膏盐层在库车秋里塔格构造带构造变形及成藏中的作用
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摘要
库车坳陷秋里塔格构造带发育古近系库姆格列木群和新近系吉迪克组两套膏盐层,这两套膏盐层对该区构造变形和油气成藏起了重要的作用。地震剖面揭示盐层的存在使得秋里塔格构造带构造上、下分层,盐上层主要形成盐推覆构造、逆冲断层、断层传播褶皱和盐核背斜等构造;膏盐层主要形成盐枕、盐焊接或断层焊接等构造;盐下层主要发生断层转折褶皱、背冲断块和逆冲断层等变形。膏盐层组成了该区主要的盖层,并与盐下储层组成了优质的储盖组合,对盐下油气藏的保存极为有利。膏盐层可以改善盐下储层的储集性能,而且膏盐层的塑性流动还可以吸收盐下构造应力,使得盐下构造圈闭在强烈的构造挤压中得以保存。
There were two gypsum-salt layers in the Qiultag structural belt,Kuqa Depression,namely,the Paleogene Kumugeliemu Group(K1-2km) and Neogene Jidike Formation(N1j),which played an important role in structural deformation and hydrocarbon accumulation of the region.Several seismic sections across the Qiultag structural belt revealed that there developed different deformational patterns in the salt-overlying layer,the gypsum-salt layer and the salt-underlying layer,which resulted in three main structural layers occurred.The salt nappes,thrust faults,fault-propagated folds,salt core anticlines,etc.,were mainly developed in the salt-overlying layer.The salt pillows,salt-welding or fault-welding were formed in the gypsum-salt layer.The fault-bended folds,back-thrusted blocks,thrust faults,etc.,were mainly occurred in the salt-underlying layer.A good combination of reservoir and cover in the region consisted of the gypsum-salt layer,as a main cover,and the reservoir in the salt-underlying layer.The gypsum-salt layer improved the reservoir capability of the salt-underlying layer,furthermore,the gypsum-salt layer absorbed structural stress in the salt-underlying layer,so that the structural trap in the salt-underlying layer could be preserved in younger structural events.
There were two gypsum-salt layers in the Qiultag structural belt,Kuqa Depression,namely,the Paleogene Kumugeliemu Group(K1-2km) and Neogene Jidike Formation(N1j),which played an important role in structural deformation and hydrocarbon accumulation of the region.Several seismic sections across the Qiultag structural belt revealed that there developed different deformational patterns in the salt-overlying layer,the gypsum-salt layer and the salt-underlying layer,which resulted in three main structural layers occurred.The salt nappes,thrust faults,fault-propagated folds,salt core anticlines,etc.,were mainly developed in the salt-overlying layer.The salt pillows,salt-welding or fault-welding were formed in the gypsum-salt layer.The fault-bended folds,back-thrusted blocks,thrust faults,etc.,were mainly occurred in the salt-underlying layer.A good combination of reservoir and cover in the region consisted of the gypsum-salt layer,as a main cover,and the reservoir in the salt-underlying layer.The gypsum-salt layer improved the reservoir capability of the salt-underlying layer,furthermore,the gypsum-salt layer absorbed structural stress in the salt-underlying layer,so that the structural trap in the salt-underlying layer could be preserved in younger structural events.
引文
陈书平,汤良杰,贾承造,皮学军,谢会文.2004a.库车坳陷西段盐构造及其与油气的关系.石油学报,25(1):30—34.Chen Shuping,Tang Liangjie,Jia Chengzao,Pi Xuejun and Xie Huiwen.2004a.Salt tectonics in the western Kuqa Depres-sion and its relation to oil and gas distribution.Acta Petrolei Sinica,25(1):30—34.
陈书平,汤良杰,贾承造,皮学军,雷刚林.2004b.秋里塔格构造带盐构造形成的传力方式的构造物理模拟.西安石油大学学报(自然科学版),19(1):6—10.Chen Shuping,Tang Liangjie,Jia Chengzao,Pi Xuejun and Lei Ganglin.2004b.Tectonophysical modeling of two kinds ofstress transmission forms for forming the salt structure in Qiulitake structural zone.Journal ofXi an UniversityofPetro-leu(Natural Sci.Ed.),19(1):6—10.
何光玉,卢华复,李树新.2003.库车盆地秋里塔格构造带构造圈闭及油气勘探方向.地质科学,38(4):506—513.He Guangyu,Lu Huafu and Li Shuxin.2003.Strcture traps and petroleumexploration potentials of the Qiulitage structure beltin the Kuqa Basin,NW China.Chinese Jour.Geol.,38(4):506—513.
何光玉,赵庆,李树新,雷刚林,齐英敏,谢会文.2006.塔里木库车盆地中生代原型分析.地质科学,41(1):44—53.He Guangyu,Zhao Qing,Li Shuxin,Lei Ganglin,Qi Yingmin and Xie Huiwen.2006.Analysis on Mesozoic prototypes of theKuqa Basin,Tarim,northwestern China.Chinese Jour.Geol.,41(1):44—53.
何治亮,徐宏节,段铁军.2005.塔里木多旋回盆地复合构造样式初步分析.地质科学,40(2):153—166.He Zhiliang,Xu Hongjie and Duan Tiejun.2005.Apreliminary analysis on compound structural styles in the Tarimpolycyclicbasin.Chinese Jour.Geol.,40(2):153—166.
胡剑风,刘玉魁,杨明慧,郑多明,刘虎,雷刚林,周厉.2004.塔里木盆地库车坳陷盐构造特征及其与油气的关系.地质科学,39(4):580—588.Hu Jianfeng,Liu Yukui,Yang Minghui,Zheng Duoming,Liu Hu,Lei Ganglin and Zhou Li.2004.Salt structure character-istics and its relation to hydrocarbon accumulation in the Kuqa Depession,Tarim Basin.Chinese Jour.Geol.,39(4):580—588.
金文正,汤良杰,王清华,万桂梅,杨文静,余一欣,彭更新.2007.新疆库车盆地东秋里塔格构造带新生代的构造演化.地质科学,42(3):444—454.Jin Wenzheng,Tang Liangjie,Wang Qinghua,Wan Guimei,Yang Wenjing,Yu Yixin and Peng Gengxin.2007.Cenozoictectonic evolution of the Eastern Qiulitag structural belt,Kuqa foreland basin in Xinjiang.Chinese Jour.Geol.,42(3):444—454.
李振生,刘德良,杨强,李景明.2005.库车坳陷异常超高压保存的主要因素.地学前缘,12(2):316.Li Zhensheng,Liu Deliang,Yang Qiang and Li Jingming.2005.The main factors of superpressure preserved in Kuqa depres-sion.Earth Science Frontiers,12(2):316.
吕修祥,金之钧,周新源,皮学军.2000.塔里木盆地库车坳陷与膏盐岩相关的油气聚集.石油勘探与开发,27(4):20—21.LüXiuxiang,Jin Zhijun,Zhou Xinyuan and Pi Xuejun.2000.Oil and gas accumulation related to evaporate rocks in Kuqa de-pression of Tarim basin.Petroleum Exploration and Development,27(4):20—21.
苗继军,贾承造,王招明,张君峰,赵恩宏.2004.秋里塔格构造带构造分段特征与油气成藏.石油勘探与开发,31(6):20—24.Miao Jijun,Jia Chengzao,Wang Zhaoming,Zhang Junfeng and Zhao Enhong.2004.Structural segmentation and reservoir-formation along the Qiulitage anticline belt of Kuche thrust belt,Tarim basin.Petroleum Exploration and Develop-ment,31(6):20—24.
苗继军,贾承造,王招明,齐英敏,张君峰,赵恩宏.2005.塔里木盆地北部库车地区秋里塔格构造带地层结构及其对构造变形的制约.地质科学,40(4):558—569.Miao Jijun,Jia Chengzao,Wang Zhaoming,Qi Yingmin,Zhang Junfeng and Zhao Enhong.2005.Stratigraphic configurationcontrol on tectonic deformation along the Qiulitag anticline belt of Kuqa area,northern Tarim Basin.Chinese Jour.Geol.,40(4):558—569.
孙冬胜,金之钧,吕修祥,周新源,杨明慧.2004.库车前陆盆地迪那2气田成藏机理及成藏年代.石油与天然气地质,25(5):559—591.Sun Dongsheng,Jin Zhijun,LüXiuxiang,Zhou Xinyuan and Yang Minghui.2004.Reservoiring mechanism and finalizationperiod of Dina 2 gas field in Kuqa basin.Oil&Gas Geology,25(5):559—591.
孙龙德,周新源,王国林.2005.塔里木盆地石油地质研究新进展和油气勘探主攻方向.地质科学,40(2):167—178.Sun Longde,Zhou Xinyuan and Wang Guolin.2005.Contributions of petroleum geology and main direction of oil-gas explra-tion in the Tarim Basin.Chinese Jour.Geol.,40(2):167—178.
汤良杰,贾承造,皮学军,陈书平,王子煜,谢会文.2003a.库车前陆褶皱带盐相关构造样式.中国科学D辑,33(1):38—46.Tang Liangjie,Jia Chengzao,Pi Xuejun.Chen Shuping,Wang Ziyu and Xie Huiwen.2003a.Stucturs styles of the salt relat-ed structures in the Kuqa Foreland Fold-and-Thrust Belt,Tarim Basin,Northwest China Kuqa.Science in China,Se-ries D,33(1):38—46.
汤良杰,贾承造,金之钧,陈书平,皮学军,谢会文.2003b.塔里木盆地库车前陆褶皱带中段盐相关构造特征与油气聚集.地质论评,49(5):501—506.Tang Liangjie,Jia Chengzao,Jin Zhijun,Chen Shuping,Pi Xuejun and Xie Huiwen.2003b.Salt-related structural charac-teristics and hydrocarbon accumulation in the middle segment of the Kuqa foreland fold belt in the northern Tarim ba-sin,NW China.Geol.Rev.,49(5):501—506.
汤良杰,贾承造,金之钧,皮学军,陈书平,谢会文.2003c.库车前陆褶皱冲断带中段第三系盐枕构造.地质科学,38(3):413—424.Tang Liangjie,Jia Chengzao,Jin Zhijun,Pi Xuejun,Chen Shuping and Xie Huiwen.2003c.Tertiary salt pillowstructures inthe central sector of the Kuqa Foreland Fold-and-Thrust Belt,Tarim Basin,Northwest China.Chinese Jour.Geol.,38(3):413—424.
汤良杰,金之钧,贾承造,皮学军,陈书平.2004a.塔里木盆地多期盐构造与油气聚集.中国科学D辑,34(增刊Ⅰ):54—60.Tang Liangjie,Jin Zhijun,Jia Chengzao,Pi Xuejun and Chen Shuping.2004a.Poly-phase salt tectonics and hydrocarbon ac-cumulation in Tarim superimposed basin,northwest China.Science in China,Series D,34(Suppl.Ⅰ):54—60.
汤良杰,金之钧,贾承造,皮学军,陈书平,谢会文,王子煜.2004b.库车前陆褶皱—冲断带前缘大型盐推覆构造.地质学报,78(1):17—25.Tang Liangjie,Jin Zhijun,Jia Chengzao,Pi Xuejun,Chen Shuping,Xie Huiwen and Wang Ziyu.2004b.A large-scale saltnappe complex in the leading edge of the Kuqa Foreland Fold-Thrust Belt,Tarim Basin,Northwest China.Acta Geo-logica Sinica,78(1):17—25.
汤良杰,李京昌,余一欣,王清华,杨文静,谢会文,陈书平,彭更新.2006.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,80(3):313—320.Tang Liangjie,Li Jingchang,Yu Yixin,Wang Qinghua,Yang Wenjing,Xie Huiwen,Chen Shuping and Peng Gengxin.2006.Differential salt tectonic deformation and segmentation of the Kuqa foreland fold-thrust belt,Tarim basin,Northwest China.Acta Geologica Sinica,80(3):313—320.
万桂梅,汤良杰,金文正,李生青,吴月风.2006.库车前陆盆地与波斯湾盆地盐构造对比研究.世界地质,25(1):59—66.Wan Guimei,Tang Liangjie,Jin Wenzheng,Li Shengqing and Wu Yuefeng.2006.Comparison between salt tectonics of Kuqaforeland basin and Persian Gulf basin.Global Geology,25(1):59—66.
王清华,杨明慧,吕修祥.2004.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,39(4):523—531.Wang Qinghua,Yang Minghui and LüXiuxiang.2004.Features of structural segmentation and accumunation of oil and gas inthe Qiulitage structural belt,Kuqa fold-and-thrust belt.Chinese Jour.Geol.,39(4):523—531.
汪新,贾承造,杨树锋.2002.南天山库车褶皱冲断带构造几何学和运动学.地质科学,37(3):372—384.Wang Xin,Jia Chengzao and Yang Shufeng.2002.Geomatry and kinematics of the Kuqa fold-and-thrust belt in the southernTianshan.Chinese Jour.Geol.,37(3):372—384.
王子煜.2002.库车坳陷秋里塔格盐构造形成过程物理模拟.西安石油学院学报(自然科学版),17(6):1—8.Wang Ziyu.2002.Physical modeling of the evolution of Qiulitake salt structure in Kuche Depression.Journal ofXi an Petrole-um Institute(Natural Sci.Ed.),17(6):1—8.
邬光辉,刘玉魁,罗俊成,汪海,雷刚林,高辉.2003.库车坳陷盐构造特征及其对油气成藏的作用.地球学报,24(3):249—254.Wu Guanghui,Liu Yukui,Luo Juncheng,Wang Hai,Lei Ganglin and Gao Hui.2003.Salt structures in the Kuche Depres-sion and their role in the formation of oil and gas accumulations.Acta Geoscientia Sinica,24(3):249—254.
邬光辉,罗春树,胡太平,黄广建,席勤,李文华.2007.褶皱相关断层——以库车坳陷新生界盐上构造层为例.地质科学,42(3):496—505.Wu Guanghui,Luo Chunshu,Hu Taiping,Huang Guangjian,Xi Qin and Li Wenhua.2007.Fold-related faulting:an exam-ple from the Cenozoic salt-overlying beds in the Kuqa Depression.Chinese Jour.Geol.,42(3):496—505.
肖中尧,黄光辉,卢玉红,吴懿,张秋茶.2004.库车坳陷却勒1井原油的重排藿烷系列及油源对比.石油勘探与开发,31(2):35—37.Xiao Zhongyao,Huang Guanghui,Lu Yuhong,Wu Yi and Zhang Qiucha.2004.Rearranged hopanes in oils from the Quele1 Well,Tarim Basin,and the significance for oil correlation.Petroleum Exploration and Development,31(2):35—37.
徐士林,吕修祥,杨明慧,马玉杰,刘洛夫.2004.库车坳陷膏盐岩对异常高压保存的控制作用.西安石油大学学报(自然科学版),19(4):5—8.Xu Shilin,LüXiuxiang,Yang Minghui,Ma Yujie and Liu Luofu.2004.Controlling effect of gypsum and salt rocks on abnor-mally high pressure in Kuche Depression.Journal ofXi an UniversityofPetroleum(Natural Sci.Ed.),19(4):5—8.
杨明慧,金之钧,吕修祥,孙冬胜,彭更新,雷刚林,张国伟.2004.塔里木盆地库车褶皱冲断带的构造特征与油气聚集.西安石油大学学报(自然科学版),19(4):1—4.Yang Minghui,Jin Zhijun,LüXiuxiang,Sun Dongsheng,Peng Gengxin,Lei Ganglin and Zhang Guowei.2004.Structuralcharacteristics and hydrocarbon accumulation of Kuche fold-thrust belts,Talimu Basin.Journal ofXi an University ofPetroleum(Natural Sci.Ed.),19(4):1—4.
张朝军,田在艺.1998.塔里木盆地库车坳陷第三系盐构造与油气.石油学报,19(1):6—10.Zhang Chaojun and Tian Zaiyi.1998.Tertiary salt structures and hydrocarbon in Kuche Depression of Tarim Basin.Acta Pe-trolei Sinica,19(1):6—10.
周兴熙.2000.库车坳陷第三系盐膏质盖层特征及其对油气成藏的控制作用.古地理学报,2(4):51—57.Zhou Xingxi.2000.The features of Tertiary halite-gypsum caprocks and their control on forming of oil and gas pools in KuqaDepression.Journal ofPalaeogeography,2(4):51—57.
周兴熙.2003.库车油气系统北带中、新生界主要储层孔隙流体超压成因探讨.古地理学报,5(1):110—119.Zhou Xingxi.2003.Discussion on origin of overpressure in main reservoir of the Mesozoic and Cenozoic in northern zone ofKuqa petroleum system.Journal ofPalaeogeography,5(1):110—119.
朱玉新,邵新军,杨思玉,蒋裕强,刘成林,李保柱.2000.克拉2气田异常高压特征及成因.西南石油学院学报,22(4):9—13.Zhu Yuxin,Shao Xinjun,Yang Siyu,Jiang Yuqiang,Liu Chenglin and Li Baozhu.2000.Character and origin of overpres-sure in Kela 2 gas field.Journal ofSouthwest Petroleum Institute,22(4):9—13.
陈书平,汤良杰,贾承造,皮学军,雷刚林.2004b.秋里塔格构造带盐构造形成的传力方式的构造物理模拟.西安石油大学学报(自然科学版),19(1):6—10.Chen Shuping,Tang Liangjie,Jia Chengzao,Pi Xuejun and Lei Ganglin.2004b.Tectonophysical modeling of two kinds ofstress transmission forms for forming the salt structure in Qiulitake structural zone.Journal ofXi an UniversityofPetro-leu(Natural Sci.Ed.),19(1):6—10.
何光玉,卢华复,李树新.2003.库车盆地秋里塔格构造带构造圈闭及油气勘探方向.地质科学,38(4):506—513.He Guangyu,Lu Huafu and Li Shuxin.2003.Strcture traps and petroleumexploration potentials of the Qiulitage structure beltin the Kuqa Basin,NW China.Chinese Jour.Geol.,38(4):506—513.
何光玉,赵庆,李树新,雷刚林,齐英敏,谢会文.2006.塔里木库车盆地中生代原型分析.地质科学,41(1):44—53.He Guangyu,Zhao Qing,Li Shuxin,Lei Ganglin,Qi Yingmin and Xie Huiwen.2006.Analysis on Mesozoic prototypes of theKuqa Basin,Tarim,northwestern China.Chinese Jour.Geol.,41(1):44—53.
何治亮,徐宏节,段铁军.2005.塔里木多旋回盆地复合构造样式初步分析.地质科学,40(2):153—166.He Zhiliang,Xu Hongjie and Duan Tiejun.2005.Apreliminary analysis on compound structural styles in the Tarimpolycyclicbasin.Chinese Jour.Geol.,40(2):153—166.
胡剑风,刘玉魁,杨明慧,郑多明,刘虎,雷刚林,周厉.2004.塔里木盆地库车坳陷盐构造特征及其与油气的关系.地质科学,39(4):580—588.Hu Jianfeng,Liu Yukui,Yang Minghui,Zheng Duoming,Liu Hu,Lei Ganglin and Zhou Li.2004.Salt structure character-istics and its relation to hydrocarbon accumulation in the Kuqa Depession,Tarim Basin.Chinese Jour.Geol.,39(4):580—588.
金文正,汤良杰,王清华,万桂梅,杨文静,余一欣,彭更新.2007.新疆库车盆地东秋里塔格构造带新生代的构造演化.地质科学,42(3):444—454.Jin Wenzheng,Tang Liangjie,Wang Qinghua,Wan Guimei,Yang Wenjing,Yu Yixin and Peng Gengxin.2007.Cenozoictectonic evolution of the Eastern Qiulitag structural belt,Kuqa foreland basin in Xinjiang.Chinese Jour.Geol.,42(3):444—454.
李振生,刘德良,杨强,李景明.2005.库车坳陷异常超高压保存的主要因素.地学前缘,12(2):316.Li Zhensheng,Liu Deliang,Yang Qiang and Li Jingming.2005.The main factors of superpressure preserved in Kuqa depres-sion.Earth Science Frontiers,12(2):316.
吕修祥,金之钧,周新源,皮学军.2000.塔里木盆地库车坳陷与膏盐岩相关的油气聚集.石油勘探与开发,27(4):20—21.LüXiuxiang,Jin Zhijun,Zhou Xinyuan and Pi Xuejun.2000.Oil and gas accumulation related to evaporate rocks in Kuqa de-pression of Tarim basin.Petroleum Exploration and Development,27(4):20—21.
苗继军,贾承造,王招明,张君峰,赵恩宏.2004.秋里塔格构造带构造分段特征与油气成藏.石油勘探与开发,31(6):20—24.Miao Jijun,Jia Chengzao,Wang Zhaoming,Zhang Junfeng and Zhao Enhong.2004.Structural segmentation and reservoir-formation along the Qiulitage anticline belt of Kuche thrust belt,Tarim basin.Petroleum Exploration and Develop-ment,31(6):20—24.
苗继军,贾承造,王招明,齐英敏,张君峰,赵恩宏.2005.塔里木盆地北部库车地区秋里塔格构造带地层结构及其对构造变形的制约.地质科学,40(4):558—569.Miao Jijun,Jia Chengzao,Wang Zhaoming,Qi Yingmin,Zhang Junfeng and Zhao Enhong.2005.Stratigraphic configurationcontrol on tectonic deformation along the Qiulitag anticline belt of Kuqa area,northern Tarim Basin.Chinese Jour.Geol.,40(4):558—569.
孙冬胜,金之钧,吕修祥,周新源,杨明慧.2004.库车前陆盆地迪那2气田成藏机理及成藏年代.石油与天然气地质,25(5):559—591.Sun Dongsheng,Jin Zhijun,LüXiuxiang,Zhou Xinyuan and Yang Minghui.2004.Reservoiring mechanism and finalizationperiod of Dina 2 gas field in Kuqa basin.Oil&Gas Geology,25(5):559—591.
孙龙德,周新源,王国林.2005.塔里木盆地石油地质研究新进展和油气勘探主攻方向.地质科学,40(2):167—178.Sun Longde,Zhou Xinyuan and Wang Guolin.2005.Contributions of petroleum geology and main direction of oil-gas explra-tion in the Tarim Basin.Chinese Jour.Geol.,40(2):167—178.
汤良杰,贾承造,皮学军,陈书平,王子煜,谢会文.2003a.库车前陆褶皱带盐相关构造样式.中国科学D辑,33(1):38—46.Tang Liangjie,Jia Chengzao,Pi Xuejun.Chen Shuping,Wang Ziyu and Xie Huiwen.2003a.Stucturs styles of the salt relat-ed structures in the Kuqa Foreland Fold-and-Thrust Belt,Tarim Basin,Northwest China Kuqa.Science in China,Se-ries D,33(1):38—46.
汤良杰,贾承造,金之钧,陈书平,皮学军,谢会文.2003b.塔里木盆地库车前陆褶皱带中段盐相关构造特征与油气聚集.地质论评,49(5):501—506.Tang Liangjie,Jia Chengzao,Jin Zhijun,Chen Shuping,Pi Xuejun and Xie Huiwen.2003b.Salt-related structural charac-teristics and hydrocarbon accumulation in the middle segment of the Kuqa foreland fold belt in the northern Tarim ba-sin,NW China.Geol.Rev.,49(5):501—506.
汤良杰,贾承造,金之钧,皮学军,陈书平,谢会文.2003c.库车前陆褶皱冲断带中段第三系盐枕构造.地质科学,38(3):413—424.Tang Liangjie,Jia Chengzao,Jin Zhijun,Pi Xuejun,Chen Shuping and Xie Huiwen.2003c.Tertiary salt pillowstructures inthe central sector of the Kuqa Foreland Fold-and-Thrust Belt,Tarim Basin,Northwest China.Chinese Jour.Geol.,38(3):413—424.
汤良杰,金之钧,贾承造,皮学军,陈书平.2004a.塔里木盆地多期盐构造与油气聚集.中国科学D辑,34(增刊Ⅰ):54—60.Tang Liangjie,Jin Zhijun,Jia Chengzao,Pi Xuejun and Chen Shuping.2004a.Poly-phase salt tectonics and hydrocarbon ac-cumulation in Tarim superimposed basin,northwest China.Science in China,Series D,34(Suppl.Ⅰ):54—60.
汤良杰,金之钧,贾承造,皮学军,陈书平,谢会文,王子煜.2004b.库车前陆褶皱—冲断带前缘大型盐推覆构造.地质学报,78(1):17—25.Tang Liangjie,Jin Zhijun,Jia Chengzao,Pi Xuejun,Chen Shuping,Xie Huiwen and Wang Ziyu.2004b.A large-scale saltnappe complex in the leading edge of the Kuqa Foreland Fold-Thrust Belt,Tarim Basin,Northwest China.Acta Geo-logica Sinica,78(1):17—25.
汤良杰,李京昌,余一欣,王清华,杨文静,谢会文,陈书平,彭更新.2006.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,80(3):313—320.Tang Liangjie,Li Jingchang,Yu Yixin,Wang Qinghua,Yang Wenjing,Xie Huiwen,Chen Shuping and Peng Gengxin.2006.Differential salt tectonic deformation and segmentation of the Kuqa foreland fold-thrust belt,Tarim basin,Northwest China.Acta Geologica Sinica,80(3):313—320.
万桂梅,汤良杰,金文正,李生青,吴月风.2006.库车前陆盆地与波斯湾盆地盐构造对比研究.世界地质,25(1):59—66.Wan Guimei,Tang Liangjie,Jin Wenzheng,Li Shengqing and Wu Yuefeng.2006.Comparison between salt tectonics of Kuqaforeland basin and Persian Gulf basin.Global Geology,25(1):59—66.
王清华,杨明慧,吕修祥.2004.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,39(4):523—531.Wang Qinghua,Yang Minghui and LüXiuxiang.2004.Features of structural segmentation and accumunation of oil and gas inthe Qiulitage structural belt,Kuqa fold-and-thrust belt.Chinese Jour.Geol.,39(4):523—531.
汪新,贾承造,杨树锋.2002.南天山库车褶皱冲断带构造几何学和运动学.地质科学,37(3):372—384.Wang Xin,Jia Chengzao and Yang Shufeng.2002.Geomatry and kinematics of the Kuqa fold-and-thrust belt in the southernTianshan.Chinese Jour.Geol.,37(3):372—384.
王子煜.2002.库车坳陷秋里塔格盐构造形成过程物理模拟.西安石油学院学报(自然科学版),17(6):1—8.Wang Ziyu.2002.Physical modeling of the evolution of Qiulitake salt structure in Kuche Depression.Journal ofXi an Petrole-um Institute(Natural Sci.Ed.),17(6):1—8.
邬光辉,刘玉魁,罗俊成,汪海,雷刚林,高辉.2003.库车坳陷盐构造特征及其对油气成藏的作用.地球学报,24(3):249—254.Wu Guanghui,Liu Yukui,Luo Juncheng,Wang Hai,Lei Ganglin and Gao Hui.2003.Salt structures in the Kuche Depres-sion and their role in the formation of oil and gas accumulations.Acta Geoscientia Sinica,24(3):249—254.
邬光辉,罗春树,胡太平,黄广建,席勤,李文华.2007.褶皱相关断层——以库车坳陷新生界盐上构造层为例.地质科学,42(3):496—505.Wu Guanghui,Luo Chunshu,Hu Taiping,Huang Guangjian,Xi Qin and Li Wenhua.2007.Fold-related faulting:an exam-ple from the Cenozoic salt-overlying beds in the Kuqa Depression.Chinese Jour.Geol.,42(3):496—505.
肖中尧,黄光辉,卢玉红,吴懿,张秋茶.2004.库车坳陷却勒1井原油的重排藿烷系列及油源对比.石油勘探与开发,31(2):35—37.Xiao Zhongyao,Huang Guanghui,Lu Yuhong,Wu Yi and Zhang Qiucha.2004.Rearranged hopanes in oils from the Quele1 Well,Tarim Basin,and the significance for oil correlation.Petroleum Exploration and Development,31(2):35—37.
徐士林,吕修祥,杨明慧,马玉杰,刘洛夫.2004.库车坳陷膏盐岩对异常高压保存的控制作用.西安石油大学学报(自然科学版),19(4):5—8.Xu Shilin,LüXiuxiang,Yang Minghui,Ma Yujie and Liu Luofu.2004.Controlling effect of gypsum and salt rocks on abnor-mally high pressure in Kuche Depression.Journal ofXi an UniversityofPetroleum(Natural Sci.Ed.),19(4):5—8.
杨明慧,金之钧,吕修祥,孙冬胜,彭更新,雷刚林,张国伟.2004.塔里木盆地库车褶皱冲断带的构造特征与油气聚集.西安石油大学学报(自然科学版),19(4):1—4.Yang Minghui,Jin Zhijun,LüXiuxiang,Sun Dongsheng,Peng Gengxin,Lei Ganglin and Zhang Guowei.2004.Structuralcharacteristics and hydrocarbon accumulation of Kuche fold-thrust belts,Talimu Basin.Journal ofXi an University ofPetroleum(Natural Sci.Ed.),19(4):1—4.
张朝军,田在艺.1998.塔里木盆地库车坳陷第三系盐构造与油气.石油学报,19(1):6—10.Zhang Chaojun and Tian Zaiyi.1998.Tertiary salt structures and hydrocarbon in Kuche Depression of Tarim Basin.Acta Pe-trolei Sinica,19(1):6—10.
周兴熙.2000.库车坳陷第三系盐膏质盖层特征及其对油气成藏的控制作用.古地理学报,2(4):51—57.Zhou Xingxi.2000.The features of Tertiary halite-gypsum caprocks and their control on forming of oil and gas pools in KuqaDepression.Journal ofPalaeogeography,2(4):51—57.
周兴熙.2003.库车油气系统北带中、新生界主要储层孔隙流体超压成因探讨.古地理学报,5(1):110—119.Zhou Xingxi.2003.Discussion on origin of overpressure in main reservoir of the Mesozoic and Cenozoic in northern zone ofKuqa petroleum system.Journal ofPalaeogeography,5(1):110—119.
朱玉新,邵新军,杨思玉,蒋裕强,刘成林,李保柱.2000.克拉2气田异常高压特征及成因.西南石油学院学报,22(4):9—13.Zhu Yuxin,Shao Xinjun,Yang Siyu,Jiang Yuqiang,Liu Chenglin and Li Baozhu.2000.Character and origin of overpres-sure in Kela 2 gas field.Journal ofSouthwest Petroleum Institute,22(4):9—13.
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