鄂尔多斯盆地西南部延长组长8油层组层序地层特征及沉积充填模式

doi:10.7623/syxb201904005

石油学报 ›› 2019, Vol. 40 ›› Issue (4): 434-447.DOI: 10.7623/syxb201904005

鄂尔多斯盆地西南部延长组长8油层组层序地层特征及沉积充填模式

陈林^1,2, 陆永潮², 林卫兵³, 邢凤存⁴, 陈平³, 刘璐⁵, 胡海燕⁶, 魏巍²

1. 中国地质调查局武汉地质调查中心湖北武汉 430205;
2. 中国地质大学(武汉)资源学院湖北武汉 430074;
3. 中国地质大学(武汉)海洋学院湖北武汉 430074;
4. 成都理工大学沉积地质研究院四川成都 610059;
5. 中国石油化工股份有限公司华北分公司勘探开发研究院河南郑州 450006;
6. 长江大学地球科学学院湖北武汉 430100

收稿日期:2018-05-15 修回日期:2019-03-15 出版日期:2019-04-25 发布日期:2019-05-07
通讯作者: 林卫兵,男,1963年2月生,1986年获武汉地质学院地质学专业学士学位,现为中国地质大学(武汉)海洋学院副教授,主要从事储层沉积学层序地层学教学及相关科研工作。Email:475519803@qq.com
作者简介:陈林,男,1989年9月生,2010年获中国矿业大学地质工程专业学士学位,2015年获中国地质大学(武汉)能源地质工程专业博士学位,现为中国地质调查局武汉地质调查中心工程师,主要从事非常规油气储层沉积相及层序地层学研究。Email:chenlin676@163.com
基金资助:
国家自然科学基金项目（No.41002045）、国家科技重大专项（2016ZX05034-001-002）和中国地质调查局地质调查项目（DD20160194）资助。

Sequence stratigraphy and sedimentary filling model of Chang-8 oil layer of Yanchang Formation in southwestern Ordos Basin

Chen Lin^1,2, Lu Yongchao², Lin Weibing³, Xing Fengcun⁴, Chen Ping³, Liu Lu⁵, Hu Haiyan⁶, Wei Wei²

1. Wuhan Center, China Geological Survey, Hubei Wuhan 430205, China;
2. Faculty of Earth Resources, China University of Geosciences, Hubei Wuhan 430074, China;
3. College of Marine Science and Technology, China University of Geosciences, Hubei Wuhan 430074, China;
4. Institute of Sedimentary Geology, Chengdu University of Technology, Sichuan Chengdu 610059, China;
5. Petroleum Exploration and Development Research Institute, Sinopec North China E & P Company, Henan Zhengzhou 450006, China;
6. School of Geosciences, Yangtze University, Hubei Wuhan 430100, China

Received:2018-05-15 Revised:2019-03-15 Online:2019-04-25 Published:2019-05-07

摘要/Abstract

摘要：

综合鄂尔多斯盆地西南部延长组长8油层组的野外露头、岩心、测井、地震以及分析测试资料，研究了长8油层组的层序地层格架、沉积特征、沉积充填的空间展布及层序控制下的沉积演化模式。结果表明，长8油层组主要发育在长7油层组—长8油层组层序的低位体系域，进一步可划分为6个准层序组，15个准层序。层序地层对比表明，长8油层组在空间上分布稳定，无明显厚度变化，地形起伏较小，发育湖盆边缘缓坡层序构成样式。沉积砂体的成分成熟度和结构成熟度较低，粒度结构具有二段性，为快速堆积产物并发育波浪改造的沉积构造，具有牵引流色彩的密度流沉积特征，沉积中可见浅水虫孔、植物根迹等，总体指示浅水三角洲环境。沉积物具有受季节性气候变化控制的多期洪泛密度流沉积特征。沉积充填的垂向、剖面和平面展布特征显示，在坡缓、浅水和快速堆积的环境下，三角洲前缘区水道在前缘区频繁分叉改道，从而形成网结化前缘分布样式。其中，在长8油层组沉积早期为三角洲主建设进积时期，水道限定性强，河道砂坝广泛垂向叠置；在长8油层组沉积晚期，在湖平面上升的背景下，物源供给能力减弱，研究区内三角洲河流建设作用弱化，水下分流河道、河口坝受较强地改造，沉积物粒度变细，砂体的横向片状展布性增强，以加积作用、进积作用为主。整体上，长8油层组记录了一套完整的水退到水进的陆相湖盆低位充填序列。

关键词: 鄂尔多斯盆地, 延长组, 长8油层组, 层序地层, 沉积充填模式

Abstract:

Comprehensively based on the analysis of outcrop, core, logging, seismic and test data of Chang-8 oil layer of Yanchang Formation in southwestern Ordos Basin, the sequence stratigraphic framework, sedimentary characteristics, spatial distribution of sedimentary filling and the sedimentary evolution model controlled by the sequence of Chang-8 oil layer are investigated. The results show that in Chang-8 oil layer, the lowstand system tract sediments of the Chang-7-Chang-8 sequence is mainly developed, which can be further divided into 6 parasequence sets and 15 parasequences. Sequence stratigraphic correlation shows that the spatial distribution of the stratum is stable, no obvious thickness change and less topographic relief. A sequence structure pattern of gentle slope is thus developed on the margin of lacustrine basin. The sedimentary sand body is characterized by low composition maturity and structure maturity, two segments of grain structure, well-developed sedimentary structures formed by rapid deposition and wave transformations, and density flow deposition with traction flow feature. In addition, it can be visibly seen that shallow water wormholes and plant roots are developed, indicating a shallow water delta environment. Sediments have multi-phase flood density flow sedimentation characteristics controlled by seasonal climate change. The vertical, sectional and planar distribution characteristics of sedimentary fillings reveal that the channels of delta front diverge frequently in the front zone, thus forming the networking distribution pattern under the background of gentle slope, shallow water and rapid deposition. Progradation of delta mainly occurred during the early period of Chang-8 oil layer deposition. The supply of provenance was reducing, so the construction ability of delta was weakened under the background of lake level rising. The channels were highly restrictive, thus the extensive vertical superposition was widely developed at sand body bar. During the late period of Chang-8 oil layer deposition, the subaqueous distributary channels and mouth bars were subject to relatively strong reforming. The grain size of the sediments became finer and the lateral distribution of sand bodies was strengthened. The lateral sheet-spreading distribution of sand bodies is enhanced, dominated by aggradation and progradation. On the whole, the Chang-8 oil layer recorded a complete cycle of lowstand filling sequence of continental lacustrine basin from regression to transgression.

Key words: Ordos Basin, Yanchang Formation, Chang-8 oil layer, sequence stratigraphy, sedimentary filling model

中图分类号:

TE121.3

陈林, 陆永潮, 林卫兵, 邢凤存, 陈平, 刘璐, 胡海燕, 魏巍. 鄂尔多斯盆地西南部延长组长8油层组层序地层特征及沉积充填模式[J]. 石油学报, 2019, 40(4): 434-447.

Chen Lin, Lu Yongchao, Lin Weibing, Xing Fengcun, Chen Ping, Liu Lu, Hu Haiyan, Wei Wei. Sequence stratigraphy and sedimentary filling model of Chang-8 oil layer of Yanchang Formation in southwestern Ordos Basin[J]. Acta Petrolei Sinica, 2019, 40(4): 434-447.

参考文献

[1] SHANLEY K W,CLUFF R M,ROBINSON J W. Factors controlling prolific gas production from low-permeability sandstone reservoirs:implications for resource assessment,prospect development,and risk analysis[J].AAPG Bulletin, 2004,88(8):1083-1121.
[2] 张金川,金之钧,袁明生.页岩气成藏机理和分布[J].天然气工业,2004,24(7):15-18.
ZHANG Jinchuan,JIN Zhijun,YUAN Mingsheng.Reservoiring mechanism of shale gas and its distribution[J].Natural Gas Industry,2004,24(7):15-18.
[3] JARVIE D M,HILL R J,RUBLE T E,et al.Unconventional shale-gas systems:the Mississippian Barnett shale of north-central Texas as one model for thermogenic shale-gas assessment[J].AAPG Bulletin,2007,91(4):475-499.
[4] JIA Chengzao,ZHENG Min,ZHANG Yongfeng.Unconventional hydrocarbon resources in China and the prospect of exploration and development[J].Petroleum Exploration and Development,2012,39(2):139-146.
[5] 黄东,段勇,杨光,等.淡水湖相沉积区源储配置模式对致密油富集的控制作用——以四川盆地侏罗系大安寨段为例[J].石油学报,2018,39(5):518-527.
HUANG Dong,DUAN Yong,YANG Guang,et al.Controlling effect of source-reservoir configuration model on tight oil enrichment in freshwater lacustrine sedimentary area:a case study of the Jurassic Da'anzhai Member in Sichuan Basin[J].Acta Petrolei Sinica,2018,39(5):518-527.
[6] YAO Jingli,DENG Xiuqin,ZHAO Yande,et al.Characteristics of tight oil in Triassic Yanchang Formation,Ordos Basin[J].Petroleum Exploration and Development,2013,40(2):161-169.
[7] SHI Lizhi,WANG Zhuozhuo,ZHANG Ge,et al.Distribution and formation of tight oil in Qijia area,Songliao Basin,NE China[J].Petroleum Exploration and Development,2015,42(1):48-55.
[8] 吴晓智,赵玉梅,王社教,等.准噶尔盆地侏罗系煤系地层致密砂岩气资源潜力分析[J]. 天然气地球科学,2016,27(9):1679-1687.
WU Xiaozhi,ZHAO Yumei,WANG Shejiao,et al.Analysis on the resource potential of tight sandstonegas of Jurassic coal measure in Junggar Basin,China[J].Natural Gas Geoscience,2016,27(9):1679-1687.
[9] 李剑,姜晓华,王秀芹,等.裂谷盆地致密砂岩气成藏机制与富集规律——以松辽盆地与渤海湾盆地为例[J].石油与天然气地质,2017,38(6):1005-1018.
LI Jian,JIANG Xiaohua,WANG Xiuqin,et al.Mechanisms for gas accumulation and enrichment in tight sandstone reservoir in rift Basins:cases from the Songliao Basin and the Bohai Bay[J].Oil & Gas Geology,2017,38(6):1005-1018.
[10] 曾翔,蔡进功,董哲,等.泥页岩沉积特征与生烃能力——以东营凹陷沙河街组三段中亚段—沙河街组四段上亚段为例[J].石油学报,2017,38(1):31-43.
ZENG Xiang,CAI Jingong,DONG Zhe,et al.Sedimentary characteristics and hydrocarbon generation potential of mudstone and shale:a case study of middle submember of Member 3 and upper submember of Member 4 in Shahejie Formation in Dongying sag[J].Acta Petrolei Sinica,2017,38(1):31-43.
[11] 丁晓琪,张哨楠,熊迪,等.鄂尔多斯盆地西南缘延长组湖盆底形演化研究[J].西南石油大学学报:自然科学版,2011,33(6):1-6.
DING Xiaoqi,ZHANG Shaonan,XIONG Di,et al.Evolution of basin bottom morphology of Yanchang Formation,upper Triassic,southwestern Ordos Basin[J].Journal of Southwest Petroleum University:Science & Technology Edition,2011,33(6):1-6.
[12] 张哨楠,丁晓琪.鄂尔多斯盆地南部延长组致密砂岩储层特征及其成因[J].成都理工大学学报:自然科学版,2010,37(4):386-394.
ZHANG Shaonan,DING Xiaoqi.Characters and causes of tight sandstones of Yanchang Formation in southern Ordos Basin,China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2010,37(4):386-394.
[13] 郭秋麟,武娜,陈宁生,等.鄂尔多斯盆地延长组第7油层组致密油资源评价[J].石油学报,2017,38(6):658-665.
GUO Qiulin,WU Na,CHEN Ningsheng,et al.An assessment of tight oil resource in 7th oil reservoirs of Yanchang Formation,Ordos Basin[J].Acta Petrolei Sinica,2017,38(6):658-665.
[14] 罗晓容,王忠楠,雷裕红,等.特超低渗砂岩油藏储层非均质性特征与成藏模式——以鄂尔多斯盆地西部延长组下组合为例[J].石油学报,2016,37(S1):87-98.
LUO Xiaorong,WANG Zhongnan,LEI Yuhong,et al.Heterogeneity characteristics and accumulation model of ultra-low permeability sandstone reservoirs:a case study of the lower part of Yanchang Formation in the Western Ordos Basin,China[J].Acta Petrolei Sinica,2016,37(S1):87-98.
[15] 吴浩,张春林,纪友亮,等.致密砂岩孔喉大小表征及对储层物性的控制——以鄂尔多斯盆地陇东地区延长组为例[J].石油学报,2017,38(8):876-887.
WU Hao,ZHANG Chunlin,JI Youliang,et al.Pore-throat size characterization of tight sandstone and its control on reservoir physical properties:a case study of Yanchang Formation,eastern Gansu,Ordos Basin[J].Acta Petrolei Sinica,2017,38(8):876-887.
[16] 杨友运,张蓬勃,张忠义.鄂尔多斯盆地西峰油田长8油组辫状河三角洲沉积特征与层序演化[J].地质科技情报,2005,24(1):45-48.
YANG Youyun,ZHANG Pengbo,ZHANG Zhongyi.Sedimentary features and sequence evolution of braided river delta of Chang 8 oil formation of Xifeng oil field in Ordos Basin[J].Geological Science and Technology Information,2005,24(1):45-48.
[17] 刘化清,李相博,完颜容,等.鄂尔多斯盆地长8油层组古地理环境与沉积特征[J].沉积学报,2011,29(6):1086-1097.
LIU Huaqing,LI Xiangbo,WAN Yanrong,et al.Palaeogeographic and sedimentological characteristics of the Triassic Chang 8,Ordos Basin,China[J].Acta Sedimentologica Sinica,2011,29(6):1086-1097.
[18] 刁帆,文志刚,邹华耀,等.鄂尔多斯盆地陇东地区长8油层组浅水三角洲沉积特征[J].地球科学:中国地质大学学报,2013,38(6):1289-1298.
DIAO Fan,WEN Zhigang,ZOU Huayao,et al.Sedimentary characteristics of shallow-water deltas in Chang 8 oil-bearing interval in eastern Gansu,Ordos Basin[J].Earth Science:Journal of China University of Geosciences,2013,38(6):1289-1298.
[19] 李士祥,楚美娟,黄锦绣,等.鄂尔多斯盆地延长组长8油层组砂体结构特征及成因机理[J].石油学报,2013,34(3):435-444.
LI Shixiang,CHU Meijuan,HUANG Jinxiu,et al.Characteristics and genetic mechanism of sandbody architecture in Chang-8 oil layer of Yanchang Formation,Ordos Basin[J].Acta Petrolei Sinica,2013,34(3):435-444.
[20] 齐亚林,邓秀芹,楚美娟,等.鄂尔多斯盆地晚三叠世长8期沉积环境分析[J].地质科技情报,2014,33(4):170-176.
QI Yalin,DENG Xiuqin,CHU Meijuan,et al.Analysis of depositional environment of Chang 8 of Upper Triassic,Ordos Basin[J].Geological Science and Technology Information,2014,33(4):170-176.
[21] 江琦,丁晓琪,刘曦翔,等.鄂尔多斯盆地南部长8段砂质碎屑流储层特征及主控因素 [J].东北石油大学学报,2015,39(6):56-65.
JIANG Qi,DING Xiaoqi,LIU Xixiang,et al.Reservoir characteristics and control factors of sandy debris flow from Chang 8 interval,south of Ordos Basin[J].Journal of Northeast Petroleum University,2015,39(6):56-65.
[22] LIU Shaofeng.The coupling mechanism of Basin and orogen in the western Ordos Basin and adjacent regions of China[J].Journal of Asian Earth Sciences,1998,16(4):369-383.
[23] 李树同,王多云,王彬,等.坳陷型湖盆缓坡边缘沉积坡折带的识别——以鄂尔多斯盆地三叠纪延长期沉积坡折带为例[J].天然气地球科学,2008,19(1):83-88.
LI Shutong,WANG Duoyun,WANG Bin,et al.Identification of sedimentary slope breaks in the margin of a down warped lake basin's ramp belt:a case from Triassic Yanchang Formation,Ordos Basin[J].Natural Gas Geoscience,2008,19(1):83-88.
[24] ZOU Caineng,WANG Lan,LI Ying,et al.Deep-lacustrine transformation of sandy debrites into turbidites,Upper Triassic,central China[J].Sedimentary Geology,2012,265-266:143-155.
[25] 李斌,孟自芳,宋岩,等.鄂尔多斯盆地西缘前陆盆地构造-沉积响应[J].吉林大学学报:地球科学版,2007,37(4):703-709.
LI Bin,MENG Zifang,SONG Yan,et al.Tectonic-sedimentary response of foreland basin in western margin of Ordos Basin[J].Journal of Jilin University:Earth Science Edition,2007,37(4):703-709.
[26] 王峰,田景春,范立勇,等.鄂尔多斯盆地三叠系延长组沉积充填演化及其对印支构造运动的响应[J].天然气地球科学,2010,21(6):882-889.
WANG Feng,TIAN Jingchun,FAN Liyong,et al.Evolution of sedimentary fillings in Triassic Yanchang Formation and its response to Indosinian movement in Ordos Basin[J].Natural Gas Geoscience,2010,21(6):882-889.
[27] 罗静兰,KETZER J M,李文厚,等.延长油区侏罗系上三叠统层序地层与生储盖组合[J].石油与天然气地质,2001,22(4):337-341,351.
LUO Jinglan,KETZER M J,LI Wenhou,et al.Sequence stratigraphy and source-reservoir-cap assemblages of Jurassic-Upper Triassic in Yanchang oil province[J].Oil & Gas Geology,2001,22(4):337-341,351.
[28] 李凤杰,王多云.鄂尔多斯盆地西峰油田延长组高分辨率层序地层学研究[J].天然气地球科学,2006,17(3):339-344.
LI Fengjie,WANG Duoyun.The high-resolution sequence stratigraphic feature of Yanchang Formation in Xifeng oilfield,Ordos Basin[J].Natural Gas Geoscience,2006,17(3):339-344.
[29] 刘世昊,丰爱平,夏东兴,等.辽东湾西岸典型岬湾海滩表层沉积物粒度分布特征及水动力条件浅析[J].沉积学报,2014,32(4):700-709.
LIU Shihao,FENG Aiping,XIA Dongxing,et al.Grain-size distribution of surface sediments of two typical headland bay beaches on western Liaodong Bay,Bohai Sea and simply analysis of hydrodynamic conditions[J].Acta Sedimentologica Sinica,2014,32(4):700-709.
[30] SAHU B K.Depositional mechanisms from the size analysis of clastic sediments[J].Journal of Sedimentary Petrology,1964,34(1):73-83.
[31] 李明诚,李剑,万玉金,等.沉积盆地中的流体[J].石油学报,2001,22(4):13-17.
LI Mingcheng,LI Jian,WAN Yujin,et al.Fluids in the sedimentary basin[J].Acta Petrolei Sinica,2001,22(4):13-17.
[32] 赵方臣,朱茂炎,胡世学.不同生活方式的物种对快速沉积埋藏事件的反应——来自寒武纪早期澄江生物群中的证据[J].古生物学报,2012,51(3):265-280.
ZHAO Fangchen,ZHU Maoyan,HU Shixue.Diverse responses of Cambrian organisms to sedimentary events:evidence from the Chengjiang Lagerstatte of eastern Yunnan[J].Acta Palaeontologica Sinica,2012,51(3):265-280.
[33] 罗静兰,史成恩,李博,等.鄂尔多斯盆地周缘及西峰地区延长组长8、长6沉积物源——来自岩石地球化学的证据[J].中国科学:地球科学,2007(S1):62-72.
LUO Jinglan,SHI Cheng’en,LI Bo,et al.Provenance for the Chang 6 and Chang 8 Member of the Yanchang Formation in the Xifeng area and in the periphery Ordos Basin:evidence from petrologic geochemistry[J].Science in China Series D:Earth Sciences,2007,50(S2):75-90.
[34] 杨明慧,刘池洋,郑孟林,等.鄂尔多斯盆地中晚三叠世两种不同类型边缘层序构成及对构造活动响应[J].中国科学 D辑:地球科学,2007,37(S1):173-184.
YANG Minghui,LIU Chiyang,ZHENG Menglin,et al.Sequence framework of two different kinds of margins and their response to tectonic activity during the Middle-Late Triassic,Ordos Basin[J].Science in China Series D:Earth Sciences,2007,50(S2):203-216.
[35] 张天舒,吴因业,郭彬程,等.鄂尔多斯盆地西南缘晚三叠世前陆冲断活动控制的沉积层序特征[J].地学前缘,2012,19(1):40-50.
ZHANG Tianshu,WU Yinye,GUO Bincheng,et al.The characteristics of late Triassic depositional sequence controlled by foreland thrust-faulting in south-western Ordos Basin[J].Earth Science Frontiers,2012,19(1):40-50.

鄂尔多斯盆地西南部延长组长8油层组层序地层特征及沉积充填模式

Sequence stratigraphy and sedimentary filling model of Chang-8 oil layer of Yanchang Formation in southwestern Ordos 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]	付锁堂, 金之钧, 付金华, 李士祥, 杨伟伟. 鄂尔多斯盆地延长组7段从致密油到页岩油认识的转变及勘探开发意义[J]. 石油学报, 2021, 42(5): 561-569.
[2]	张家强, 李士祥, 李宏伟, 周新平, 刘江艳, 郭睿良, 陈俊霖, 李树同. 鄂尔多斯盆地延长组7油层组湖盆远端重力流沉积与深水油气勘探——以城页水平井区长7₃小层为例[J]. 石油学报, 2021, 42(5): 570-587.
[3]	付锁堂, 付金华, 牛小兵, 李士祥, 吴志宇, 周新平, 刘江艳. 庆城油田成藏条件及勘探开发关键技术[J]. 石油学报, 2020, 41(7): 777-795.
[4]	赵靖舟, 孟选刚, 韩载华. 近源成藏——来自鄂尔多斯盆地延长组湖盆东部“边缘”延长组6段原油的地球化学证据[J]. 石油学报, 2020, 41(12): 1513-1526.
[5]	李向东, 陈海燕. 深水环境下古水流方向分析和阻塞浊流沉积的识别——以鄂尔多斯盆地桌子山地区上奥陶统拉什仲组为例[J]. 石油学报, 2020, 41(11): 1348-1365.
[6]	张磊, 乔向阳, 张亮, 吴克柳, 周伟, 白慧芳, 辛翠平, 王涛. 鄂尔多斯盆地旬邑探区延长组储层特征和开发效果[J]. 石油学报, 2020, 41(1): 88-95.
[7]	徐旺林, 胡素云, 李宁熙, 魏新善, 高建荣, 赵振宇, 李相博, 刘俊榜, 张月巧, 宋微. 鄂尔多斯盆地奥陶系中组合内幕气源特征及勘探方向[J]. 石油学报, 2019, 40(8): 900-913.
[8]	张译丹, 姜在兴, 杜克峰, 张建国, 年涛, 周学文, 罗丹婷, 王力. 鄂尔多斯盆地志丹—富县地区三叠系延长组长8油层组风暴沉积特征及意义[J]. 石油学报, 2019, 40(7): 813-822.
[9]	谭聪, 阮壮, 于炳松, 刘策, 苏玲. 鄂尔多斯盆地西缘中—晚三叠世构造-物源-古地貌体系演化——来自碎屑锆石、地球化学和岩石学的证据[J]. 石油学报, 2019, 40(6): 660-676.
[10]	樊建明, 王冲, 屈雪峰, 成良丙, 薛婷. 鄂尔多斯盆地致密油水平井注水吞吐开发实践——以延长组长7油层组为例[J]. 石油学报, 2019, 40(6): 706-715.
[11]	黄兴, 李天太, 王香增, 高辉, 倪军, 赵金省, 王琛. 致密砂岩储层可动流体分布特征及影响因素——以鄂尔多斯盆地姬塬油田延长组长8油层组为例[J]. 石油学报, 2019, 40(5): 557-567.
[12]	康永尚, 皇甫玉慧, 张兵, 邓泽, 毛得雷, 何志平, 王建, 袁春林. 含煤盆地深层“超饱和”煤层气形成条件[J]. 石油学报, 2019, 40(12): 1426-1438.
[13]	谢环羽, 赵靖舟, 王培玺, 谢武仁, 杨雨. 中—上扬子地区奥陶系层序地层格架[J]. 石油学报, 2019, 40(10): 1202-1222.
[14]	李易隆, 贾爱林, 冀光, 郭建林, 王国亭, 郭智, 张吉. 鄂尔多斯盆地中-东部下石盒子组八段辫状河储层构型[J]. 石油学报, 2018, 39(9): 1037-1050.
[15]	魏新善, 傅强, 淡卫东, 赵世杰, 庞锦莲, 楚美娟. 鄂尔多斯盆地延长组成岩流体滞留效应与致密砂岩储层成因[J]. 石油学报, 2018, 39(8): 858-868.