柴北缘东段中—新生代构造演化及其对油气的控制作用
|
摘要
综合分析柴北缘东段区域构造背景、残留地层分布、构造变形、裂变径迹和构造演化史,认为研究区中—新生代构造演化可划分为燕山早中期伸展弱断陷—挤压坳陷、燕山晚期挤压隆升、喜马拉雅早期弱挤压坳陷和喜马拉雅晚期强烈逆冲4个阶段。不同构造带的沉降、隆升活动时间与强度存在差异,燕山晚期的差异剥蚀决定了中—下侏罗统的残留展布,喜马拉雅晚期不同的改造作用形成了现今的构造格架。构造运动期次和强度控制了中—下侏罗统烃源岩有机质热演化过程和生排烃期次,燕山期以来继承性古隆起和喜马拉雅早期发育的古构造是深层油气运移的有利指向。有效烃源岩落实、古构造继承性发育、油源断裂时空匹配较好的马海东构造L1井的勘探发现证实了以上认识。
Based on comprehensive analysis of regional tectonic background, residual stratigraphic distribution, tectonic deformation, fission track and tectonic evolution history in the eastern section of the north margin of the Qaidam Basin, it is concluded that the MesozoicCenozoic tectonic evolution can be divided into four stages: the extensional weak rift and compressive depression during the early-middle Yanshan Movement, the compressive uplift during the late Yanshan Movement, the weak compressive depression during the early Himalayan Movement, and the strong thrust during the late Himalayan Movement. The active time and intensity of the subsidence and uplift in different tectonic belts are different. The differential denudation during the late Yanshan Movement determined the residual distribution of the MiddleLower Jurassic Series, and the different transformations during the late Himalayan Movement formed the present tectonic framework. The periods and intensity of tectonic movements controlled the thermal evolution of organic matter and the periods of hydrocarbons generation and expulsion in Middle and Lower Jurassic source rocks. The inherited paleo-uplifts since the Yanshan Movement and the paleo-structures developed during the early Himalayan Movement are favorable directions of deep hydrocarbon migration. The exploration discovery of Well L1 drilled in Mahaidong structure with proven effective source rock, inherited development of paleo-structures and well matched between oil source and faults have confirmed the above understanding.
Based on comprehensive analysis of regional tectonic background, residual stratigraphic distribution, tectonic deformation, fission track and tectonic evolution history in the eastern section of the north margin of the Qaidam Basin, it is concluded that the MesozoicCenozoic tectonic evolution can be divided into four stages: the extensional weak rift and compressive depression during the early-middle Yanshan Movement, the compressive uplift during the late Yanshan Movement, the weak compressive depression during the early Himalayan Movement, and the strong thrust during the late Himalayan Movement. The active time and intensity of the subsidence and uplift in different tectonic belts are different. The differential denudation during the late Yanshan Movement determined the residual distribution of the MiddleLower Jurassic Series, and the different transformations during the late Himalayan Movement formed the present tectonic framework. The periods and intensity of tectonic movements controlled the thermal evolution of organic matter and the periods of hydrocarbons generation and expulsion in Middle and Lower Jurassic source rocks. The inherited paleo-uplifts since the Yanshan Movement and the paleo-structures developed during the early Himalayan Movement are favorable directions of deep hydrocarbon migration. The exploration discovery of Well L1 drilled in Mahaidong structure with proven effective source rock, inherited development of paleo-structures and well matched between oil source and faults have confirmed the above understanding.
引文
[1]李明义,岳湘安,江青春,吴珍珍,张春楠,魏学斌,等.柴达木盆地北缘主要构造带构造演化与油气成藏关系[J].天然气地球科学,2012,23(3):461-468.Li Mingyi,Yue Xiang’an,Jiang Qingchun,Wu Zhenzhen,Zhang Chunnan,Wei Xuebin,et al.Relationship between hydrocarbon accumulation and tectonic evolution in main structural belt of the northern border of Qaidam Basin[J].Natural Gas Geoscience,2012,23(3):461-468.
[2]汤良杰,金之钧,戴俊生,张明利,张兵山.柴达木盆地及相邻造山带区域断裂系统[J].地球科学--中国地质大学学报,2002,27(6):676-682.Tang Liangjie,Jin Zhijun,Dai Junsheng,Zhang Mingli,Zhang Bingshan.Regional fault systems of Qaidam Basin and adjacent orogenic belts[J].Earth Science-Journal of China University of Geosciences,2002,27(6):676-682.
[3]王桂宏,谭彦虎,陈新领,马立协,苏爱国,张水昌,等.新生代柴达木盆地构造演化与油气勘探领域[J].中国石油勘探,2006,11(1):80-84.Wang Guihong,Tan Yanhu,Chen Xinling,Ma Lixie,Su Aiguo,Zhang Shuichang,et al.Cenozoic tectonic evolution and oil/gas exploration field in Qaidam Basin[J].China Petroleum Exploration,2006(1):80-84.
[4]翟光明.中国石油地质志(卷十四):青藏油气区[M].北京:石油工业出版社,1990.Zhai Guangming.Petroleum geology of China(Vol.14):Qinghai-tibet oil and gas region[M].Beijing:Petroleum Industry Press,1990.
[5]徐凤银,尹成明,巩庆林,沈亚.柴达木盆地中、新生代构造演化及其对油气的控制[J].中国石油勘探,2006,11(6):9-16.Xu Fengyin,Yin Chengming,Gong Qinglin,Shen Ya.Mesozoic-Cenozoic structural evolution in Qaidam Basin and its control on hydrocarbon occurrence[J].China Petroleum Exploration,2006(6):9-16.
[6]曾旭,田继先,杨桂茹,王波,郭泽清,王薇,等.柴北缘侏罗纪凹陷结构特征及石油地质意义[J].中国石油勘探,2017,22(5):54-63.Zeng Xu,Tian Jixian,Yang Guiru,Wang Bo,Guo Zeqing,Wang Wei,et al.Structure characteristics and petroleum geological significance of Jurassic sags at the northern margin of Qaidam Basin[J].China Petroleum Exploration,2017,22(5):54-63.
[7]王艳清,刘占国,杨少勇,魏学斌,李森明,吴颜雄.柴达木盆地英雄岭构造带新近系碎屑岩发育特征及油气勘探方向[J].中国石油勘探,2019,24(1):60-71.Wang Yanqing,Liu Zhanguo,Yang Shaoyong,Wei Xuebin,Li Senming,Wu Yanxiong.Development characteristics and exploration targets of Neogene clastic rocks in the Yingxiongling structural belt,Qaidam Basin[J].China Petroleum Exploration,2019,24(1):60-71.
[8]侯启军,何海清,李建忠,杨涛.中国石油天然气股份有限公司近期油气勘探进展及前景展望[J].中国石油勘探,2018,23(1):1-13.Hou Qijun,He Haiqing,Li Jianzhong,Yang Tao.Recent progress and prospect of oil and gas exploration by PetroChina Company Limited[J].China Petroleum Exploration,2018,23(1):1-13.
[9]易定红,王建功,石亚军,孙秀健,马新民,王鹏,等.柴西狮子沟地区渐新统下干柴沟组上段膏盐岩沉积演化特征[J].天然气工业,2017,37(5):1-9.Yi Dinghong,Wang Jiangong,Shi Yajun,Sun Xiujian,Ma Xinmin,Wang Peng,et al.Evolution characteristic of gypsum-salt rocks of the upper member of Oligocene Lower Ganchaigou Fm in the Shizigou area,western Qaidam Basin[J].Natural Gas Industry,2017,37(5):1-9.
[10]邵绪鹏,管树巍,靳久强,沈亚,孟庆洋,王丽宁,等.柴西地区英雄岭构造带构造特征差异及控制因素[J].油气地质与采收率,2018,25(4):67-72.Shao Xupeng,Guan Shuwei,Jin Jiuqiang,Shen Ya,Meng Qingyang,Wang Lining,et al.Differences in structural characteristics and control factors of Yingxiong Range structural belt in the western Qaidam Basin[J].Petroleum Geology and Recovery Efficiency,2018,25(4):67-72.
[11]赵谦,周江羽,李兰斌,刘馨遥,张臣,光佳敏.柴达木盆地七个泉地区渐新世沉积特征与隐蔽油藏预测[J].油气地质与采收率,2017,24(4):22-29.Zhao Qian,Zhou Jiangyu,Li Lanbin,Liu Xinyao,Zhang Chen,Guang Jiamin.Analysis of Oligocene sedimentary characteristics and subtle oil reservoir prediction in the Qigequan area,Qaidam Basin[J].Petroleum Geology and Recovery Efficiency,2017,24(4):22-29.
[12]谢文泉,刘招君,肖丽佳,宋朔,刘金霖.柴北缘鱼卡地区中侏罗统石门沟组油页岩资源潜力[J].特种油气藏,2018,25(5):78-83.Xie Wenquan,Liu Zhaojun,Xiao Lijia,Song Shuo,Liu Jinlin.Oil shale resource potential of the Middle Jurassic Shimengou Formation in Yuka of the north rim in Qaidam Basin[J].Special Oil&Gas Reservoirs,2018,25(5):78-83.
[13]孙秀建,杨巍,白亚东,谢梅,石正灏.柴达木盆地基岩油气藏特征与有利区带研究[J].特种油气藏,2018,25(6):49-54.Sun Xiujian,Yang Wei,Bai Yadong,Xie Mei,Shi Zhenghao.Bedrock reservoir characterization and favorable zones in Qaidam Basin[J].Special Oil&Gas Reservoirs,2018,25(6):49-54.
[14]金之钧,张明利,汤良杰,万天丰,李京昌,张兵山.柴达木盆地中新生代构造演化[J].地球学报,1999,20(增刊1):68-77.Jin Zhijun,Zhang Mingli,Tang Liangjie,Wan Tianfeng,Li Jingchang,Zhang Bingshan.The tectonic evolution of the Qaidam Basin in Meso-Cenozoic era[J].Acta Geoscientia Sinica,1999,20(S1):68-77.
[15]牟中海,陈新领,薛建勤,武天祥.柴达木盆地北缘红山地区白垩系勘探目标[J].中国石油勘探,2008,13(4):8-13.Mu Zhonghai,Chen Xinling,Xue Jianqin,Wu Tianxiang.Exploration prospect of Cretaceous formation in Hongshan area of northern Qaidam Basin[J].China Petroleum Exploration,2008(4):8-13.
[16]陈世悦,徐凤银,彭德华.柴达木盆地基底构造特征及其控油意义[J].新疆石油地质,2000,21(3):175-180.Chen Shiyue,Xu Fengyin,Peng Dehua.Characteristics of basement structures and their controls on hydrocarbon in Qaidam Basin[J].Xinjiang Petroleum Geology,2000,21(3):175-180.
[17]王兆明,罗晓容,汪立群,马立协,申玉山,高雪峰,等.柴达木盆地北缘西段不整合发育特征及其油气地质意义[J].中国石油勘探,2010,15(4):19-25.Wang Zhaoming,Luo Xiaorong,Wang Liqun,Ma Lixie,Shen Yushan,Gao Xuefeng,et al.Unconformity characteristics of west segment of northern margin in Qaidam Basin and its significance in petroleum exploration[J].China Petroleum Exploration,2010,15(4):19-25.
[18]蒋荣宝,陈宣华,党玉琪,尹安,汪立群,蒋武明,等.柴达木盆地东部中新生代两期逆冲断层作用的FT定年[J].地球物理学报,2008,51(1):116-124.Jiang Rongbao,Chen Xuanhua,Dang Yuqi,Yin An,Wang Liqun,Jiang Wuming,et al.Apatite fission track evidence for two phases Mesozoic-Cenozoic thrust faulting in eastern Qaidam Basin[J].Chinese Journal of Geophysics,2008,51(1):116-124.
[19]陈宣华,Michael W.Mcrivette,李丽,尹安,蒋荣宝,万景林,等.东昆仑造山带多期隆升历史的地质热年代学证据[J].地质通报,2011,30(11):1647-1659.Chen Xuanhua,Mcrivette M W,Li Li,Yin An,Jiang Rongbao,Wan Jinglin,et al.Thermochronological evidence for multi-phase uplifting of the East Kunlun Mountains[J].Geological Bulletin of China,2011,30(11):1647-1659.
[20]Ketcham R A,Donelick R A,Donelick M B.AFTSlove:a program for multi-kinetic modeling of apatite fission-track data[J].Geological Materials Research,2000,2:1-32.
[21]高洪雷,刘红旭,何建国,田明明,车永飞.东天山地区中-新生代隆升-剥蚀过程:来自磷灰石裂变径迹的证据[J].地学前缘,2014,21(1):249-260.Gao Honglei,Liu Hongxu,He Jianguo,Tian Mingming,Che Yongfei.Mesozoic-Cenozoic uplift-exhumation history of East Tianshan:evidence from apatite fission track[J].Earth Sicence Frontiers,2014,21(1):249-260.
[22]Nansheng Qiu,Guang Jiang,Qinghua Mei,Jian Chang,Shengjun Wang,Jiyang Wang.The Paleozoic tectono-thermal evolution of the Bachu uplift of the Tarim Basin,NW China:constraints from(U-Th)/He ages,apatite fission track and vitrinite reflectance data[J].Journal of Asian Earth Sciences,2011,41:551-563.
[23]李曰俊,杨海军,赵岩,罗俊成,郑多明,刘亚雷.南天山区域大地构造与演化[J].大地构造与成矿学,2009,33(1):94-104.Li Yuejun,Yang Haijun,Zhao Yan,Luo Juncheng,Zheng Duoming,Liu Yalei.Tectonic framework and evolution of South Tianshan,NW China[J].Geotectonica et Metallogenia,2009,33(1):94-104.
[24]孙波,王金铎,肖永军,林武,柴先平,张俊锋,等.柴北缘东段中、新生代构造物理模拟研究[J].科学技术与工程,2016,16(19):37-44.Sun Bo,Wang Jinduo,Xiao Yongjun,Lin Wu,Chai Xianping,Zhang Junfeng,et al.Meso-Cenozoic tectonic structural physical simulation research of the eastern section of north Qaidam Basin[J].Science Technology and Engineering,2016,16(19):37-44.
[25]商琳,戴俊生,杨学君,夏瑞杰.柴北缘东段构造应力场数值模拟及构造演化模式探讨[J].高校地质学报,2014,20(2):260-267.Shang Lin,Dai Junsheng,Yang Xuejun,Xia Ruijie.Numerical simulation of the tectonic stress field and tectonic evolution pattern of the eastern section of North Qaidam[J].Geological Journal of China Universities,2014,20(2):260-267.
[26]王信国,曹代勇,占文锋,刘天绩.柴达木盆地北缘中、新生代盆地性质及构造演化[J].现代地质,2006,20(4):592-596.Wang Xinguo,Cao Daiyong,Zhan Wenfeng,Liu Tianji.The Meso-Cenozoic basin type and tectonic evolution in the northern margin region of the Qaidam Basin[J].Geoscience,2006,20(4):592-596.
[27]杨超,陈清华,王冠民,庞小军,马婷婷.柴达木盆地晚古生代沉积构造演化[J].中国石油大学学报:自然科学版,2010,34(5):38-43.Yang Chao,Chen Qinghua,Wang Guanmin,Pang Xiaojun,Ma Tingting.Sedimentary and tectonic evolution of Qaidam areas in Late Paleozoic[J].Journal of China University of Petroleum:Edition of Natural Sciences,2010,34(5):38-43.
[28]吴汉宁,刘池阳,张小会,任战利.用古地磁资料探讨柴达木地块构造演化[J].中国科学D辑:地球科学,1997,27(1):9-14.Wu Hanning,Liu Chiyang,Zhang Xiaohui,Ren Zhanli.Astudy of evolution of Qaidam in the view of paleomagnetic[J].Science in China Series D:Earth Sciences,1997,27(1):9-14.
[29]平贵东,吕延防,付晓飞,康琳,周庆强.海拉尔盆地乌尔逊-贝尔凹陷构造演化对油气成藏的控制作用[J].地质科学,2014,49(1):114-130.Ping Guidong,Lv Yanfang,Fu Xiaofei,Kang Lin,Zhou Qingqiang.Controls of structural evolution on the hydrocarbon accumulations of Urxun-Beier depression,Hailar Basin[J].Chinese Journal of Geology,2014,49(1):114-130.
[30]隋风贵.准噶尔盆地西北缘构造演化与油气成藏的关系[J].地质学报,2015,89(4):779-793.Sui Fenggui.Tectonic Evolution and its relationship with hydrocarbon accumulation in the northwest margin of Junggar Basin[J].Acta Geologica Sinica,2015,89(4):779-793.
[2]汤良杰,金之钧,戴俊生,张明利,张兵山.柴达木盆地及相邻造山带区域断裂系统[J].地球科学--中国地质大学学报,2002,27(6):676-682.Tang Liangjie,Jin Zhijun,Dai Junsheng,Zhang Mingli,Zhang Bingshan.Regional fault systems of Qaidam Basin and adjacent orogenic belts[J].Earth Science-Journal of China University of Geosciences,2002,27(6):676-682.
[3]王桂宏,谭彦虎,陈新领,马立协,苏爱国,张水昌,等.新生代柴达木盆地构造演化与油气勘探领域[J].中国石油勘探,2006,11(1):80-84.Wang Guihong,Tan Yanhu,Chen Xinling,Ma Lixie,Su Aiguo,Zhang Shuichang,et al.Cenozoic tectonic evolution and oil/gas exploration field in Qaidam Basin[J].China Petroleum Exploration,2006(1):80-84.
[4]翟光明.中国石油地质志(卷十四):青藏油气区[M].北京:石油工业出版社,1990.Zhai Guangming.Petroleum geology of China(Vol.14):Qinghai-tibet oil and gas region[M].Beijing:Petroleum Industry Press,1990.
[5]徐凤银,尹成明,巩庆林,沈亚.柴达木盆地中、新生代构造演化及其对油气的控制[J].中国石油勘探,2006,11(6):9-16.Xu Fengyin,Yin Chengming,Gong Qinglin,Shen Ya.Mesozoic-Cenozoic structural evolution in Qaidam Basin and its control on hydrocarbon occurrence[J].China Petroleum Exploration,2006(6):9-16.
[6]曾旭,田继先,杨桂茹,王波,郭泽清,王薇,等.柴北缘侏罗纪凹陷结构特征及石油地质意义[J].中国石油勘探,2017,22(5):54-63.Zeng Xu,Tian Jixian,Yang Guiru,Wang Bo,Guo Zeqing,Wang Wei,et al.Structure characteristics and petroleum geological significance of Jurassic sags at the northern margin of Qaidam Basin[J].China Petroleum Exploration,2017,22(5):54-63.
[7]王艳清,刘占国,杨少勇,魏学斌,李森明,吴颜雄.柴达木盆地英雄岭构造带新近系碎屑岩发育特征及油气勘探方向[J].中国石油勘探,2019,24(1):60-71.Wang Yanqing,Liu Zhanguo,Yang Shaoyong,Wei Xuebin,Li Senming,Wu Yanxiong.Development characteristics and exploration targets of Neogene clastic rocks in the Yingxiongling structural belt,Qaidam Basin[J].China Petroleum Exploration,2019,24(1):60-71.
[8]侯启军,何海清,李建忠,杨涛.中国石油天然气股份有限公司近期油气勘探进展及前景展望[J].中国石油勘探,2018,23(1):1-13.Hou Qijun,He Haiqing,Li Jianzhong,Yang Tao.Recent progress and prospect of oil and gas exploration by PetroChina Company Limited[J].China Petroleum Exploration,2018,23(1):1-13.
[9]易定红,王建功,石亚军,孙秀健,马新民,王鹏,等.柴西狮子沟地区渐新统下干柴沟组上段膏盐岩沉积演化特征[J].天然气工业,2017,37(5):1-9.Yi Dinghong,Wang Jiangong,Shi Yajun,Sun Xiujian,Ma Xinmin,Wang Peng,et al.Evolution characteristic of gypsum-salt rocks of the upper member of Oligocene Lower Ganchaigou Fm in the Shizigou area,western Qaidam Basin[J].Natural Gas Industry,2017,37(5):1-9.
[10]邵绪鹏,管树巍,靳久强,沈亚,孟庆洋,王丽宁,等.柴西地区英雄岭构造带构造特征差异及控制因素[J].油气地质与采收率,2018,25(4):67-72.Shao Xupeng,Guan Shuwei,Jin Jiuqiang,Shen Ya,Meng Qingyang,Wang Lining,et al.Differences in structural characteristics and control factors of Yingxiong Range structural belt in the western Qaidam Basin[J].Petroleum Geology and Recovery Efficiency,2018,25(4):67-72.
[11]赵谦,周江羽,李兰斌,刘馨遥,张臣,光佳敏.柴达木盆地七个泉地区渐新世沉积特征与隐蔽油藏预测[J].油气地质与采收率,2017,24(4):22-29.Zhao Qian,Zhou Jiangyu,Li Lanbin,Liu Xinyao,Zhang Chen,Guang Jiamin.Analysis of Oligocene sedimentary characteristics and subtle oil reservoir prediction in the Qigequan area,Qaidam Basin[J].Petroleum Geology and Recovery Efficiency,2017,24(4):22-29.
[12]谢文泉,刘招君,肖丽佳,宋朔,刘金霖.柴北缘鱼卡地区中侏罗统石门沟组油页岩资源潜力[J].特种油气藏,2018,25(5):78-83.Xie Wenquan,Liu Zhaojun,Xiao Lijia,Song Shuo,Liu Jinlin.Oil shale resource potential of the Middle Jurassic Shimengou Formation in Yuka of the north rim in Qaidam Basin[J].Special Oil&Gas Reservoirs,2018,25(5):78-83.
[13]孙秀建,杨巍,白亚东,谢梅,石正灏.柴达木盆地基岩油气藏特征与有利区带研究[J].特种油气藏,2018,25(6):49-54.Sun Xiujian,Yang Wei,Bai Yadong,Xie Mei,Shi Zhenghao.Bedrock reservoir characterization and favorable zones in Qaidam Basin[J].Special Oil&Gas Reservoirs,2018,25(6):49-54.
[14]金之钧,张明利,汤良杰,万天丰,李京昌,张兵山.柴达木盆地中新生代构造演化[J].地球学报,1999,20(增刊1):68-77.Jin Zhijun,Zhang Mingli,Tang Liangjie,Wan Tianfeng,Li Jingchang,Zhang Bingshan.The tectonic evolution of the Qaidam Basin in Meso-Cenozoic era[J].Acta Geoscientia Sinica,1999,20(S1):68-77.
[15]牟中海,陈新领,薛建勤,武天祥.柴达木盆地北缘红山地区白垩系勘探目标[J].中国石油勘探,2008,13(4):8-13.Mu Zhonghai,Chen Xinling,Xue Jianqin,Wu Tianxiang.Exploration prospect of Cretaceous formation in Hongshan area of northern Qaidam Basin[J].China Petroleum Exploration,2008(4):8-13.
[16]陈世悦,徐凤银,彭德华.柴达木盆地基底构造特征及其控油意义[J].新疆石油地质,2000,21(3):175-180.Chen Shiyue,Xu Fengyin,Peng Dehua.Characteristics of basement structures and their controls on hydrocarbon in Qaidam Basin[J].Xinjiang Petroleum Geology,2000,21(3):175-180.
[17]王兆明,罗晓容,汪立群,马立协,申玉山,高雪峰,等.柴达木盆地北缘西段不整合发育特征及其油气地质意义[J].中国石油勘探,2010,15(4):19-25.Wang Zhaoming,Luo Xiaorong,Wang Liqun,Ma Lixie,Shen Yushan,Gao Xuefeng,et al.Unconformity characteristics of west segment of northern margin in Qaidam Basin and its significance in petroleum exploration[J].China Petroleum Exploration,2010,15(4):19-25.
[18]蒋荣宝,陈宣华,党玉琪,尹安,汪立群,蒋武明,等.柴达木盆地东部中新生代两期逆冲断层作用的FT定年[J].地球物理学报,2008,51(1):116-124.Jiang Rongbao,Chen Xuanhua,Dang Yuqi,Yin An,Wang Liqun,Jiang Wuming,et al.Apatite fission track evidence for two phases Mesozoic-Cenozoic thrust faulting in eastern Qaidam Basin[J].Chinese Journal of Geophysics,2008,51(1):116-124.
[19]陈宣华,Michael W.Mcrivette,李丽,尹安,蒋荣宝,万景林,等.东昆仑造山带多期隆升历史的地质热年代学证据[J].地质通报,2011,30(11):1647-1659.Chen Xuanhua,Mcrivette M W,Li Li,Yin An,Jiang Rongbao,Wan Jinglin,et al.Thermochronological evidence for multi-phase uplifting of the East Kunlun Mountains[J].Geological Bulletin of China,2011,30(11):1647-1659.
[20]Ketcham R A,Donelick R A,Donelick M B.AFTSlove:a program for multi-kinetic modeling of apatite fission-track data[J].Geological Materials Research,2000,2:1-32.
[21]高洪雷,刘红旭,何建国,田明明,车永飞.东天山地区中-新生代隆升-剥蚀过程:来自磷灰石裂变径迹的证据[J].地学前缘,2014,21(1):249-260.Gao Honglei,Liu Hongxu,He Jianguo,Tian Mingming,Che Yongfei.Mesozoic-Cenozoic uplift-exhumation history of East Tianshan:evidence from apatite fission track[J].Earth Sicence Frontiers,2014,21(1):249-260.
[22]Nansheng Qiu,Guang Jiang,Qinghua Mei,Jian Chang,Shengjun Wang,Jiyang Wang.The Paleozoic tectono-thermal evolution of the Bachu uplift of the Tarim Basin,NW China:constraints from(U-Th)/He ages,apatite fission track and vitrinite reflectance data[J].Journal of Asian Earth Sciences,2011,41:551-563.
[23]李曰俊,杨海军,赵岩,罗俊成,郑多明,刘亚雷.南天山区域大地构造与演化[J].大地构造与成矿学,2009,33(1):94-104.Li Yuejun,Yang Haijun,Zhao Yan,Luo Juncheng,Zheng Duoming,Liu Yalei.Tectonic framework and evolution of South Tianshan,NW China[J].Geotectonica et Metallogenia,2009,33(1):94-104.
[24]孙波,王金铎,肖永军,林武,柴先平,张俊锋,等.柴北缘东段中、新生代构造物理模拟研究[J].科学技术与工程,2016,16(19):37-44.Sun Bo,Wang Jinduo,Xiao Yongjun,Lin Wu,Chai Xianping,Zhang Junfeng,et al.Meso-Cenozoic tectonic structural physical simulation research of the eastern section of north Qaidam Basin[J].Science Technology and Engineering,2016,16(19):37-44.
[25]商琳,戴俊生,杨学君,夏瑞杰.柴北缘东段构造应力场数值模拟及构造演化模式探讨[J].高校地质学报,2014,20(2):260-267.Shang Lin,Dai Junsheng,Yang Xuejun,Xia Ruijie.Numerical simulation of the tectonic stress field and tectonic evolution pattern of the eastern section of North Qaidam[J].Geological Journal of China Universities,2014,20(2):260-267.
[26]王信国,曹代勇,占文锋,刘天绩.柴达木盆地北缘中、新生代盆地性质及构造演化[J].现代地质,2006,20(4):592-596.Wang Xinguo,Cao Daiyong,Zhan Wenfeng,Liu Tianji.The Meso-Cenozoic basin type and tectonic evolution in the northern margin region of the Qaidam Basin[J].Geoscience,2006,20(4):592-596.
[27]杨超,陈清华,王冠民,庞小军,马婷婷.柴达木盆地晚古生代沉积构造演化[J].中国石油大学学报:自然科学版,2010,34(5):38-43.Yang Chao,Chen Qinghua,Wang Guanmin,Pang Xiaojun,Ma Tingting.Sedimentary and tectonic evolution of Qaidam areas in Late Paleozoic[J].Journal of China University of Petroleum:Edition of Natural Sciences,2010,34(5):38-43.
[28]吴汉宁,刘池阳,张小会,任战利.用古地磁资料探讨柴达木地块构造演化[J].中国科学D辑:地球科学,1997,27(1):9-14.Wu Hanning,Liu Chiyang,Zhang Xiaohui,Ren Zhanli.Astudy of evolution of Qaidam in the view of paleomagnetic[J].Science in China Series D:Earth Sciences,1997,27(1):9-14.
[29]平贵东,吕延防,付晓飞,康琳,周庆强.海拉尔盆地乌尔逊-贝尔凹陷构造演化对油气成藏的控制作用[J].地质科学,2014,49(1):114-130.Ping Guidong,Lv Yanfang,Fu Xiaofei,Kang Lin,Zhou Qingqiang.Controls of structural evolution on the hydrocarbon accumulations of Urxun-Beier depression,Hailar Basin[J].Chinese Journal of Geology,2014,49(1):114-130.
[30]隋风贵.准噶尔盆地西北缘构造演化与油气成藏的关系[J].地质学报,2015,89(4):779-793.Sui Fenggui.Tectonic Evolution and its relationship with hydrocarbon accumulation in the northwest margin of Junggar Basin[J].Acta Geologica Sinica,2015,89(4):779-793.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |