引文
[1]贾承造,魏国齐,姚慧君,等.盆地构造演化与区域构造地质.北京:石油工业出版社,1995:149-162
[2]崔泽宏,王志欣,汤良杰.塔北隆起北部叠加断裂构造特征与成因背景分析.中国地质,2005,32(3):378-385
[3]张光亚,陈发景,汪新文.塔北地区变形样式及其分布规律.地球科学——中国地质大学学报,1994,19(6):755-768
[4]龚铭,邵鸿良,伍泽厚,等.塔里木盆地断裂世代初探.石油实验地质,1995,17(2):105-113
[5]王燮培,严俊君.塔里木盆地北部断裂格架分析.地球科学——中国地质大学学报,1995,20(3):237-242
[6]谢晓安,吴奇之,高岩,等.塔里木盆地压扭断裂带构造特征与油气聚集.石油学报,1997,18(2):13-17
[7]陈楚铭,卢华复,王国强,等.塔里木盆地塔北隆起叠加构造分析.高校地质学报,1998,4(3):294-302
[8]汤良杰,金之钧,张一伟,等.塔里木盆地北部隆起负反转构造及其地质意义.现代地质,1999,13(1):93-98
[9]杨春林,吴奇之,夏义平.塔里木盆地北部隆起中、新生界张扭断裂系统成因及其油气聚集的作用.石油地球物理勘探,2000,35(4):461-468
[10]何文渊,李江海,钱祥麟,等.塔里木盆地北部隆起负反转构造成因机制探讨.地质科学,2001,36(2):234-240
[11]魏国齐,贾承造,施央申,等.塔北隆起北部中新生界张扭性断裂系统特征.石油学报,2001,22(1):19-24
[12]温声明,王贵重,程明华,等.南天山山前冲断带的构造样式及成因探讨.新疆地质,2006,24(1):24-29
[13]张光亚.塔里木盆地北部构造转换形式及其成因.现代地质,1997,11(4):453-460
[14]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特征.地震地质,2001,23(3):381-389
[15]王清华,杨明慧,吕修祥.库车褶皱冲断带秋里塔格构造带东、西分段构造特征与油气聚集.地质科学,2004,39(4):523-531
[16]邬光辉,郑多明.塔里木北部地区北北西向构造变换带特征及对石油勘探的启示.地质科学,2004,39(4):551-560
[17]李涛,王宗秀.塔里木地块北部横向构造及断条模式.中国地质,2006,33(1):14-27
[18]汤良杰,李京昌,余一欣,等.库车前陆褶皱-冲断带盐构造差异变形和分段性特征探讨.地质学报,2006,80(3):313-320
[19]杨春林.塔里木盆地压扭构造组合与油气聚集.石油地球物理勘探,1999,34(6):682-689
[20]魏国齐,贾承造,姚慧君.塔北地区海西晚期逆冲-走滑构造与含油气关系.新疆石油地质,1995,16(2):96-101
[21]许志琴,曾令森,杨经绥,等.走滑断裂、“挤压性盆-山构造”与油气资源关系的探讨.地球科学———中国地质大学学报,2004,29(6):631-643
[22]肖安成,杨树锋,王清华,等.塔里木盆地巴楚-柯坪地区南北向断裂系统的空间对应性研究.地质科学,2002,37(增刊):64-72
[23]Harding T P.Newport-inglewood trend.Californian exampleof wrenching style of deformation.AAPG Bulletin,1973,57:97-116
[24]Harding T P.Petroleum traps associated with wrench faults.AAPG Bulletin,1974,58:1290-1304
[25]Sylvester A G.Strike-slip faults.GSA Bulletin,1988,100:1666-1703
[26]Richard P,Mocquet B,Cobbold P R.Experiments onsimultaneous faulting and folding above a basement wrenchfault.Tectonophysics,1991,188:133-141
[27]Crowell J C,Ramirez V R.Late Cenozoic faults insoutheastern California//Crowell J C,Sylvester A G.Tectonics of the Juncture between the San Andreas FaultSystem and the Salton Trough,Southeastern California.Geological Society of America Annual Meeting Guidebook,San Diego,California,1979:27-39
[28]Naylor M A,Mandl G,Sijpesteijn P H K.Fault geometriesin basement-induced wrench faulting under different initialstress states.Journal of Structural Geology,1986,8:737-752
[29]Sanderson D J,Marchini R D.Transpression.Journal ofStructural Geology,1984,6:449-458
[30]Tikoff B,Teyssier C.Strain modelling of displacement-fieldpartitioning in transpressional orogens.Journal of StructuralGeology,1994,16:1575-1588
[31]Krantz R W.The transpressional strain model applied tostrike-slip,oblique-convergent and oblique-divergentdeformation.Journal of Structural Geology,1995,17:1125-1137
[32]Dewey J F,Holdsworth R E,Strachan R A.Transpressionand transtension zones//Holdsworth R E,Strachan R A,Dewey J F.Continental Transpressional and TranstensionalTectonics.London:Geological Society Special Publication,1998,135:1-13
[33]Schreurs G,Colletta B.Analogue modelling of faulting inzones of continental transpression and transtension//Holdsworth R E,Strachan R A,Dewey J F.ContinentalTranspressional and Transtensional Tectonics.London:Geological Society Special Publication,1998,135:59-79
[34]Casasa A M,Gapaisb D,Nalpasb T,et al.Analoguemodels of transpressive systems.Journal of StructuralGeology,2001,23:733-743
[35]Walker R T.A remote sensing study of active folding andfaulting in southern Kerman province,SE Iran.Journal ofStructural Geology,2006,28:654-668
[36]Woodcock N H,Fischer M.Strike-slip duplexes.Journal ofStructural Geology,1986,8:725-735
[37]Moody J D,Hill M J.Wrench-fault tectonics.GSABulletin,1956,67(9):1207-1246
[38]刘和甫,李晓清,刘立群,等.走滑构造体系盆山耦合与区带分析.现代地质,2004,18(2):139-150
[39]苗继军,贾承造,戴金星,等.南天山前陆冲断带中段乌什-温宿地区构造分析与油气成藏.天然气地球科学,2005,16(4):428-432
[40]郭召杰,吴泰然,王冬,等.塔里木西北缘晚新生代印干断层及其与帕米尔构造结的关系.自然科学进展,2004,14(9):1072-1076