342(in Chinese with English abstract).
[32]张传林,陆松年,于海锋,等.青藏高原北缘西昆仑造山带构造演化:来自锆石SHRIMP及LA-ICP-MS测年的证据[J].中国科学(D辑),2007,37(2):145-154.Zhang Chuanlin,Lu Songnian,Yu Haifeng,et al.Tectonic evolution of structural zone in the northern mergin of Tibetan plateau:evidence of dating from SHRIMP and LA-ICP-MS[J].Science in China(Series D),2007,37(2):145-154(in Chinese).
[33]覃小锋,李江,陆济璞,等.阿尔金碰撞造山带西段的构造特征[J].地质通报,2006,25(1/2):104-112.Qin Xiaofeng,Li Jiang,Lu Jipu,et al.Tectonic evolution of the western segment of the Altun Tagh collisional orogen,Northwest China[J].Geological Bulletin of China,2006,25(1/2):104-112(in Chinese with English abstract).
[34]许志琴,戚学祥,刘福来,等.西昆仑康西瓦加里东期孔兹岩系及地质意义[J].地质学报,2004,78(6):733-743.Xu Zhiqin,Qi Xuexiang,Liu Fulai,et al.The Kangxiwa Caledoniankhondalite series in West Kunlun,China,and its geological significance[J].Acta Geologica Sinica,2004,78(6):733-743(in Chinese with English abstract).
[35]高俊,龙灵利,钱青,等.南天山:晚古生代还是三叠纪碰撞造山带-[J].岩石学报,2006,22(5):1049-1061.Gao Jun,Long Lingli,Qian Qing,et al.South Tianshan:a Late Paleozoie or a Triassic orogen-[J].Acta Petrologica Sinica,2006,22(5):1049-1061(in Chinese with English abstract).
[36]杨品,丁跃潮.塔里木盆地杜瓦剖面二叠-三叠系界限及其特征[J].新疆石油地质,1996,17(3):255-259.Yang Pin,Ding Yuechao.Boundary of Permian-Triassic on Duwa section and its characteristics in the Tarim basin[J].Xinjiang Petroleum Geology,1996,17(3):255-259(in Chinese).
[37]赵冬冬,陈汉林,杨树锋,等.西昆仑甜水海地区前陆褶皱冲断带的构造样式及其演化[J].地质学报,2000,74(2):134-141.Zhao Dongdong,Chen Hanling,Yang Shufeng,et al.Structural styles of the foreland fold and thrust belt in the Tianshuihai area,western Kunlun,and its tectonic evolution[J].Acta Geologica Sinica,2000,134-141(in Chinese with English abstract).
[38]贾承造,杨树锋,陈汉林,等.特提斯北缘盆地群构造地质与天然气[M].北京:石油工业出版社,2001:1-16,136-143.Jia Chengzao,Yang Shufeng,Chen Hanlin,et al.Structural Geology and Natural Gas in the Northern Magin Basin Group[M].Beijing:Petroleum Industry Press,2001:1-16,136-143(in Chinese).
[39]杨树锋,贾承造,陈汉林,等.特提斯构造带的演化和北缘盆地群形成及塔里木天然气勘探远景[J].科学通报,2002,47(增刊):36-43.Yang Shufeng,Jia Chengzao,Chen Hanlin,et al.Evolution of the Tethys tectonic zone,formation of the northern margin basin group and exploration prospect of natural gas in the Tarim basin[J].Chinese Science Bulletin,2002,47(supp.):36-43(in Chinese).
[40]Xiao W J,Windley B F,Hao J,et al.Arc-ophiolite obduction in the western of Kunlun range(China):implications for the palaeozoic evolution of central Asia[J].Jour Geol.Soc,London,2002,159:517-528.
[41]刘训,肖序常,等.中国新疆南部(青藏高原北缘)盆山构造格局的演化[M].北京:地质出版社,2006:273-282.Liu Xun,Xiao Xuchang,et al.Evolution of Basin-Mountain Tectonic Framework in Southern Xinjiang,China(Northern Margin of Qinghai-Tibet Plateau)[M].Beijing:Geological Publishing House,2006:273-282(in Chinese with English abstract).
[42]贾承造,魏国齐,李本亮.中国中西部燕山期构造特征及其油气地质意义[J].石油与天然气地质,2005,26(1):9-15.Jia Chengzao,Wei Guoqi,Li Benliang.Yanshanian tectonic features in West-Central China and their petroleum geological significance[J].Oil&Gas Geology,2005,26(1):9-15(in Chinese with English abstract).
[43]中国地质调查局.阿尔金-昆仑山地区区域地质调查成果与进展[J].地质通报,2004,23(1):28-96.China Geology Survey.Survey results and progress of regional geology in the Altun-Kunlun mountains areas[J].Geological Bulletin of China,2004,23(1):28-96(in Chinese).
[44]McKenzie D P,Sclater J G.The evolution of the Indian Ocean since the Late Cretaceous[J].Geophys.Jour.R.Soc.,1971,24:437-528.
[45]Patriat P,Achache J.The chronology of the India-Eurasia collision:implications for crustal shortening and the driving mechanism of plates[J].Nature,1984,311:615-621.
[46]Rowley D B.Age of initiation of collision between India and Asia:a review of stratigraphic data[J].Earth and Planetary Science Letters.1996,145:1-13.
[47]丁道桂,罗月明.帕米尔地区碰撞构造与塔里木盆地的改造[J].石油与天然气地质,2005,26(1):57-64,77.Ding Daogui,Luo Yueming.Collision structures in Pamir region and reformation of Tarim basin[J].Oil&Gas Geology,2005,26(1):57-64,77(in Chinese with English abstract).
[48]肖序常,刘训,高锐,等.西昆仑及邻区岩石圈结构构造演化-塔里木南-西昆仑多学科地学断面简要报道[J].地质通报,2002,21(2):63-68.Xiao Xuchang,Liu Xun,Gao Rui,et al.Lithospheric structure and tectonic evolution of the west Kunlun and its adjacent areas-brief report on the south Tarim-west Kunlun multidisciplinary geoscience transect[J].Geological Bulletin of China,2002,21(2):63-68(in Chinese with English abstract).
[49]潘桂棠,王培生,徐耀荣,等.中华人民共和国地质矿产部·地质专报(五)构造地质·地质力学·第9号青藏高原新生代构造演化[M].北京:地质出版社,1990:1-190.Pan Guitang,Wang Peisheng,Xu Yaorong,et al.People's Republic of China Ministry of Geology and Mineral Resources Geological Memoirs Series5Number9Cenozoic Tectonic Evolution of Qinghai-Tibet Plateau[M].Beijing:Geological Publishing House,1990:1-190(in Chinese with English abstract).
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