高孔隙性砂岩内变形带特征及对流体流动的影响——以柴达木盆地西缘油砂山背斜为例

doi:10.7623/syxb201805006

石油学报 ›› 2018, Vol. 39 ›› Issue (5): 554-563.DOI: 10.7623/syxb201805006

高孔隙性砂岩内变形带特征及对流体流动的影响——以柴达木盆地西缘油砂山背斜为例

王海学^1,2, 刘志达^1,2, 沙威³, 付晓飞^1,2, 孙永河^1,2, 赵政权⁴, 卢明旭⁵, 吴桐^1,2

1. 东北石油大学地球科学学院 CNPC断裂控藏研究室黑龙江大庆 163318;
2. 东北石油大学非常规油气成藏与开发省部共建国家重点实验室培育基地黑龙江大庆 163318;
3. 中国石油青海油田公司勘探开发研究院甘肃敦煌 736202;
4. 中国石油华北油田公司第五采油厂河北辛集 052360;
5. 大庆油田有限责任公司第四采油厂黑龙江大庆 163511

收稿日期:2017-11-29 修回日期:2018-04-08 出版日期:2018-05-25 发布日期:2018-06-06
通讯作者: 刘志达,女,1994年1月生,2014年获东北石油大学学士学位,现为东北石油大学博士研究生,主要从事高孔隙性岩石变形伴生构造方面的研究工作。Email:lzd6536@163.com
作者简介:王海学,男,1987年1月生,2009年获大庆石油学院学士学位,2016年获东北石油大学博士学位,现为东北石油大学讲师,主要从事断层生长机制及控藏作用研究。Email:wanghaixue116@163.com
基金资助:
国家自然科学基金（No.41602129）、国家自然科学基金重点联合基金（No.U1562214）、东北石油大学优秀科研人才培育基金黑龙江省创新后备人才项目（2017-KYYWF-0063）和国家科技重大专项（2016ZX05054-009，2016ZX05003-002）资助。

Characteristics of deformation bands in high-porosity sandstone and their influence on fluid flow: a case study of Youshashan anticline at the western margin of Q aidam Basin

Wang Haixue^1,2, Liu Zhida^1,2, Sha Wei³, Fu Xiaofei^1,2, Sun Yonghe^1,2, Zhao Zhengquan⁴, Lu Mingxu⁵, Wu Tong^1,2

1. College of Earth Science, CNPC Fault Controlling Reservoir Research Laboratory, Northeast Petroleum University, Heilongjiang Daqing 163318, China;
2. Accumulation and Development of Unconventional Oil and Gas, State Key Laboratory Cultivation Base Jointly-constructed by Heilongjiang Province and the Ministry of Science and Technology, Northeast Petroleum University, Heilongjiang Daqing 163318, China;
3. Exploration and Development Institute of PetroChina Qinghai Oilfield Company, Gansu Dunhuang 736202, China;
4. NO.5 Production Plant, PetroChina Huabei Oilfield Company, Hebei Xinji 052360, China;
5. No.4 Oil Recovery Plant, Daqing Oilfield Limited Company, Heilongjiang Daqing 163511, China

Received:2017-11-29 Revised:2018-04-08 Online:2018-05-25 Published:2018-06-06

摘要/Abstract

摘要：

传统观点认为岩石受力变形发生破裂作用形成裂缝，对流体流动起到输导作用。实际上，高孔隙性岩石受力变形，发生颗粒的旋转、滚动、重排和（或）破碎，应变集中形成与裂缝特征截然不同的变形带，降低了储层的孔隙度和渗透率，影响流体的流动。基于野外观察描述和室内分析测试资料，以柴达木盆地西缘油砂山背斜下油砂山组地层为研究对象，从变形带形成机制出发，系统描述了高孔隙性砂岩中变形带的宏观、微观特征，剖析了变形带和未变形母岩的物性特征，明确了变形带形成时期和油气成藏期的耦合关系，探讨了变形带对流体流动的影响。研究结果表明：油砂山背斜带转折端处下油砂山组高孔隙性砂岩受力变形发生了碎裂作用，形成了典型的碎裂型变形带。碎裂型变形带的颜色发白，比母岩浅；呈正风化地形特征，以"肋状"凸出的形态发育；极少单条发育，多呈"簇状"等组合特征发育。微观上，碎裂型变形带表现为颗粒发生旋转、滚动，沿着颗粒接触边界摩擦导致颗粒破碎，颗粒尺寸明显减小、分选变差，带内颜色相对变深和孔隙坍塌、孔隙空间明显降低的特征。与母岩相比，变形带的孔隙度平均降低约17.4%。应用母岩与变形带渗透率比值与流体流动效率的定量图版分析，当变形带渗透率较母岩降低3个数量级以上时，对流体流动起到阻碍作用，油砂山背斜带变形带渗透率降低1~2个数量级，对流体流动基本无明显阻滞作用。

关键词: 高孔隙性砂岩, 变形带, 碎裂作用, 油砂山背斜, 柴达木盆地

Abstract:

It is traditionally considered that the rocks are deformed by force to induce fracturing, and thus form the fractures playing a role of conduction in fluid flow. In fact, the deformation of high-porosity rocks by force leads to the rotation, sliding, disaggregation and/or rupture of particles. The strain concentration results in the deformation bands with characteristics obviously different from fracture, reducing the reservoir porosity and permeability as well as influencing fluid flow. Based on field observation and description and laboratory analysis test data, the Lower Youshashan Formation strata of Youshashan anticline at the western margin of Qaidam Basin is taken as the research object to systematically describe the macro and micro characteristics of deformation bands in high-porosity sandstones in term of deformation-band formation mechanism. Meanwhile, this paper analyzes the petrophysical properties of deformation bands and un-deformed parent rocks, makes clear the coupling relationship between the forming period of deformation band and hydrocarbon accumulation period, and discusses the influence of deformation bands on fluid flow. Research results indicate that the high-porosity sandstones in Youshashan Formation at the hinge zone of Youshashan anticline are deformed by force to induce cataclasis, thus forming the typical cataclastic deformation band. The cataclastic deformation band is white, lighter than parent rock, characterized by positive weathering landform and rib protruding morphology. It rarely shows singular development, dominated by "clustered" assemblage development. On a microscopic level, the cataclastic deformation bands are characterized by rotation and sliding of particles; the frictions along grain contact boundaries lead to the fractured pariticles, obviously decreased grain size, poor sorting, darkening band color, pore collapse, and significant decline of pore space. Compared with parent rock, the porosity of deformation band is reduced by about 17.4% on average. Through applying the quantitative chart of flow efficiency versus the permeability ratio of parent rock and deformation band for analysis, it is found that when the permeability of deformation band is reduced by three orders of magnitude over parent rock, fluid flow is hindered. When the permeability of deformation band in Youshashan Anticline is reduced by 1-2 orders of magnitude, there is basically no obvious hindering effect on fluid flow.

Key words: high-porosity sandstone, deformation band, cataclasis, Youshashan anticline, Qaidam Basin

中图分类号:

TE32

王海学, 刘志达, 沙威, 付晓飞, 孙永河, 赵政权, 卢明旭, 吴桐. 高孔隙性砂岩内变形带特征及对流体流动的影响——以柴达木盆地西缘油砂山背斜为例[J]. 石油学报, 2018, 39(5): 554-563.

Wang Haixue, Liu Zhida, Sha Wei, Fu Xiaofei, Sun Yonghe, Zhao Zhengquan, Lu Mingxu, Wu Tong. Characteristics of deformation bands in high-porosity sandstone and their influence on fluid flow: a case study of Youshashan anticline at the western margin of Q aidam Basin[J]. Acta Petrolei Sinica, 2018, 39(5): 554-563.

参考文献

[1] FOSSEN H,SCHULTZ R A,SHIPTON Z K,et al.Deformation bands in sandstone:a review[J].Journal of the Geological Society,2007,164(4):755-769.
[2] FOSSEN H.Structural geology[M].New York:Cambridge University Press,2010:119-185.
[3] 付晓飞,肖建华,孟令东.断裂在纯净砂岩中的变形机制及断裂带内部结构[J].吉林大学学报:地球科学版,2014,44(1):25-37.
FU Xiaofei,XIAO Jianhua,MENG Lingdong.Fault deformation mechanisms and internal structure characteristics of fault zone in pure sandstone[J].Journal of Jilin University:Earth Science Edition,2014,44(1):25-37.
[4] 黄小娟,李治平,周光亮,等.裂缝性致密砂岩储层裂缝孔隙度建模——以四川盆地平落坝构造须家河组二段储层为例[J].石油学报,2017,38(5):570-577.
HUANG Xiaojuan,LI Zhiping,ZHOU Guangliang,et al.Fracture porosity modeling of fractured tight sandstone reservoir:a case study of the reservoir in Member 2 of Xujiahe Formation,Pingluoba structure,Sichuan Basin[J].Acta Petrolei Sinica,2017,38(5):570-577.
[5] POLLARD D D,FLETCHER R C.Fundamentals of structural geology[M].Cambridge:Cambridge University Press,2005:512.
[6] AYDIN A,JOHNSON A M.Development of faults as zones of deformation bands and as slip surfaces in sandstone[J].Pure and Applied Geophysics,1978,116(4/5):931-942.
[7] ANTONELLINI M,AYDIN A,ORR L.Outcrop-Aided characterization of a faulted hydrocarbon reservoir:arroyo Grande oil field,California,USA[M]//HANEBERG W C,MOZLEY P S,MOORE J C,et al.Faults and Subsurface Fluid Flow in the Shallow Crust.California,USA:American Geophysical Union,1999:7-26.
[8] HESTHAMMER J,FOSSEN H.Uncertainties associated with fault sealing analysis[J].Petroleum Geoscience,2000,6(1):37-45.
[9] FISHER Q J,KNIPE R J.The permeability of faults within siliciclastic petroleum reservoirs of the North Sea and Norwegian Continental Shelf[J].Marine and Petroleum Geology,2001,18(10):1063-1081.
[10] SCHUELLER S,BRAATHEN A,FOSSEN H,et al.Spatial distribution of deformation bands in damage zones of extensional faults in porous sandstones:statistical analysis of field data[J].Journal of Structural Geology,2013,52:148-162.
[11] SCHULTZ R A,FOSSEN H.Terminology for structural discontinuities[J].AAPG Bulletin,2008,92(7):853-867.
[12] 吴婵,阎存凤,李海兵,等.柴达木盆地西部新生代构造演化及其对青藏高原北部生长过程的制约[J].岩石学报,2013,29(6):2211-2222.
WU Chan,YAN Cunfeng,LI Haibing,et al.Cenozoic tectonic evolution of the western Qaidam Basin and its constrain on the growth of the northern Tibetan Plateau[J].Acta Petrologica Sinica,2013,29(6):2211-2222.
[13] 付锁堂,张道伟,薛建勤,等.柴达木盆地致密油形成的地质条件及勘探潜力分析[J].沉积学报,2013,31(4):672-682.
FU Suotang,ZHANG Daowei,XUE Jianqin,et al.Exploration potential and geological conditions of tight oil in the Qaidam Basin[J].Acta Sedimentologica Sinica,2013,31(4):672-682.
[14] 夏志远,刘占国,李森明,等.岩盐成因与发育模式——以柴达木盆地英西地区古近系下干柴沟组为例[J].石油学报,2017,38(1):55-66.
XIA Zhiyuan,LIU Zhanguo,LI Senming,et al.Origin and developing model of rock salt:a case study of Lower Ganchaigou Formation of Paleogene in the west of Yingxiong ridge,Qaidam Basin[J].Acta Petrolei Sinica,2017,38(1):55-66.
[15] 张斌,何媛媛,陈琰,等.柴达木盆地西部咸化湖相优质烃源岩地球化学特征及成藏意义[J].石油学报,2017,38(10):1158-1167.
ZHANG Bin,HE Yuanyuan,CHEN Yan,et al.Geochemical characteristics and oil accumulation significance of the high quality saline lacustrine source rocks in the western Qaidam Basin,NW China[J].Acta Petrolei Sinica,2017,38(10):1158-1167.
[16] 管树巍,张水昌,张永庶,等.柴达木盆地西部古近系生烃凹陷的边界效应与油气聚集模式[J].石油学报,2017,38(11):1217-1229.
GUAN Shuwei,ZHANG Shuichang,ZHANG Yongshu,et al.Boundary effect and hydrocarbon accumulation pattern of Paleogene hydrocarbon-generation depression in the western Qaidam Basin[J].Acta Petrolei Sinica,2017,38(11):1217-1229.
[17] 黄成刚,常海燕,崔俊,等.柴达木盆地西部地区渐新世沉积特征与油气成藏模式[J].石油学报,2017,38(11):1230-1243.
HUANG Chenggang,CHANG Haiyan,CUI Jun,et al.Oligocene sedimentary characteristics and hydrocarbon accumulation model in the western Qaidam Basin[J].Acta Petrolei Sinica,2017,38(11):1230-1243.
[18] 王亚东,张涛,迟云平,等.柴达木盆地西部地区新生代演化特征与青藏高原隆升[J].地学前缘,2011,18(3):141-150.
WANG Yadong,ZHANG Tao,CHI Yunping,et al.Cenozoic uplift of the Tibetan Plateau:evidence from tectonic-sedimentary evolution of the Western Qaidam Basin[J].Earth Science Frontiers,2011,18(3):141-150.
[19] 郭泽清,马寅生,易士威,等.柴西地区古近系-新近系含气系统模拟及勘探方向[J].天然气地球科学,2017,28(1):82-92.
GUO Zeqing,MA Yinsheng,YI Shiwei,et al.Simulation and exploration direction of Paleogene-Neogene gas system in the western Qaidam Basin[J].Natural Gas Geoscience,2017,28(1):82-92.
[20] 赵凡,孙德强,闫存凤,等.柴达木盆地中新生代构造演化及其与油气成藏关系[J].天然气地球科学,2013,24(5):940-947.
ZHAO Fan,SUN Deqiang,YAN Cunfeng,et al.Meso-cenozoic tectonic evolution of Qaidam Basin and its relationship with oil and gas accumulation[J].Natural Gas Geoscience,2013,24(5):940-947.
[21] 何登发,李德生,吕修祥.中国西北地区含油气盆地构造类型[J].石油学报,1996,17(4):8-18.
HE Dengfa,LI Desheng,LV Xiuxiang.Tectonic types of petroliferous basins in NW China[J].Acta Petrolei Sinica,1996,17(4):8-18.
[22] 郭召杰,张志诚.阿尔金盆地群构造类型与演化[J].地质论评,1998,44(4):357-364.
GUO Zhaojie,ZHANG Zhicheng.Structural style and tectonic evolution of the basins in the Altun Region[J].Geological Review,1998,44(4):357-364.
[23] 李相博,袁剑英,陈启林,等.柴达木盆地新生代成盆动力学模式[J].石油学报,2006,27(3):6-10.
LI Xiangbo,YUAN Jianying,CHEN Qilin,et al.Patterns of Cenozoic sedimentary basin-forming dynamics in Qaidam Basin[J].Acta Petrolei Sinica,2006,27(3):6-10.
[24] 肖安成,陈志勇,杨树锋,等.柴达木盆地北缘晚白垩世古构造活动的特征研究[J].地学前缘,2005,12(4):451-457.
XIAO Ancheng,CHEN Zhiyong,YANG Shufeng,et al.The study of Late Cretaceous paleostructural characteristics in northern Qaidam Basin[J].Earth Science Frontiers,2005,12(4):451-457.
[25] 杨藩,叶素娟,曹春潮,等.新生代阿尔金断层中、东段右行走滑特征[J].地质科学,1994,29(4):346-354.
YANG Fan,YE Sujuan,CAO Chunchao,et al.Right lateral characteristics of the middle eastern segment of Altun fault in Cenozoic Era[J].Science Geologica Sinica,1994,29(4):346-354.
[26] 陈正乐,张岳桥,陈宣华,等.阿尔金断裂中段晚新生代走滑过程的沉积响应[J].中国科学(D辑),2001,31(S1):90-96.
CHEN Zhengle,ZHANG Yueqiao,CHEN Xuanhua,et al.Late Cenozoic sedimentary process and its response to the slip history of the central Altyn Tagh fault,NW China[J].Science in China Series D:Earth Sciences,2001,44(S1):103-111.
[27] 魏国齐,贾承造,李本亮.我国中西部前陆盆地的特殊性和多样性及其天然气勘探[J].高校地质学报,2005,11(4):552-557.
WEI Guoqi,JIA Chengzao,LI Benliang.Particularity and diversity of the foreland basins in the central and western China and the natural gas exploration in the foreland basins[J].Geological Journal of China Universities,2005,11(4):552-557.
[28] 付玲,关平,赵为永,等.柴达木盆地古近系路乐河组重矿物特征与物源分析[J].岩石学报,2013,29(8):2867-2875.
FU Ling,GUAN Ping,ZHAO Weiyong,et al.Heavy mineral feature and provenance analysis of paleogene Lulehe formation in Qaidam Basin[J].Acta Petrologica Sinica, 2013,29(8):2867-2875.
[29] 隋立伟,方世虎,孙永河,等.柴达木盆地西部狮子沟-英东构造带构造演化及控藏特征[J].地学前缘,2014,21(1):261-270.
SUI Liwei,FANG Shihu,SUN Yonghe,et al.The tectonic evolution and accumulation controlling characteristics of Shizigou-Yingdong structural belt of western Qaidam Basin[J].Earth Science Frontiers,2014,21(1):261-270.
[30] 高树生,胡志明,刘华勋,等.不同岩性储层的微观孔隙特征[J].石油学报,2016,37(2):248-256.
GAO Shusheng,HU Zhiming,LIU Huaxun,et al.Microscopic pore characteristics of different lithological reservoirs[J].Acta Petrolei Sinica,2016,37(2):248-256.
[31] 杨凯峰.英东地区油砂山组储层成岩作用研究[D].西安:西北大学,2016.
YANG Kaifeng.Research on diagenesis of the Youshashan formation in Yingdong Areas,Qaidam Basin[D].Xi'an:Northwest University,2016.
[32] 黄叶秋.英东地区沉积储层特征及主控因素分析[D].青岛:中国石油大学,2015.
HUANG Yeqiu.Sedimentary reservoir characteristics and main control factors analysis in Ying Dong Area[D].Qingdao:China University of Petroleum(East China),2015.
[33] SIBSON R H.Fault rocks and fault mechanisms[J].Journal of the Geological Society,1977,133(3):191-213.
[34] PITTMAN E D.Effect of fault-related granulation on porosity and permeability of quartz sandstones,Simpson Group(Ordovician),Oklahoma[J].AAPG Bulletin,1981,65(11):2381-2387.
[35] KNIPE R J.Faulting processes and fault seal[M]//LARSEN R M,BREKKE H,LARSEN B T,et al.Structural and Tectonic Modelling and Its Application to Petroleum Geology.Stavanger,Norway:Elsevier,1992:325-342.
[36] CHEMENDA A I,BALLAS G,SOLIVA R.Impact of a multilayer structure on initiation and evolution of strain localization in porous rocks:field observations and numerical modeling[J].Tectonophysics,2014,631:29-36.
[37] CASHMAN S,CASHMAN K.Cataclasis and deformation-band formation in unconsolidated marine terrace sand,Humboldt County,California[J].Geology,2000,28(2):111-114.
[38] BALLAS G,FOSSEN H,SOLIVA R.Factors controlling permeability of cataclastic deformation bands and faults in porous sandstone reservoirs[J].Journal of Structural Geology,2015,76:1-21.
[39] ANTONELLINI M A,AYDIN A,POLLARD D D.Microstructure of deformation bands in porous sandstones at Arches National Park,Utah[J].Journal of Structural Geology,1994,16(7):941-959.
[40] FOSSEN H,BALE A.Deformation bands and their influence on fluid flow[J].AAPG Bulletin,2007,91(12):1685-1700.
[41] ROTEVATN A,FOSSMARK H S,BASTESEN E,et al.Do deformation bands matter for flow? Insights from permeability measurements and flow simulations in porous carbonate rocks[J].Petroleum Geoscience,2017,23(1):104-119.
[42] 刘志达.高孔隙性岩石中变形带成因机制及对流体流动的影响[D].大庆:东北石油大学,2017.
LIU Zhida.The Mechanisms and the influence on fluid flow of deformation bands[D].Daqing:Northeast Petroleum University,2017.
[43] FOSSEN H,ZULUAGA L F,BALLAS G,et al.Contractional deformation of porous sandstone:insights from the Aztec Sandstone,SE Nevada,USA[J].Journal of Structural Geology,2015,74:172-184.
[44] FOSSEN H,SOLIVA R,BALLAS G,et al.A review of deformation bands in reservoir sandstones:geometries,mechanisms and distribution[J].Geological Society,London,Special Publications,2017,459:25.
[45] FOSSEN H,SCHULTZ R A,TORABI A.Conditions and implications for compaction band formation in the Navajo Sandstone,Utah[J].Journal of Structural Geology,2011,33(10):1477-1490.
[46] 贾茹,付晓飞,孟令东,等.断裂及其伴生微构造对不同类型储层的改造机理[J].石油学报,2017,38(3):286-296.
JIA Ru,FU Xiaofei,MENG Lingdong,et al.Transformation mechanism of fault and its associated microstructures for different kinds of reservoirs[J].Acta Petrolei Sinica,2017,38(3):286-296.

高孔隙性砂岩内变形带特征及对流体流动的影响——以柴达木盆地西缘油砂山背斜为例

Characteristics of deformation bands in high-porosity sandstone and their influence on fluid flow: a case study of Youshashan anticline at the western margin of Q aidam Basin

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	张世铭, 王建功, 张永庶, 张小军, 张婷静, 崔俊. 柴达木盆地西部地区下干柴沟组湖相白云岩晶间孔型储层物性下限的确定[J]. 石油学报, 2021, 42(1): 45-55,118.
[2]	何媛媛, 张斌, 桂丽黎, 张国卿, 袁莉. 从原油地球化学特征看致密油聚集机制——以柴达木盆地西部扎哈泉油藏为例[J]. 石油学报, 2020, 41(9): 1060-1072.
[3]	王建功, 张永庶, 李翔, 徐丽, 石亚军, 黄叶秋, 王玉林, 管斌, 张世铭, 高妍芳. 柴达木盆地西部渐新统纹理石沉积特征与原位成藏[J]. 石油学报, 2020, 41(8): 940-959.
[4]	田继先, 李剑, 曾旭, 孔骅, 沙威, 郭泽清, 张静, 付艳双. 柴达木盆地东坪地区原油裂解气的发现及成藏模式[J]. 石油学报, 2020, 41(2): 154-162,255.
[5]	黄成刚, 张小军, 胡贵, 刘应如, 张希文, 张国辉, 李红哲, 吴梁宇. 高原咸化湖盆基底储层特征与成藏主控因素——以柴达木盆地东坪地区为例[J]. 石油学报, 2020, 41(2): 179-196.
[6]	卞青, 陈琰, 张国卿, 刘润超, 王振东, 郭召杰. 柴达木盆地膏盐层岩石物理特征及其对构造变形的影响[J]. 石油学报, 2020, 41(2): 197-204.
[7]	刘池洋, 付锁堂, 张道伟, 陈琰, 黄雷, 石亚军. 柴达木盆地巨型油气富集区的确定及勘探成效——改造型盆地原盆控源、改造控藏之范例[J]. 石油学报, 2020, 41(12): 1527-1537.
[8]	宫清顺, 刘占国, 宋光永, 夏志远, 柳金城, 管斌, 范卫光. 柴达木盆地昆北油田冲积扇厚层砂砾岩储集层内部隔夹层[J]. 石油学报, 2019, 40(2): 152-164.
[9]	马达德, 陈琰, 夏晓敏, 魏学斌, 吴颜雄, 袁莉, 何柳. 英东油田成藏条件及勘探开发关键技术[J]. 石油学报, 2019, 40(1): 115-130.
[10]	曹正林, 孙秀建, 吴武军, 田光荣, 张世铭, 李海滨, 孙知明, 徐丽, 王瑞菊. 柴达木盆地盆缘冲断古隆起的形成演化及对油气成藏的影响[J]. 石油学报, 2018, 39(9): 980-989.
[11]	张斌, 何媛媛, 陈琰, 孟庆洋, 黄家旋, 袁莉. 柴达木盆地西部咸化湖相优质烃源岩形成机理[J]. 石油学报, 2018, 39(6): 674-685.
[12]	贾茹, 付晓飞, 孟令东, 巩磊, 刘志达. 断裂及其伴生微构造对不同类型储层的改造机理[J]. 石油学报, 2017, 38(3): 286-296.
[13]	黄成刚, 常海燕, 崔俊, 李亚锋, 路艳平, 李翔, 马新民, 吴梁宇. 柴达木盆地西部地区渐新世沉积特征与油气成藏模式[J]. 石油学报, 2017, 38(11): 1230-1243.
[14]	张敏, 欧光习, 张枝焕, 黎琼, 宫晓峰. 柴达木盆地东部石炭系页岩气储层流体地球化学特征[J]. 石油学报, 2017, 38(11): 1244-1252.
[15]	付锁堂, 马达德, 陈琰, 张国卿, 伍坤宇. 柴达木盆地油气勘探新进展[J]. 石油学报, 2016, 37(S1): 1-10.