柴达木盆地及邻区侏罗纪原型盆地恢复及油气勘探前景
|
摘要
侏罗系是柴达木盆地最重要的源储层系之一。通过野外地质、剖面实测、地震解释、显微构造分析等大量系列资料的综合应用与分析,认为研究区自中生代以来,经历了印支期右行逆冲-走滑构造运动、早—中侏罗世伸展运动、早白垩世北西-南东向挤压及新生代南北向挤压运动,它们与早侏罗世至中侏罗世早期(小煤沟组至大煤沟组)在NE向伸展应力场作用下形成的断陷盆地、中侏罗世晚期至晚侏罗世(彩石岭组—洪水沟组)热力沉降坳陷盆地、早白垩世南北向挤压坳陷盆地密切相关。侏罗纪原型盆地发育三类沉积边界,即盆缘不整合边界(缓坡型和陡坡型边界)、盆内正断层边界、后期逆断层改造边界。不同的现存盆地边界类型对原型盆地恢复的作用不同。侏罗纪盆地以东昆仑构造带为界具有"北陆南洋"的古地理格局,柴达木地区的侏罗纪盆地主要发育在沿岸造山带和岛弧带的山前坳陷以及薄弱的柴北缘加里东俯冲碰撞带之上,形成相对分隔的独立盆地群。柴达木早、中、晚侏罗世原型盆地的分布因受到古特提斯洋向北偏东方向的俯冲作用和阿尔金断裂左旋走滑作用的影响,其沉积中心和沉积范围呈现出从早到晚向东北方向逐渐迁移的规律。早侏罗世盆地的沉积沉降中心主要位于柴北缘西部的冷湖—马海一带,中侏罗世盆地的沉积沉降中心主要位于柴北缘中段的大柴旦—怀头他拉一带,而晚侏罗世盆地的沉积沉降中心主要位于德令哈—乌兰一带。
The Jurassic is one of the most important sources and reservoirs in the Qaidam Basin.In this report,we conducted a comprehensive study on field geology,profile measurement,seismic interpretation and microscopic structural features of the study area in the Qaidam Basin.The results indicate the study area experienced the Indo-Chinese tectonic movement of right thrust and strike-slip structure in the Late Triassic,stretch movement in the Early to Middle Jurassic,NW-SE compressive stress in the Early Cretaceous,and NS compressional stress in the Cenozoic since the Mesozoic.These tectonic events can be related to the Early Jurassic fault basin formed by the NE stretch stress field,the Middle to Late Jurassic depression basin by the thermal subsidence,and the Early Cretaceous NS compressional depression basin.Three types of sedimentary boundary developed in the Jurassic prototype basin:the unconformity boundary at the edge of the basin(Gentle or steep slope),the normal fault boundary within the sedimentary basin,and the reverse fault reconstruction boundary in the later period.And different existing basin boundary types have different effects on the restoration of the prototype basin.The Jurassic basin East Kunlun tectonic belt boundary has the ancient geographical pattern of"northern land and southern ocean".Jurassic basin in the Qaidam region is mainly developed in the foreland depression of coastal orogenic and island arc belts as well as the Caledonian subduction collision zone on the northern margin,forming a relatively separate and independent basin group.The development of the Qaidam prototype basin is affected by the subduction of the Paleotethys Ocean northward and the left-lateral slip fault of Altyn tagh.The sedimentary center and range assumed the law of gradual migration to the northeast from Early to Late Jurassic.The sedimentary and subsidence centers of Early Jurassic basin are located mainly in the Lenghu-Mahai area in western Qaidam Basin,and that of Middle and Late Jurassic basins are located in the Dachaidan-Huaitoutala and Delinha-Wulan areas,respectively.
The Jurassic is one of the most important sources and reservoirs in the Qaidam Basin.In this report,we conducted a comprehensive study on field geology,profile measurement,seismic interpretation and microscopic structural features of the study area in the Qaidam Basin.The results indicate the study area experienced the Indo-Chinese tectonic movement of right thrust and strike-slip structure in the Late Triassic,stretch movement in the Early to Middle Jurassic,NW-SE compressive stress in the Early Cretaceous,and NS compressional stress in the Cenozoic since the Mesozoic.These tectonic events can be related to the Early Jurassic fault basin formed by the NE stretch stress field,the Middle to Late Jurassic depression basin by the thermal subsidence,and the Early Cretaceous NS compressional depression basin.Three types of sedimentary boundary developed in the Jurassic prototype basin:the unconformity boundary at the edge of the basin(Gentle or steep slope),the normal fault boundary within the sedimentary basin,and the reverse fault reconstruction boundary in the later period.And different existing basin boundary types have different effects on the restoration of the prototype basin.The Jurassic basin East Kunlun tectonic belt boundary has the ancient geographical pattern of"northern land and southern ocean".Jurassic basin in the Qaidam region is mainly developed in the foreland depression of coastal orogenic and island arc belts as well as the Caledonian subduction collision zone on the northern margin,forming a relatively separate and independent basin group.The development of the Qaidam prototype basin is affected by the subduction of the Paleotethys Ocean northward and the left-lateral slip fault of Altyn tagh.The sedimentary center and range assumed the law of gradual migration to the northeast from Early to Late Jurassic.The sedimentary and subsidence centers of Early Jurassic basin are located mainly in the Lenghu-Mahai area in western Qaidam Basin,and that of Middle and Late Jurassic basins are located in the Dachaidan-Huaitoutala and Delinha-Wulan areas,respectively.
引文
[1] KLEMME H D.Petroleum basin:classifications and characteristics[J].Journal of Petroleum Geology,1980,3(3):187-207.
[2] BALLY A W.Basin and subsidence:a summary[M]∥BALLY A W,BENDER P L,MCGET T R,et al.Dynamics of plate interiors.AGUGS Geodynamics Series,American Geophysical Union.Washington D C:Geological Society of America,1980,1:5-20.
[3] MIALL A D.Principles of sedimentary basin analysis[M].New York,Beilin,Heidelberg,Tokyo:Springer-Verlag,1984:371-444.
[4] MIALL A D.Principles of sedimentary basin analysis[M].Beilin,Heidelberg:Springer-Verlag,2000:467-577.
[5] ALLEN P A,ALLEN J R.Basin analysis,principle and application[M].Oxford:Blackwell Scientific Publications,1990.
[6] ALLEN P A,ALLEN J R.Basin analysis,principle and application[M].2nd ed.Oxford:Blackwell Scientific Publications,2005.
[7] LEIGTON M W,KOLATA D R,OLTZ D F,等.内克拉通盆地[M].刘里斌,于福华,杨时榜,等译.北京:石油工业出版社,2000.
[8]张渝昌.石油实验地质中的盆地分析[J].石油实验地质,1990,18(4):12-16.
[9]刘池洋.后期改造强烈:中国沉积盆地的重要特点之一[J].石油与天然气地质,1996,17(4):255-261.
[10]刘池洋,孙海山.改造型盆地类型划分[J].新疆石油地质,1999,20(2):79-82,168.
[11]刘池洋,赵重远,杨兴科.活动性强、深部作用活跃:中国沉积盆地的两个重要特点[J].石油与天然气地质,2000,21(1):1-6.
[12]刘池洋,张复新,高飞.沉积盆地成藏(矿)系统[J].中国地质,2007,34(3):365-374.
[13]刘池洋,王建强,赵红格,等.沉积盆地类型划分及其相关问题讨论[J].地学前缘,2015,22(3):1-26.
[14]童晓光,何登发.油气勘探原理和方法[M].北京:石油工业出版社,2001:32-39.
[15]何登发,贾承造,童晓光,等.叠合盆地概念辨析[J].石油勘探与开发,2004,31(1):1-7.
[16]何登发,周新源,张朝军,等.塔里木地区奥陶纪原型盆地类型及其演化[J].科学通报,2007,52(增刊Ⅰ):126-135.
[17]何登发,李德生,王成善,等.中国沉积盆地深层构造地质学的研究进展与展望[J].地学前缘,2017,24(3):219-233.
[18]陈发景,汪新文.中国西北地区早—中侏罗世盆地原型分析[J].地学前缘,2000,7(4):459-469.
[19]陈发景,汪新文,汪新伟.准噶尔盆地的原型和构造演化[J].地学前缘,2005,12(3):77-89.
[20] DICKINSON W R,ANDERSON R N,BIDDLE K T,et al.The dynamics of sedimentary basins[M].Washington:National Academy Press,1997:1-43.
[21]温志新,童晓光,张光亚,等.全球板块构造演化过程中五大成盆期原型盆地的形成、改造及叠加过程[J].地学前缘,2014,21(3):36-37.
[22]琚宜文,孙盈,王国昌,等.盆地形成与演化的动力学类型及其地球动力学机制[J].地质科学,2015,50(2):503-523.
[23]汪祖智.柴达木盆地北缘中生界沉积分布特征[J].石油勘探与开发,1981,8(2):20-26.
[24]岳鹏升,王平,郁东良,等.柴达木盆地北缘下中侏罗统沉积特征及其石油地质意义[J].海洋地质前沿,2011,27(11):38-44.
[25]杨永泰,刘桂侠,贾兴友,等.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[J].地球学报,2002,23(1):67-72.
[26]杜建军,张士安,肖伟峰.等.柴达木盆地北缘中—下侏罗统碎屑岩地球化学特征及其地质意义[J].地球科学与环境学报,2017,39(6):721-734.
[27]郭佳佳,孙国强,龙国徽,等.柴达木盆地北缘冷湖五号构造下侏罗统沉积-成岩环境分析[J].天然气地球科学,2017,28(12):1839-1845.
[28]汤良杰,金之钧,张明利,等.柴达木盆地北缘构造演化与油气成藏阶段[J].石油勘探与开发,2000,27(2):36-39.
[29]周建勋,徐凤银,朱战军.从反转构造的砂箱模型看柴达木早—中侏罗世盆地的构造性质[J].地质科学,2002,37(4):430-435.
[30]周建勋,徐凤银,胡勇.柴达木盆地北缘中、新生代构造变形及其对油气成藏的控制[J].石油学报,2003,24(1):19-24.
[31]郑孟林,李明杰,曹春潮,等.柴达木北缘西段侏罗纪盆地构造特征及其演化[J].石油实验地质,2004,26(4):315-318.
[32]汤良杰,金之钧,张明利,等.柴达木盆地构造古地理分析[J].地学前缘,2000,7(4):421-429.
[33]谢庆宾,管守锐.从岩相古地理看柴达木盆地侏罗系的油气前景[J].古地理学报,2003,5(4):475-485.
[34]胡受权,曹运江,黄继祥,等.柴达木盆地侏罗纪盆地原型及其形成与演化探讨[J].石油实验地质,1999,21(3):189-195.
[35]李军亮,肖永军,王大华,等.柴达木盆地东部侏罗纪原型盆地恢复[J].地学前缘,2016,23(5):11-22.
[36]付锁堂,袁剑英,汪立群,等.柴达木盆地油气地质成藏条件研究[M].北京:科学出版社,2015.
[37]青海省地质局第一区调队.1∶20万怀头他拉幅区域地质调查报告(J-47-19)[R].北京:地质出版社,1980:73-77.
[38]鲁静,邵龙义,鞠奇,等.柴北缘大煤沟矿区侏罗纪煤系层序地层及其煤岩变化特征[J].煤田地质与勘探,2009,37(4):9-14.
[39]鲁静,邵龙义,杨敏芳,等.陆相盆地沼泽体系煤相演化、层序地层与古环境[J].煤炭学报,2014,39(12):2473-2481.
[40]青海省地质矿产局.青海省区域地质志[M].北京:地质出版社,1991:181-185.
[41]杨永泰,张宝民,李伟,等.柴达木盆地北缘侏罗系层序地层与沉积相研究[J].地学前缘,2000,7(3):145-151.
[42]金振奎,齐聪伟,薛建勤,等.柴达木盆地北缘侏罗系沉积相[J].古地理学报,2006,18(2):199-210.
[43]阎存凤,袁剑英,陈启林.柴达木盆地北缘东段中下侏罗统孢粉相及生烃潜力[J].地球科学进展,2007,22(12):1268-1273.
[44]魏彬炎.青海省北半部陆相侏罗系地层[J].煤田地质与勘探,1978,6(4):16-30.
[45]何元良.青海省陆相侏罗系划分的初步探讨[J].青藏高原地质文集,1984,14(1):165-184.
[46]杨平,谢宗奎,袁秀君.柴达木盆地北缘侏罗纪古生态特征及其古地理意义[J].古地理学报,2006,18(12):165-173.
[47]杨平,杨玉芹,马立协,等.柴达木盆地北缘侏罗系沉积环境演变及其石油地质意义[J].石油勘探与开发,2007,34(2):160-164.
[48]孙洪杰,雷敏,王大华,等.柴达木盆地北缘东部侏罗系发育特征[J].世界地质,2013,32(3):531-538.
[49]杨德寿,范文科,林文良.柴达木盆地北缘侏罗系含煤研究[J].中国煤炭地质,2011,23(2):4-10.
[50]邓胜徽,卢远征,樊茹,等.早侏罗世Toarcian期大洋缺氧事件及其在陆地生态系统中的响应[J].地球科学:中国地质大学学报,2012,37(增刊2):23-38.
[51]冯益民,何世平.祁连山大地构造与造山作用[M].北京:地质出版社,1996.
[52]冯益民.祁连造山带研究概况:历史、现状及展望[J].地球科学进展,1997,12(4):307-314.
[53]夏林圻,夏祖春,徐学义.北祁连山早古生代洋脊-洋岛和弧后盆地火山作用[J].地质学报,1998,72(4):301-312.
[54]许志琴,杨经绥,姜枚,等.大陆俯冲作用及青藏高原周缘造山带的崛起[J].地学前缘,1999,6(3):139-151.
[55]许志琴,杨经缓,吴才来,等.柴达木北缘超高压变质带形成与折返的时限及机制[J].地质学报,2003,77(2):163-176.
[56]戴传固,李硕,边申武.青藏高原北缘昆仑—羊湖地区构造演化特征[J].贵州地质,2006,23(1):1-4.
[57]夏文臣,张宁,袁晓萍,等.柴达木侏罗系的构造层序及前陆盆地演化[J].石油与天然气地质,1998,19(3):173-181.
[58]杨明慧.德令哈中生代沉积盆地成因类型及其与南祁连造山带的关系[J].西北地质科学,1999,20(1):15-22.
[59]胡授权,曹运江,黄继祥,等.柴达木盆地北缘地区前陆盆地演化及油气勘探目标[J].天然气工业,1999,19(4):1-5.
[60]胡授权,郭文凭,曹运江,等.柴达木盆地北缘构造格局及在中新生代的演化[J].新疆石油地质,2001,22(1):13-18.
[61]和钟铧,刘招君,郭巍,等.柴达木北缘中生代盆地的成因类型及构造沉积演化[J].吉林大学学报:地球科学版,2002,32(4):333-339.
[62]靳久强,赵文智,薛良清.中国西北地区侏罗纪原型盆地与演化特征[J].地质论评,1999,45(1):92-104.
[63]汪劲草,胡勇,刘云田.多世代旋转正断层对断陷盆地沉积迁移的控制:柴达木早、中侏罗世盆地性质[J].地质学报,2006,80(8):1141-1148.
[64]李伟,刘宝珺,白淑艳.柴达木盆地侏罗系地层沉积大迁移及成因分析[J].石油学报,2002,23(6):16-19.
[65]曾联波,金之钧,张明利,等.柴达木侏罗纪盆地性质及其演化特征[J].沉积学报,2002,20(2):288-292.
[66]刘平,王英超.柴达木侏罗纪盆地是“前陆盆地”吗?[J].天然气工业,2006,26(2):43-45.
[67]党玉琪,马达德,汪立群,等.认识再升华勘探无止境:从柴北缘勘探历程看南八仙-马北油气田的发现[C]∥中国西部科技进步与经济社会发展专家论坛专辑(九).西安:青海省科技协会,2007:352-356.
[2] BALLY A W.Basin and subsidence:a summary[M]∥BALLY A W,BENDER P L,MCGET T R,et al.Dynamics of plate interiors.AGUGS Geodynamics Series,American Geophysical Union.Washington D C:Geological Society of America,1980,1:5-20.
[3] MIALL A D.Principles of sedimentary basin analysis[M].New York,Beilin,Heidelberg,Tokyo:Springer-Verlag,1984:371-444.
[4] MIALL A D.Principles of sedimentary basin analysis[M].Beilin,Heidelberg:Springer-Verlag,2000:467-577.
[5] ALLEN P A,ALLEN J R.Basin analysis,principle and application[M].Oxford:Blackwell Scientific Publications,1990.
[6] ALLEN P A,ALLEN J R.Basin analysis,principle and application[M].2nd ed.Oxford:Blackwell Scientific Publications,2005.
[7] LEIGTON M W,KOLATA D R,OLTZ D F,等.内克拉通盆地[M].刘里斌,于福华,杨时榜,等译.北京:石油工业出版社,2000.
[8]张渝昌.石油实验地质中的盆地分析[J].石油实验地质,1990,18(4):12-16.
[9]刘池洋.后期改造强烈:中国沉积盆地的重要特点之一[J].石油与天然气地质,1996,17(4):255-261.
[10]刘池洋,孙海山.改造型盆地类型划分[J].新疆石油地质,1999,20(2):79-82,168.
[11]刘池洋,赵重远,杨兴科.活动性强、深部作用活跃:中国沉积盆地的两个重要特点[J].石油与天然气地质,2000,21(1):1-6.
[12]刘池洋,张复新,高飞.沉积盆地成藏(矿)系统[J].中国地质,2007,34(3):365-374.
[13]刘池洋,王建强,赵红格,等.沉积盆地类型划分及其相关问题讨论[J].地学前缘,2015,22(3):1-26.
[14]童晓光,何登发.油气勘探原理和方法[M].北京:石油工业出版社,2001:32-39.
[15]何登发,贾承造,童晓光,等.叠合盆地概念辨析[J].石油勘探与开发,2004,31(1):1-7.
[16]何登发,周新源,张朝军,等.塔里木地区奥陶纪原型盆地类型及其演化[J].科学通报,2007,52(增刊Ⅰ):126-135.
[17]何登发,李德生,王成善,等.中国沉积盆地深层构造地质学的研究进展与展望[J].地学前缘,2017,24(3):219-233.
[18]陈发景,汪新文.中国西北地区早—中侏罗世盆地原型分析[J].地学前缘,2000,7(4):459-469.
[19]陈发景,汪新文,汪新伟.准噶尔盆地的原型和构造演化[J].地学前缘,2005,12(3):77-89.
[20] DICKINSON W R,ANDERSON R N,BIDDLE K T,et al.The dynamics of sedimentary basins[M].Washington:National Academy Press,1997:1-43.
[21]温志新,童晓光,张光亚,等.全球板块构造演化过程中五大成盆期原型盆地的形成、改造及叠加过程[J].地学前缘,2014,21(3):36-37.
[22]琚宜文,孙盈,王国昌,等.盆地形成与演化的动力学类型及其地球动力学机制[J].地质科学,2015,50(2):503-523.
[23]汪祖智.柴达木盆地北缘中生界沉积分布特征[J].石油勘探与开发,1981,8(2):20-26.
[24]岳鹏升,王平,郁东良,等.柴达木盆地北缘下中侏罗统沉积特征及其石油地质意义[J].海洋地质前沿,2011,27(11):38-44.
[25]杨永泰,刘桂侠,贾兴友,等.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[J].地球学报,2002,23(1):67-72.
[26]杜建军,张士安,肖伟峰.等.柴达木盆地北缘中—下侏罗统碎屑岩地球化学特征及其地质意义[J].地球科学与环境学报,2017,39(6):721-734.
[27]郭佳佳,孙国强,龙国徽,等.柴达木盆地北缘冷湖五号构造下侏罗统沉积-成岩环境分析[J].天然气地球科学,2017,28(12):1839-1845.
[28]汤良杰,金之钧,张明利,等.柴达木盆地北缘构造演化与油气成藏阶段[J].石油勘探与开发,2000,27(2):36-39.
[29]周建勋,徐凤银,朱战军.从反转构造的砂箱模型看柴达木早—中侏罗世盆地的构造性质[J].地质科学,2002,37(4):430-435.
[30]周建勋,徐凤银,胡勇.柴达木盆地北缘中、新生代构造变形及其对油气成藏的控制[J].石油学报,2003,24(1):19-24.
[31]郑孟林,李明杰,曹春潮,等.柴达木北缘西段侏罗纪盆地构造特征及其演化[J].石油实验地质,2004,26(4):315-318.
[32]汤良杰,金之钧,张明利,等.柴达木盆地构造古地理分析[J].地学前缘,2000,7(4):421-429.
[33]谢庆宾,管守锐.从岩相古地理看柴达木盆地侏罗系的油气前景[J].古地理学报,2003,5(4):475-485.
[34]胡受权,曹运江,黄继祥,等.柴达木盆地侏罗纪盆地原型及其形成与演化探讨[J].石油实验地质,1999,21(3):189-195.
[35]李军亮,肖永军,王大华,等.柴达木盆地东部侏罗纪原型盆地恢复[J].地学前缘,2016,23(5):11-22.
[36]付锁堂,袁剑英,汪立群,等.柴达木盆地油气地质成藏条件研究[M].北京:科学出版社,2015.
[37]青海省地质局第一区调队.1∶20万怀头他拉幅区域地质调查报告(J-47-19)[R].北京:地质出版社,1980:73-77.
[38]鲁静,邵龙义,鞠奇,等.柴北缘大煤沟矿区侏罗纪煤系层序地层及其煤岩变化特征[J].煤田地质与勘探,2009,37(4):9-14.
[39]鲁静,邵龙义,杨敏芳,等.陆相盆地沼泽体系煤相演化、层序地层与古环境[J].煤炭学报,2014,39(12):2473-2481.
[40]青海省地质矿产局.青海省区域地质志[M].北京:地质出版社,1991:181-185.
[41]杨永泰,张宝民,李伟,等.柴达木盆地北缘侏罗系层序地层与沉积相研究[J].地学前缘,2000,7(3):145-151.
[42]金振奎,齐聪伟,薛建勤,等.柴达木盆地北缘侏罗系沉积相[J].古地理学报,2006,18(2):199-210.
[43]阎存凤,袁剑英,陈启林.柴达木盆地北缘东段中下侏罗统孢粉相及生烃潜力[J].地球科学进展,2007,22(12):1268-1273.
[44]魏彬炎.青海省北半部陆相侏罗系地层[J].煤田地质与勘探,1978,6(4):16-30.
[45]何元良.青海省陆相侏罗系划分的初步探讨[J].青藏高原地质文集,1984,14(1):165-184.
[46]杨平,谢宗奎,袁秀君.柴达木盆地北缘侏罗纪古生态特征及其古地理意义[J].古地理学报,2006,18(12):165-173.
[47]杨平,杨玉芹,马立协,等.柴达木盆地北缘侏罗系沉积环境演变及其石油地质意义[J].石油勘探与开发,2007,34(2):160-164.
[48]孙洪杰,雷敏,王大华,等.柴达木盆地北缘东部侏罗系发育特征[J].世界地质,2013,32(3):531-538.
[49]杨德寿,范文科,林文良.柴达木盆地北缘侏罗系含煤研究[J].中国煤炭地质,2011,23(2):4-10.
[50]邓胜徽,卢远征,樊茹,等.早侏罗世Toarcian期大洋缺氧事件及其在陆地生态系统中的响应[J].地球科学:中国地质大学学报,2012,37(增刊2):23-38.
[51]冯益民,何世平.祁连山大地构造与造山作用[M].北京:地质出版社,1996.
[52]冯益民.祁连造山带研究概况:历史、现状及展望[J].地球科学进展,1997,12(4):307-314.
[53]夏林圻,夏祖春,徐学义.北祁连山早古生代洋脊-洋岛和弧后盆地火山作用[J].地质学报,1998,72(4):301-312.
[54]许志琴,杨经绥,姜枚,等.大陆俯冲作用及青藏高原周缘造山带的崛起[J].地学前缘,1999,6(3):139-151.
[55]许志琴,杨经缓,吴才来,等.柴达木北缘超高压变质带形成与折返的时限及机制[J].地质学报,2003,77(2):163-176.
[56]戴传固,李硕,边申武.青藏高原北缘昆仑—羊湖地区构造演化特征[J].贵州地质,2006,23(1):1-4.
[57]夏文臣,张宁,袁晓萍,等.柴达木侏罗系的构造层序及前陆盆地演化[J].石油与天然气地质,1998,19(3):173-181.
[58]杨明慧.德令哈中生代沉积盆地成因类型及其与南祁连造山带的关系[J].西北地质科学,1999,20(1):15-22.
[59]胡授权,曹运江,黄继祥,等.柴达木盆地北缘地区前陆盆地演化及油气勘探目标[J].天然气工业,1999,19(4):1-5.
[60]胡授权,郭文凭,曹运江,等.柴达木盆地北缘构造格局及在中新生代的演化[J].新疆石油地质,2001,22(1):13-18.
[61]和钟铧,刘招君,郭巍,等.柴达木北缘中生代盆地的成因类型及构造沉积演化[J].吉林大学学报:地球科学版,2002,32(4):333-339.
[62]靳久强,赵文智,薛良清.中国西北地区侏罗纪原型盆地与演化特征[J].地质论评,1999,45(1):92-104.
[63]汪劲草,胡勇,刘云田.多世代旋转正断层对断陷盆地沉积迁移的控制:柴达木早、中侏罗世盆地性质[J].地质学报,2006,80(8):1141-1148.
[64]李伟,刘宝珺,白淑艳.柴达木盆地侏罗系地层沉积大迁移及成因分析[J].石油学报,2002,23(6):16-19.
[65]曾联波,金之钧,张明利,等.柴达木侏罗纪盆地性质及其演化特征[J].沉积学报,2002,20(2):288-292.
[66]刘平,王英超.柴达木侏罗纪盆地是“前陆盆地”吗?[J].天然气工业,2006,26(2):43-45.
[67]党玉琪,马达德,汪立群,等.认识再升华勘探无止境:从柴北缘勘探历程看南八仙-马北油气田的发现[C]∥中国西部科技进步与经济社会发展专家论坛专辑(九).西安:青海省科技协会,2007:352-356.
© 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 |