引文
[1]中石化西部新区勘探指挥部.和田区块南部山前带构造特征与油气区带研究.1999.
[1]Wang S H,Xu X K,Song G Q.Tectonic features of the foreland obduction zone in the Hetian sag of the southwest Tari m depression[J].Petroleum Geology&Experi ment,2001,23(4):378-383(in Chinese).
[2]Cui J W,Guo X P,Ding X Z,et al.Mesozoic-Cenozoic de-formation structures and their dynamics in the basin-range junction belt of the west Kunlun Tari m basin[J].Earth Sci-ence Frontiers,2006,13(4):103-118(in Chinese).
[3]Shang X L,Chen X W,Wu C,et al.Cenozoic thrust struc-tures in the Kashi area,western Tari m basin[J].Chinese Journal of Geology,2004,39(4):543-550(in Chinese).
[4]Qu G S,Li Y G,Li Y F,et al.The structural segmentation of foreland and its genesis in the southwestern Tari m basin[J].Sciencein China:Series D,2005,35(3):193-202(in Chi-nese).
[5]Song Y,Fang S H,Zhao MJ,et a1.The structural segmen-tation of foreland thrust belts and its i mplications for hydro-carbon accumulationin foreland basins in central and western China[J].Earth Science Frontiers,2005,12(3):31-38(in Chinese).
[6]Luo J H,He D F.Tectonic characteristics of foreland thrust belt in Hetian section,north margin of west Kunlun[J].Oil&Gas Geology,1999,20(3):237-241(in Chinese).
[7]Yao WJ,Chen WL,Xiao Y,et al.Establishment of typical structural models for piedmont areas surrounding southwest-ern Tari m depression[J].Xinjiang Geology,2002,20(Sup-pl):47-50(in Chinese).
[8]Xiao A C,Chen Y S,Hu W S,et al.Structural type of southwest depression,Tari m basin[J].Xinjiang Petroleum Geology,1995,16(2):102-108(in Chinese).
[9]Hu WS,Liu X F,Chen YS,et al.The Cenozoic structural evolution andits relationship with oil and gas accumulationin the southwestern Tari m depression[J].Experi mental Petro-leum Geology,1996,18(3):244-251(in Chinese).
[10]Chen X A,Zhang X L,Qu QP,et al.The character and hy-drocarbon potential of piedmont structures in southwestern Tari mbasin[J].Xinjiang Petroleum Geology,1999,20(6):468-472(in Chinese).
[11]Zhou X Y,Luo J H,Wang Q H.Structural features and pe-troleumgeology of the fold-thrust belt in the southern Tari m basin,China[J].Science in China:Series D,2004,47(Sup-pl):66-73.
[12]Pan Y S,Wang Y.Tectonic evolution along the geotraverse from Yecheng to Shiquanhe[J].Acta Geologica Sinica,1994,68(4):295-307(in Chinese).
[13]Ding D G,Liu W X,Cui K R,et al.Tectonic analyses and hydrocarbon domains in the Mesozoic and Cenozoic foreland basins of Tari m[J].Experi mental Petroleum Geology,1997,19(2):97-107(in Chinese).
[14]Liu X F,Chen YS,Xiao AC,et al.Characteristics of Ceno-zoic structural deformation in north margin of southwest de-pression,Tari m[J].Oil&Gas Geology,1995,16(3):234-239(in Chinese).
[15]Liu Z R,Yuan WX,Xi B X,et al.Structures of Qi mugen-Sangzhuhe area[J].Xinjiang Geology,2002,20(Suppl):51-57(in Chinese).
[16]Li X D,Wang KZ.The tectonic transformation of mountains and basins at northern margin of West Kunlun mountains[J].Xinjiang Geology,2002,20(Suppl):19-25(in Chinese).
[17]Luo J H,Zhou X Y,Qiu B,et al.Structural features of fold-thrust zonein Kashi depression,western Tari mbasin[J].Oil&Gas Geology,2004,25(2):199-203(in Chinese).
[18]Xiao A C,Yang S F,Chen HL,et al.Structural character-istics of thrust systemin the front of West Kunlun mountains[J].Earth Science Frontiers,2000,7(Suppl):128-136(in Chinese).
[19]Jia C Z.Tectonic features and oil gas of Tari m basin,China[M].Beijing:PetroleumIndustry Press,1997(in Chinese).
[20]Shen J,Wang Y P,Zhao R B,et al.Propagation of cenozoic arcuate structures in northeast Pamir and northwest Tari m basin[J].Seismology and Geology,2001,23(3):381-389(in Chinese).
[21]Gao R,Xiao X C,Gao H,et al.Summary of deep seismic probing of the lithospheric structure across West Kunlun-Ta-ri m-Tianshan[J].Geological Bulletin of China,2002,21(1):11-18(in Chinese).
[22]Xiao X C,Liu X,Gao R,et al.Lithospheric structure and tectonic evolution of the west Kunlun andits adjacent areas—brief report on the south Tari m-West Kunlun multidiscipli-nary geoscience transect[J].Geological Bulletin of China,2002,21(2):63-68(in Chinese).
[23]Lu X B,Shi Y,Tian C L.Tectonic electrical characteristics and A-model subducting patterns of southwest Tari m basin-West Kunlun area[J].Experi mental Petroleum Geology,1995,17(3):238-248(in Chinese).
[24]Lu X B,He F Q,Zhao HS.The geophysical feature,struc-ture and evolution of the tectonic belt inthe southwest margin of the Tari mbasin[J].Geophysical Prospecting for Petrole-um,1997,36(1):43-52(in Chinese).
[25]Zhang X K,Zhao J R,Zhang C K,et al.Crustal structure at the northeast side of the Pamirs[J].Chinese Journal of Geo-physic,2002,45(5):665-671(in Chinese).
[26]Yang K M.The formation and evolution of the western Kun-lun continental margin[J].Geological Review,1994,40(1):9-18(in Chinese).
[27]Jiang C F.Opening-closing tectonics of Kunlun[M].Beijing:Geological Publishing House,1992(in Chinese).
[28]Ding D G,Tang LJ,Qian Y X,et al.Formation andtectonic evolution of Tari m basin[M].Nanjing:Hohai University Press,1996,232-256(in Chinese).
[29]Zhang G Y.The formation,evolution and oil gas of Palaeozo-ic era craton basinin Tari m[M].Beijing:Geological Publish-ing House,2000(in Chinese).
[30]Tang L J.Tectonic evolution and styles of Tari mbasin[M].Beijing:Geological Publishing House,1996(in Chinese).
[31]Wang Z H.Tectonic evolution of the western Kunlun orogen-ic belt,western China[J].Journal of Asian Earth Sciences,2004,24:153-161.
[32]Wang Y B,Wang Y,Liu X,et al.Apatite fission-track re-cords of Mesozoic and Cenozoic episodic reactivation of the Tianshan and West Kunlun mountains[J].Regional Geology of China,2001,20(1):94-99(in Chinese).
[33]Wan J L,Wang E Q.FT evidence of West Kunlun uplift in Pulu[J].Nuclear Techniques,2002,25(7):565-567(in Chinese).
[34]Wang J.Uplift of the Karibasheng and Kuzigan graniteinthe West Kunlun mountains—evidence fromapatite fission track analysis[J].Geological Review,1998,44(4):435-442(inChinese).
[35]Wu X F,Liu S,Wang X,et al.Analysis on structural sec-tions in the Cenozoic Pamir-western Kunlun foreland fold and thrust belt[J].Chinese Journal of Geology,2004,39(2):260-271(in Chinese).
[36]Chen J,Qu GS,Hu J,et al.Arcuate thrust tectonics andits contemporary seismicity in the eastern section of the external zone of the Pamir[J].Seismology and Geology,1997,19(4):301-311(in Chinese).
[37]Liu S,Qiu B,Yin H,et al.Structural characteristics of Wu-boer thrust belts in the foreland of West Kunlun mountain[J].Acta Petrolei Sinica,2005,26(6):16-19(in Chinese).
[38]Wu C,Shang X L,Chen J,et al.Tectonic feature and poten-tials of the Sugaite structural belt in west Xinjiang[J].Chi-nese Journal of Geology,2004,39(4):571-579(in Chinese).
[39]Qu G S,Li Y G,Zhang N,et al.A study on the foreland structure of the Qi mugen arc in southwest Tari mand its ge-netic mechanism[J].Geological Review,2004,50(6):567-576(in Chinese).
[40]Xiao AC.Depth of detachment surfaceinforelandthrust-fold belt of Western Kunlun mountainin southwestern Tari m ba-sin[J].Journal of Jianghan Petroleum Institute,1996,18(1):19-23(in Chinese).
[41]Boyer S E,Elliott D.Thrust systems[J].AAPG,1982,66:1196-1230.
[42]Dahlstrom C D A.Structural geologyinthe eastern margin of the Canadian Rocky mountains[J].Bull Canadian Petroleum Geology,1970,18:332-406.
[43]Li X D,Wang K Z.The tethys framework and its tectonic significance of southwest Tari mand the adjacent region[J].Xinjiang Geology,2000,18(2):113-120(in Chinese).
[44]Liu S,Wang X,Wu X F,et al.Growth strata and the de-formation ti me of thelate Cenozoic alongfront belts of Pamir-western Kunlun-Southwest Tianshan in China[J].Acta Pe-trolei Sinica,2004,25(5):24-28(in Chinese).
[45]Suppe J,Chou G T,Hook S C.Rates of folding and faulting determined from growth strata[M]∥McClay K R.Thrust tectonics.London:Chapman and Hall,1992:105-121.
[46]Lu HF,Jia D,Chen C M,et al.Evidence for growth fault-bend folds in the Tari m basin and its i mplications for fault-slip rates in the Mesozoic and Cenozoic[C]∥Proc30th Inter Geol Congr,Beijing,1997,14:253-262.
[47]Chen J,Lu Y C,Ding G Y.Records of late Cenozoic moun-tain buildingin western Tari mbasin:molasses,growth stra-ta and growth unconformity[J].Quaternary Sciences,2001,21(6):528-539(in Chinese).
[1]王世虎,徐希坤,宋国奇.塔西南坳陷和田凹陷前陆逆冲带构造特征[J].石油实验地质,2001,23(4):378-383.
[2]崔军文,郭宪璞,丁孝忠,等.西昆仑—塔里木盆地盆-山结合带的中、新生代变形构造及其动力学[J].地学前缘,2006,13(4):103-118.
[3]尚新璐,陈新卫,吴超,等.塔里木盆地西部喀什地区的新生代冲断构造[J].地质科学,2004,39(4):543-550.
[4]曲国胜,李亦纲,李岩峰,等.塔里木盆地西南前陆构造分段及其成因[J].中国科学:D辑,2005,35(3):193-202.
[5]宋岩,方世虎,赵孟军,等.前陆盆地冲断带构造分段特征及其对油气成藏的控制作用[J].地学前缘,2005,12(3):31-38.
[6]罗金海,何登发.西昆仑北缘冲断带和田段的构造特征[J].石油与天然气地质,1999,20(3):237-241.
[7]姚卫江,陈文利,肖燕,等.塔里木盆地西南坳陷周边山前的典型构造模式建立[J].新疆地质,2002,20(增刊):47-50.
[8]肖安成,陈毓遂,胡望水,等.塔里木盆地西南坳陷的构造类型[J].新疆石油地质,1995,16(2):102-108.
[9]胡望水,刘学锋,陈毓遂,等.塔里木西南拗陷新生代构造演化与油气的关系[J].石油实验地质,1996,18(3):244-251.
[10]陈新安,张兴林,屈秋平,等.塔西南山前构造特征及含油气前景[J].新疆石油地质,1999,20(6):468-472.
[12]潘裕生,王毅.青藏高原叶城—狮泉河路线地质特征及区域构造演化[J].地质学报,1994,68(4):295-307.
[13]丁道桂,刘伟新,崔可锐,等.塔里木中新生代前陆盆地构造分析与油气领域[J].石油实验地质,1997,19(2):97-107.
[14]刘学锋,陈毓遂,肖安成,等.塔西南坳陷北缘新生代构造形变特征[J].石油与天然气地质,1995,16(3):234-239.
[15]刘增仁,袁文贤,奚伯雄,等.齐姆根—桑株河地区构造特征及演化[J].新疆地质,2002,20(增刊):51-57.
[16]李向东,王克卓.西昆仑山北缘盆山构造转换解析[J].新疆地质,2002,20(增刊):19-25.
[17]罗金海,周新源,邱斌,等.塔里木盆地西部喀什凹陷褶皱冲断带的构造特征[J].石油与天然气地质,2004,25(2):199-203.
[18]肖安成,杨树锋,陈汉林,等.西昆仑山前冲断系的结构特征[J].地学前缘,2000,7(增刊):128-136.
[19]贾承造.中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997.
[20]沈军,汪一鹏,赵瑞斌,等.帕米尔东北缘及塔里木盆地西北部弧形构造的扩展[J].地震地质,2001,23(3):381-389.
[21]高锐,肖序常,高弘,等.西昆仑—塔里木—天山岩石圈深地震探测综述[J].地质通报,2002,21(1):11-18.
[22]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.
[23]鲁新便,石彦,田春来.塔里木盆地西南部—西昆仑地区构造电性特征与A型俯冲模式[J].石油实验地质,1995,17(3):238-248.
[24]鲁新便,何发岐,赵洪生.塔里木盆地西南缘构造带的地球物理特征、构造及其演化[J].石油物探,1997,36(1):43-52.
[25]张先康,赵金仁,张成科,等.帕米尔东北侧地壳结构研究[J].地球物理学报,2002,45(5):665-671.
[26]杨克明.论西昆仑大陆边缘构造演化及塔里木西南盆地类型[J].地质论评,1994,40(1):9-18.
[27]姜春发.昆仑开合构造[M].北京:地质出版社,1992.
[28]丁道桂,汤良杰,钱一雄,等.塔里木盆地形成与演化[M].南京:河海大学出版社,1996:232-256.
[29]张光亚.塔里木古生代克拉通盆地形成演化与油气[M].北京:地质出版社,2000.
[30]汤良杰.塔里木盆地演化和构造样式[M].北京:地质出版社,1996.
[32]王彦斌,王永,刘训,等.天山、西昆仑山中、新生代幕式活动的磷灰石裂变径迹记录[J].中国区域地质,2001,20(1):94-99.
[33]万景林,王二七.西昆仑北部山前普鲁地区山体抬升的裂变径迹研究[J].核技术,2002,25(7):565-567.
[34]王军.西昆仑卡日巴生岩体和苦子干岩体的隆升——来自磷灰石裂变径迹分析的证据[J].地质论评,1998,44(4):435-442.
[35]伍秀芳,刘胜,汪新,等.帕米尔—西昆仑北麓新生代前陆褶皱冲断带构造剖面分析[J].地质科学,2004,39(2):260-271.
[36]陈杰,曲国胜,胡军,等.帕米尔北缘弧形推覆构造带东段的基本特征与现代地震活动[J].地震地质,1997,19(4):301-311.
[37]刘胜,邱斌,尹宏,等.西昆仑山前乌泊尔逆冲推覆带构造特征[J].石油学报,2005,26(6):16-19.
[38]吴超,尚新璐,陈军,等.新疆西部苏盖特构造带构造特征及勘探前景[J].地质科学,2004,39(4):571-579.
[39]曲国胜,李亦纲,张宁,等.塔里木西南缘(齐姆根弧)前陆构造及形成机理[J].地质论评,2004,50(6):567-576.
[40]肖安成.塔里木盆地西南缘西昆仑前陆逆冲一褶皱带主滑脱面深度[J].江汉石油学院学报,1996,18(1):19-23.
[43]李向东,王克卓.塔里木盆地西南及邻区特提斯格局和构造意义[J].新疆地质,2000,18(2):113-120.
[44]刘胜,汪新,伍秀芳,等.塔西南山前晚新生代构造生长地层与变形时代[J].石油学报,2004,25(5):24-28.
[47]陈杰,卢演俦,丁国瑜.塔里木西缘晚新生代造山过程的记录——磨拉石建造及生长地层和生长不整合[J].第四纪研究,2001,21(6):528-539.