柴达木盆地西部中生界原型盆地及其演化
|
摘要
柴达木中生界盆地形成时间及其盆地原型研究存在很大争议,主要原因在于对盆地内有无三叠系陆相沉积及其与上覆下侏罗统地层接触关系和中生界原型盆地形成的构造背景等问题认识不清。区域地质调查在盆地西部月牙山北发现中、上三叠统陆相地层与上覆下侏罗统地层整合接触,在此基础上,结合地表露头、古流分析及地震解释资料研究认为:柴达木中生界盆地起始于中三叠世。中生代在古阿拉巴斯套山与古昆仑山间发育一个大的近东西向展布的活动型山间盆地,盆地经历了中—晚三叠世、早—中侏罗世和晚侏罗世—白垩纪三个演化阶段,分别对应发育了中—晚三叠世坳陷型盆地、早—中侏罗世断陷型盆地和晚侏罗世—白垩纪坳陷型盆地三种原型盆地类型。中—晚三叠世盆地分布比较局限,沉积以氧化环境下的红色碎屑岩建造为主,不具生烃能力;早—中侏罗世盆地范围扩大,沉积物以暗色含煤建造为主,主要分布于现今的阿尔金山地区及其山前地带,沉积中心在阿尔金山地区。晚侏罗世—白垩纪阿尔金山快速隆升,成为主要物源区,开始分割塔里木和柴达木盆地沉积,沉积物为红色磨拉石建造。该研究对于准确评价柴达木盆地生烃潜力及合理进行勘探部署具有重要意义。
Based on an investigation of Mesozoic outcrops as well as paleocurrent and seismic interpretation data,the authors studied the prototypes and evolution of the Mesozoic Qaidam basin.The results show that the Mesozoic Qaidam basin started with Middle Triassic small intermontane depressions.There also developed an intermontane basin between the old Alabasitao Mountain and the Kunlun Mountains in Mesozoic,trending in E-W direction.The basin underwent three tectonic evolution stages,i.e.,Middle-Late Triassic,Early-Middle Jurassic and Late Jurassic-Cretaceous,corresponding to the development of three prototype basins.The Middle-Late Triassic basin was of the depression type,the Early-Middle Jurassic basin was of the fault basin type,and the Late Jurassic-Cretaceous basin was of the depression type.The Middle-Late Triassic depression was restricted in the Yueyashanbei region,and the sediments were red clastic rocks which deposited under an oxidizing environment with no hydrocarbon-generating potential.The Early-Middle Jurassic fault type basin was characterized by the coal-bearing formation,which was widespread in the present Altun Mountains and the neighboring areas in the Qaidam basin.The depocenter was in the present Altun Mountain area.During Late Jurassic-Cretaceous,the Altyn Mountainsa-Qingshuigou cross section;b-Meigou cross section;c-Quanyagou cross section;d-Quan nan 1 cross section;e-Caishiling cross section;f-Heishishan cross section;g-Sanjiaojia cross section;h-Yueyashanbei cross section;i-Meiyaogou cross section;1-Proterozoic;2-granite;3-Ordovician;4-Triassic;5-Upper Jurassic;6-Lower-Middle Jurassic;7-Cretaceous;8-Cenozoic;9-location of cross section;10-study area;11-location of well uplifted rapidly and,as the major provenance,began to separate the Tarim basin from the Qaidam basin.The Late Jurassic-Cretaceous sediments were coarse clastic formations.This study is of significance in the exact evaluation of hydrocarbon potential and the rational arrangement of the exploration work in the Qaidam basin.
Based on an investigation of Mesozoic outcrops as well as paleocurrent and seismic interpretation data,the authors studied the prototypes and evolution of the Mesozoic Qaidam basin.The results show that the Mesozoic Qaidam basin started with Middle Triassic small intermontane depressions.There also developed an intermontane basin between the old Alabasitao Mountain and the Kunlun Mountains in Mesozoic,trending in E-W direction.The basin underwent three tectonic evolution stages,i.e.,Middle-Late Triassic,Early-Middle Jurassic and Late Jurassic-Cretaceous,corresponding to the development of three prototype basins.The Middle-Late Triassic basin was of the depression type,the Early-Middle Jurassic basin was of the fault basin type,and the Late Jurassic-Cretaceous basin was of the depression type.The Middle-Late Triassic depression was restricted in the Yueyashanbei region,and the sediments were red clastic rocks which deposited under an oxidizing environment with no hydrocarbon-generating potential.The Early-Middle Jurassic fault type basin was characterized by the coal-bearing formation,which was widespread in the present Altun Mountains and the neighboring areas in the Qaidam basin.The depocenter was in the present Altun Mountain area.During Late Jurassic-Cretaceous,the Altyn Mountainsa-Qingshuigou cross section;b-Meigou cross section;c-Quanyagou cross section;d-Quan nan 1 cross section;e-Caishiling cross section;f-Heishishan cross section;g-Sanjiaojia cross section;h-Yueyashanbei cross section;i-Meiyaogou cross section;1-Proterozoic;2-granite;3-Ordovician;4-Triassic;5-Upper Jurassic;6-Lower-Middle Jurassic;7-Cretaceous;8-Cenozoic;9-location of cross section;10-study area;11-location of well uplifted rapidly and,as the major provenance,began to separate the Tarim basin from the Qaidam basin.The Late Jurassic-Cretaceous sediments were coarse clastic formations.This study is of significance in the exact evaluation of hydrocarbon potential and the rational arrangement of the exploration work in the Qaidam basin.
引文
[1]金之钧,杨绍清,李京昌,等.2003.柴达木盆地形成演化及其对油气控制作用.中国石油青海油田分公司勘探开发研究院内部报告.
[2]金之钧,张兵山.1997.柴达木盆地地质图(1:500000).中国石油青海油田分公司勘探开发研究院内部资料.
车自成.1986.从青藏高原的隆起看柴达木盆地的形成与演变.石油与天然气地质,7(1):87～94.
陈发景,汪新文.2000.中国西北地区早—中侏罗世盆地原型分析.地学前缘(中国地质大学,北京),7(4):459～468.
陈荣林,朱洪发,陈跃,等.1994.塔里木盆地东南断陷区侏罗系沉积特征及含油性研究.石油实验地质,16(4):339～344.
陈宣华,尹安,George E G,等.2002.青藏高原北缘中生代伸展构造40Ar/39Ar测年和MDD模拟.地球学报,2002,23(4):305～310.
狄恒恕.1984.柴达木盆地北缘逆掩断裂带及其找油前景.石油与天然气地质,5(2):79～87.
高先志,陈发景,马达德,等.2003.中、新生代柴达木北缘的盆地类型与构造演化.西北地质,36(4):16～24.
葛肖虹,张梅生,刘永江,等.1998.阿尔金断裂研究的科学问题与研究思路.现代地质,12(3):295～301.
顾树松,狄恒恕.1990.柴达木盆地形成机理及其对油气的控制.见:朱夏主编,中国中新生代沉积盆地.北京:石油工业出版社,186～195.
郭召杰,张志诚.1998.阿尔金盆地群构造类型与演化.地质论评,44(4):357～364.
郭正府,邓晋福,许志琴,等.1998.青藏东昆仑晚古生代末—中生代中酸性火成岩与陆内造山过程.现代地质,12(3):344～352.
和钟铧,刘招君,郭巍,等.2002.柴达木北缘中生代盆地的成因类型及构造沉积演化.吉林大学学报(地球科学版),32(4):333～339.
胡受权,曹运江,黄继祥,等.1999.柴达木盆地侏罗纪盆地原型及其形成与演化探讨.石油实验地质,21(3):189～195.
黄汉纯,周显强,王长利.1989.柴达木盆地构造演化与石油富集规律.地质论评,35(4):314～322.
黄立功,钟建华,郭泽清,等.2004.阿尔金造山带中、新生代的演化.地球学报,25(3):287～294.
靳久强,赵文智,薛良清,等.1999.中国西北地区侏罗纪原型盆地与演化特征.地质论评,45(1):92～104.
金之钧,张明利,汤良杰,等.2004.柴达木中新生代盆地演化及其控油气作用.石油与天然气地质,25(6):603～608.
刘桂侠,杨永泰,管全俊.2003.从冷科1井下部地层的归属探讨柴达木盆地成盆时间.地球学报,24(2):133～136.
罗照华,邓晋福,曹永清,等.1999.青海省东昆仑地区晚古生代—早中生代火山活动与区域构造演化.现代地质,13(1):51～56.
门相勇,李伟,席萍,等.2001.柴达木盆地北缘沉积凝灰质岩段的地层时代.地质科学,36(2):229～233.
青藏油气区石油地质志编写组.1990.中国石油地质志(卷十四).青藏油气区.北京:石油工业出版社,20～59.
王明儒,胡文义,彭德华.1997.柴达木盆地北缘侏罗系油气前景.石油勘探与开发,24(5):20～24.
巫礼玉.1992.柴达木盆地晚三叠世孢粉组合.见:中国油气区地层古生物编辑委员会.中国油气区地层古生物论文集(3).北京:石油工业出版社,144～149.
席萍,唐伦和.1999.柴达木盆地北部地区下侏罗统湖西山组孢粉化石.见:朱宗浩,郑国光,赵付本编.中国含油气盆地孢粉学论文集.北京:石油工业出版社,139～144.
夏文臣,张宁,袁晓萍,等.1998.柴达木侏罗系的构造层序及前陆盆地演化.石油与天然气地质,19(3):173～180.
薛良清,李文厚,宋立珩,等.2000.西北地区侏罗纪原始沉积区恢复.沉积学报,18(4):539～543.
杨永泰,刘桂侠,贾兴友,等.2002.柴达木盆地北缘上三叠统—侏罗系层序特征与含油气系统划分.地球学报,23(1):67～72.
尹安.2001.喜马拉雅—青藏高原造山带地质演化——显生宙亚洲大陆生长.地球学报,22(3):193～230.
曾联波,金之钧,张明利,等.2002.柴达木侏罗纪盆地性质及其演化特征.沉积学报,20(2):288～292.
翟光明,徐风银,李建青,等.1997.重新认识柴达木盆地,力争油气勘探获得新突破.石油学报,18(2):1～7.
张志成,郭召杰,韩作振.1998.敦煌盆地中侏罗世火山岩的地球化学特征及其地质意义.北京大学学报(自然科学版),34(1):72～79.
郑建京等,彭作林.1995.中国主要含油气盆地运动学过程与油气.沉积学报,13(2):160～168.
左国朝,刘义科,李相博,等.2004.蒙甘青宁地区侏罗纪开合盆山构造格局及原型盆地沉积特征.地质通报,23(3):261～271.
An Yin.2001.Geologic Evolution of the Himalayan-Tibetan Orogen in theContext of Phanerozoic Continental Growth.Acta Geoscientia Sinica,22(3):193～230(in Chinese).
Bradley D R,Ulderico B.2000.Magnitude of post-Middle Jurassic(Bajo-cian)displacement on the central Altyn Tagh fault system,northwestChina.GSA Bulletin,112(1):61～74.
Che Zicheng.1986.The formation and evolution of Qaidam basin in rela-tion to the uplift of Qinghai-Tibet plateau.Oil&Gas Geology,7(1):87～94(in Chinese with English abstract).
Chen Fajing,Wang Xinwen.2000.Prototype analysis of early-middle Ju-rassic basins in northwestern China.Earth Science Frontiers(ChinaUniversity of Geosciences,Beijing),7(4):459～468(in Chinesewith English abstract).
Chen Ronglin,Zhu Hongfa,Chen Yue,et al.1994.Astudy of sedimentarycharacteristics and petrollferousness in the Jurassic sequences of thefault region,the SE Tarim basin.Experimental and Petroleum Geolo-gy,16(4):339～344(in Chinese with English abstract).
Chen Xuanhua,An Yin,George E G,et al.2002.Mesozoic Extension inNorthern Tibetan Plataeu:40Ar/39Ar Analyses and MDD Modeling.Acta Geoscientia Sinica,23(4):305～310(in Chinese with Eng-lish abstract).
Di Hengshu.1984.Overthrust belts on the northern margin of Qaidam ba-sin and their oil prospecting.Oil&Gas Geology,5(2):79～87(inChinese with English abstract).
Editorial Committee of"Petroleum Geology of Qinghai-Tebit of China".1990.Petroleum Geology of China.Vol.14.Qinghai-Tibet Region.Beijing:Petroleum Industry Press,20～59(in Chinese).
Gao Xianzhi,Chen Fajing,Ma Dade,et al.2003.Tectonic evolution of theNorthern Qaidam basin during Mesozoic and Cenozoic eras.North-western Geology,36(4):16～24(in Chinese with English ab-stract).
Ge Xiaohong,Zhang Mmeisheng,Liu Yongjiang,et al.1998.Scientificproblems and thought for research of the Altun Fault.Journal ofGraduate School,China University of Geosciences,12(3):295～301(in Chinese with English abstract).
Gu Shusong,Di Hengshu.1990.Formation Mechanism and its controllingon oil and gas in the Qaidam basin.See:Zhu Xia.The sedimentarybasins of Mesozoic and Cenozoic in China.Beijing:Petroleum Indus-try Press,186～195(in Chinese).
Guo Zhaojie,Zhang Zhicheng.1998.Structural style and tectonic evolu-tion of basins in the Altun region.Geological Review,44(4):357～364(in Chinese with English abstract).
Guo Zhengfu,Deng Jinfu,Xu Zhiqin,et al.1998.Late Paleozoic-Mesozoicintracontinental orogenic process and intermediate-acidic igneousrocks from the eastern Kunlun mountains of northwestern China.Ge-oscience,12(3):344～352(in Chinese with English abstract).
He Zhonghua,Liu Zhaojun,Guo Wei,et al.2002.The genetic type of theMesozoic basin in northern Chaida mu and it tectonic-sedimentary e-volution.Journal of Jilin University(Earth Science Edition),32(4):333～339(in Chinese with English abstract).
Hu Shouquan,Cao Yunjiang,Huang Jixiang,et al.1999.Discussion onformation and evolution of Jurassic basin-prototype of Qaidam basin.Experimental and Petroleum Geology,1999,21(3):189～195(inChinese with English abstract).
Huang Hanchun,Zhou Xianqiang,Wang Changli.1989.Geological Re-view,35(4):314～322(in Chinese with English abstract).
Huang Ligong,Zhong Jianhua,Guo Zeqing,et al.2004.Evolution of theAltun Orogenic Belt in the Mesozoic and Cenozoic.Acta Geoscienc-tica Sinaca,25(3):287～294(in Chinese with English abstract).
Jin Jiuqiang,Zhao Wenzhi,Xue Liangqing,et al.1999.Proto-types and e-volution of Jurassic basins in NWChina.Geological Review,45(1):92～104(in Chinese with English abstract).
Jin Zhijun,Zhang Mingli,Tang Liangjie,et al.2004.Evolution of Meso-Cenozoic Qaidam basin and its control on oil and gas.Oil&Gas Ge-ology,25(6):603～608(in Chinese with English abstract).
Liu Guixia,Yang Yongtai,Guan Quanjun.2003.Inquiry of iniciation ageof the Qaidam basin based on stratigraphic study of the lower part ofthe well Lengke1.Acta Geoscientia Sinica,24(2):133～136(inChinese with English abstract).
Luo Zhaohua,Deng Jinfu,Cao Yongqing,et al.1999.On Late Paleozoic-Early Mesozoic volcanism and regional tectonic evolution of EasternKunlun,Qinghai province.Geoscience,13(1):51～56(in Chinesewith English abstract).
Meng Xiangyong,Li Wei,Xi Ping,et al.2001.Stratigraphic time of sedi-mentary tuffaceous bed in north Qaidam basin.Chinese Journal ofGeology,36(2):229～233(in Chinese with English abstract).
Wang Mingru,Hu Wenyi,Peng Dehua.1997.Oil and gas potential of Ju-rassic strata in northern margin of Qaidam basin.Petroleum explora-tion and development,24(5):20～24(in Chinese with English ab-stract).
Wu Liyu.1992.Late Triassic Sporo-pollen assemblages in the Caidam Ba-sin,Qinghai Province.See:Editorial committee of stratigraphy andpalaeontology of oil and gas bearing areas in China.Stratigraphy andpalaeontology of oil and gas bearing areas in China(3).Beijing:Pe-troleum Industry Press,144～149(in Chinese).
Xi Ping,Tang Lunhe.1999.The fossil Sporopollen of Huxishan Formationof the lower Jurassic in the northern region of the Qaidam basin.See:Zhu Zonghao,Zheng Guoguang,Zhao Fuben.Symposium onpalynology of petroliferous basins in China.Beijing:Petroleum In-dustry Press,139～144(in Chinese).
Xia Wenchen,Zhang Ning,Yuan Xiaoping,et al.1998.Jurassic tectonicssequences of Qaidam and foreland basin evolution.Oil&Gas Geolo-gy,19(3):173～180(in Chinese with English abstract).
Xue Liangqing,Li Wenhou,Song Liheng,et al.2000.Reconstruction of o-riginal sedimentary province of the Jurassic in the Northwestern Chi-na.Acta Sedimentary Sinca,18(4):539～543(in Chinese withEnglish abstract).
Yang Yongtai,Liu Guixia,Jia Xingyou,et al.2002.Characteristics of stra-tigraphic sequence and classification of petroleum systems in thenorthern Qaibam basin.Acta Geoscientia Sinica,23(1):67～72(in Chinese with English abstract).
Zen Lianbo,Jin Zhijun,Zhang Mingli,et al.2002.The Jurassic basin typeand its evolution characteristic in Qaidam Basin.Acta SedimentarySinca,20(2):288～292(in Chinese with English abstract).
Zhai Guangming,Xu Fengyin,Li Jianqing,et al.1997.A recondiration ofQaidam basin for a great breakthrough in oil and natural gas explora-tion.Acta Petrolei Sinica,18(2):1～7(in Chinese with Englishabstract).
Zhang Zhicheng,Guo Zhaojie,Han Zuozhen.1998.Geochemistry and Ge-ological Significance of the Mid-Jurassic Volcanic Rocks in Dun-huang Basin.Acta Scientiarum Naturalium Universitatis Pekinensis,34(1):72～79(in Chinese with English abstract).
Zhen Jianjing,Pen Zuolin.1995.Tectonic Kinematic Process of ChiefOil-gas Bearing Basin and the Formation of Oil-gas in China.ActaSedimentary Sinca,13(2):160～168(in Chinese with English ab-stract).
Zuo Guochao,Liu Yike,Li Xiangbo,et al.2004.Jurassic basin-range tec-tonic pattern and depositional features of prototype basins in the in-ner Mongolia-Gansu-Qinghai-Ningxia region.Geological Bulletin ofChina,23(3):261～271(in Chinese with English abstract).
[2]金之钧,张兵山.1997.柴达木盆地地质图(1:500000).中国石油青海油田分公司勘探开发研究院内部资料.
车自成.1986.从青藏高原的隆起看柴达木盆地的形成与演变.石油与天然气地质,7(1):87～94.
陈发景,汪新文.2000.中国西北地区早—中侏罗世盆地原型分析.地学前缘(中国地质大学,北京),7(4):459～468.
陈荣林,朱洪发,陈跃,等.1994.塔里木盆地东南断陷区侏罗系沉积特征及含油性研究.石油实验地质,16(4):339～344.
陈宣华,尹安,George E G,等.2002.青藏高原北缘中生代伸展构造40Ar/39Ar测年和MDD模拟.地球学报,2002,23(4):305～310.
狄恒恕.1984.柴达木盆地北缘逆掩断裂带及其找油前景.石油与天然气地质,5(2):79～87.
高先志,陈发景,马达德,等.2003.中、新生代柴达木北缘的盆地类型与构造演化.西北地质,36(4):16～24.
葛肖虹,张梅生,刘永江,等.1998.阿尔金断裂研究的科学问题与研究思路.现代地质,12(3):295～301.
顾树松,狄恒恕.1990.柴达木盆地形成机理及其对油气的控制.见:朱夏主编,中国中新生代沉积盆地.北京:石油工业出版社,186～195.
郭召杰,张志诚.1998.阿尔金盆地群构造类型与演化.地质论评,44(4):357～364.
郭正府,邓晋福,许志琴,等.1998.青藏东昆仑晚古生代末—中生代中酸性火成岩与陆内造山过程.现代地质,12(3):344～352.
和钟铧,刘招君,郭巍,等.2002.柴达木北缘中生代盆地的成因类型及构造沉积演化.吉林大学学报(地球科学版),32(4):333～339.
胡受权,曹运江,黄继祥,等.1999.柴达木盆地侏罗纪盆地原型及其形成与演化探讨.石油实验地质,21(3):189～195.
黄汉纯,周显强,王长利.1989.柴达木盆地构造演化与石油富集规律.地质论评,35(4):314～322.
黄立功,钟建华,郭泽清,等.2004.阿尔金造山带中、新生代的演化.地球学报,25(3):287～294.
靳久强,赵文智,薛良清,等.1999.中国西北地区侏罗纪原型盆地与演化特征.地质论评,45(1):92～104.
金之钧,张明利,汤良杰,等.2004.柴达木中新生代盆地演化及其控油气作用.石油与天然气地质,25(6):603～608.
刘桂侠,杨永泰,管全俊.2003.从冷科1井下部地层的归属探讨柴达木盆地成盆时间.地球学报,24(2):133～136.
罗照华,邓晋福,曹永清,等.1999.青海省东昆仑地区晚古生代—早中生代火山活动与区域构造演化.现代地质,13(1):51～56.
门相勇,李伟,席萍,等.2001.柴达木盆地北缘沉积凝灰质岩段的地层时代.地质科学,36(2):229～233.
青藏油气区石油地质志编写组.1990.中国石油地质志(卷十四).青藏油气区.北京:石油工业出版社,20～59.
王明儒,胡文义,彭德华.1997.柴达木盆地北缘侏罗系油气前景.石油勘探与开发,24(5):20～24.
巫礼玉.1992.柴达木盆地晚三叠世孢粉组合.见:中国油气区地层古生物编辑委员会.中国油气区地层古生物论文集(3).北京:石油工业出版社,144～149.
席萍,唐伦和.1999.柴达木盆地北部地区下侏罗统湖西山组孢粉化石.见:朱宗浩,郑国光,赵付本编.中国含油气盆地孢粉学论文集.北京:石油工业出版社,139～144.
夏文臣,张宁,袁晓萍,等.1998.柴达木侏罗系的构造层序及前陆盆地演化.石油与天然气地质,19(3):173～180.
薛良清,李文厚,宋立珩,等.2000.西北地区侏罗纪原始沉积区恢复.沉积学报,18(4):539～543.
杨永泰,刘桂侠,贾兴友,等.2002.柴达木盆地北缘上三叠统—侏罗系层序特征与含油气系统划分.地球学报,23(1):67～72.
尹安.2001.喜马拉雅—青藏高原造山带地质演化——显生宙亚洲大陆生长.地球学报,22(3):193～230.
曾联波,金之钧,张明利,等.2002.柴达木侏罗纪盆地性质及其演化特征.沉积学报,20(2):288～292.
翟光明,徐风银,李建青,等.1997.重新认识柴达木盆地,力争油气勘探获得新突破.石油学报,18(2):1～7.
张志成,郭召杰,韩作振.1998.敦煌盆地中侏罗世火山岩的地球化学特征及其地质意义.北京大学学报(自然科学版),34(1):72～79.
郑建京等,彭作林.1995.中国主要含油气盆地运动学过程与油气.沉积学报,13(2):160～168.
左国朝,刘义科,李相博,等.2004.蒙甘青宁地区侏罗纪开合盆山构造格局及原型盆地沉积特征.地质通报,23(3):261～271.
An Yin.2001.Geologic Evolution of the Himalayan-Tibetan Orogen in theContext of Phanerozoic Continental Growth.Acta Geoscientia Sinica,22(3):193～230(in Chinese).
Bradley D R,Ulderico B.2000.Magnitude of post-Middle Jurassic(Bajo-cian)displacement on the central Altyn Tagh fault system,northwestChina.GSA Bulletin,112(1):61～74.
Che Zicheng.1986.The formation and evolution of Qaidam basin in rela-tion to the uplift of Qinghai-Tibet plateau.Oil&Gas Geology,7(1):87～94(in Chinese with English abstract).
Chen Fajing,Wang Xinwen.2000.Prototype analysis of early-middle Ju-rassic basins in northwestern China.Earth Science Frontiers(ChinaUniversity of Geosciences,Beijing),7(4):459～468(in Chinesewith English abstract).
Chen Ronglin,Zhu Hongfa,Chen Yue,et al.1994.Astudy of sedimentarycharacteristics and petrollferousness in the Jurassic sequences of thefault region,the SE Tarim basin.Experimental and Petroleum Geolo-gy,16(4):339～344(in Chinese with English abstract).
Chen Xuanhua,An Yin,George E G,et al.2002.Mesozoic Extension inNorthern Tibetan Plataeu:40Ar/39Ar Analyses and MDD Modeling.Acta Geoscientia Sinica,23(4):305～310(in Chinese with Eng-lish abstract).
Di Hengshu.1984.Overthrust belts on the northern margin of Qaidam ba-sin and their oil prospecting.Oil&Gas Geology,5(2):79～87(inChinese with English abstract).
Editorial Committee of"Petroleum Geology of Qinghai-Tebit of China".1990.Petroleum Geology of China.Vol.14.Qinghai-Tibet Region.Beijing:Petroleum Industry Press,20～59(in Chinese).
Gao Xianzhi,Chen Fajing,Ma Dade,et al.2003.Tectonic evolution of theNorthern Qaidam basin during Mesozoic and Cenozoic eras.North-western Geology,36(4):16～24(in Chinese with English ab-stract).
Ge Xiaohong,Zhang Mmeisheng,Liu Yongjiang,et al.1998.Scientificproblems and thought for research of the Altun Fault.Journal ofGraduate School,China University of Geosciences,12(3):295～301(in Chinese with English abstract).
Gu Shusong,Di Hengshu.1990.Formation Mechanism and its controllingon oil and gas in the Qaidam basin.See:Zhu Xia.The sedimentarybasins of Mesozoic and Cenozoic in China.Beijing:Petroleum Indus-try Press,186～195(in Chinese).
Guo Zhaojie,Zhang Zhicheng.1998.Structural style and tectonic evolu-tion of basins in the Altun region.Geological Review,44(4):357～364(in Chinese with English abstract).
Guo Zhengfu,Deng Jinfu,Xu Zhiqin,et al.1998.Late Paleozoic-Mesozoicintracontinental orogenic process and intermediate-acidic igneousrocks from the eastern Kunlun mountains of northwestern China.Ge-oscience,12(3):344～352(in Chinese with English abstract).
He Zhonghua,Liu Zhaojun,Guo Wei,et al.2002.The genetic type of theMesozoic basin in northern Chaida mu and it tectonic-sedimentary e-volution.Journal of Jilin University(Earth Science Edition),32(4):333～339(in Chinese with English abstract).
Hu Shouquan,Cao Yunjiang,Huang Jixiang,et al.1999.Discussion onformation and evolution of Jurassic basin-prototype of Qaidam basin.Experimental and Petroleum Geology,1999,21(3):189～195(inChinese with English abstract).
Huang Hanchun,Zhou Xianqiang,Wang Changli.1989.Geological Re-view,35(4):314～322(in Chinese with English abstract).
Huang Ligong,Zhong Jianhua,Guo Zeqing,et al.2004.Evolution of theAltun Orogenic Belt in the Mesozoic and Cenozoic.Acta Geoscienc-tica Sinaca,25(3):287～294(in Chinese with English abstract).
Jin Jiuqiang,Zhao Wenzhi,Xue Liangqing,et al.1999.Proto-types and e-volution of Jurassic basins in NWChina.Geological Review,45(1):92～104(in Chinese with English abstract).
Jin Zhijun,Zhang Mingli,Tang Liangjie,et al.2004.Evolution of Meso-Cenozoic Qaidam basin and its control on oil and gas.Oil&Gas Ge-ology,25(6):603～608(in Chinese with English abstract).
Liu Guixia,Yang Yongtai,Guan Quanjun.2003.Inquiry of iniciation ageof the Qaidam basin based on stratigraphic study of the lower part ofthe well Lengke1.Acta Geoscientia Sinica,24(2):133～136(inChinese with English abstract).
Luo Zhaohua,Deng Jinfu,Cao Yongqing,et al.1999.On Late Paleozoic-Early Mesozoic volcanism and regional tectonic evolution of EasternKunlun,Qinghai province.Geoscience,13(1):51～56(in Chinesewith English abstract).
Meng Xiangyong,Li Wei,Xi Ping,et al.2001.Stratigraphic time of sedi-mentary tuffaceous bed in north Qaidam basin.Chinese Journal ofGeology,36(2):229～233(in Chinese with English abstract).
Wang Mingru,Hu Wenyi,Peng Dehua.1997.Oil and gas potential of Ju-rassic strata in northern margin of Qaidam basin.Petroleum explora-tion and development,24(5):20～24(in Chinese with English ab-stract).
Wu Liyu.1992.Late Triassic Sporo-pollen assemblages in the Caidam Ba-sin,Qinghai Province.See:Editorial committee of stratigraphy andpalaeontology of oil and gas bearing areas in China.Stratigraphy andpalaeontology of oil and gas bearing areas in China(3).Beijing:Pe-troleum Industry Press,144～149(in Chinese).
Xi Ping,Tang Lunhe.1999.The fossil Sporopollen of Huxishan Formationof the lower Jurassic in the northern region of the Qaidam basin.See:Zhu Zonghao,Zheng Guoguang,Zhao Fuben.Symposium onpalynology of petroliferous basins in China.Beijing:Petroleum In-dustry Press,139～144(in Chinese).
Xia Wenchen,Zhang Ning,Yuan Xiaoping,et al.1998.Jurassic tectonicssequences of Qaidam and foreland basin evolution.Oil&Gas Geolo-gy,19(3):173～180(in Chinese with English abstract).
Xue Liangqing,Li Wenhou,Song Liheng,et al.2000.Reconstruction of o-riginal sedimentary province of the Jurassic in the Northwestern Chi-na.Acta Sedimentary Sinca,18(4):539～543(in Chinese withEnglish abstract).
Yang Yongtai,Liu Guixia,Jia Xingyou,et al.2002.Characteristics of stra-tigraphic sequence and classification of petroleum systems in thenorthern Qaibam basin.Acta Geoscientia Sinica,23(1):67～72(in Chinese with English abstract).
Zen Lianbo,Jin Zhijun,Zhang Mingli,et al.2002.The Jurassic basin typeand its evolution characteristic in Qaidam Basin.Acta SedimentarySinca,20(2):288～292(in Chinese with English abstract).
Zhai Guangming,Xu Fengyin,Li Jianqing,et al.1997.A recondiration ofQaidam basin for a great breakthrough in oil and natural gas explora-tion.Acta Petrolei Sinica,18(2):1～7(in Chinese with Englishabstract).
Zhang Zhicheng,Guo Zhaojie,Han Zuozhen.1998.Geochemistry and Ge-ological Significance of the Mid-Jurassic Volcanic Rocks in Dun-huang Basin.Acta Scientiarum Naturalium Universitatis Pekinensis,34(1):72～79(in Chinese with English abstract).
Zhen Jianjing,Pen Zuolin.1995.Tectonic Kinematic Process of ChiefOil-gas Bearing Basin and the Formation of Oil-gas in China.ActaSedimentary Sinca,13(2):160～168(in Chinese with English ab-stract).
Zuo Guochao,Liu Yike,Li Xiangbo,et al.2004.Jurassic basin-range tec-tonic pattern and depositional features of prototype basins in the in-ner Mongolia-Gansu-Qinghai-Ningxia region.Geological Bulletin ofChina,23(3):261～271(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