四川盆地及邻区上奥陶统五峰组-下志留统龙马溪组底部笔石带及沉积特征

doi:10.7623/syxb201702004

石油学报 ›› 2017, Vol. 38 ›› Issue (2): 160-174.DOI: 10.7623/syxb201702004

四川盆地及邻区上奥陶统五峰组-下志留统龙马溪组底部笔石带及沉积特征

聂海宽^1,2,3, 金之钧^1,2,3, 马鑫⁴, 刘忠宝^1,2,3, 林拓⁵, 杨振恒^1,2,3

1. 页岩油气富集机理与有效开发国家重点实验室北京 100083;
2. 中国石油化工股份有限公司石油勘探开发研究院北京 100083;
3. 中国石油化工集团公司页岩油气勘探开发重点实验室北京 100083;
4. 中国地质大学能源学院北京 100083;
5. 中国地质调查局油气资源调查中心北京 100083

收稿日期:2016-09-28 修回日期:2016-11-25 出版日期:2017-02-25 发布日期:2017-03-08
通讯作者: 聂海宽,男,1982年4月生,2005年获中国地质大学(北京)学士学位,2010年获中国地质大学(北京)博士学位,现为中国石油化工股份有限公司石油勘探开发研究院研究员,主要从事非常规油气地质研究工作。Email:niehk.syky@sinopec.com
作者简介:聂海宽,男,1982年4月生,2005年获中国地质大学(北京)学士学位,2010年获中国地质大学(北京)博士学位,现为中国石油化工股份有限公司石油勘探开发研究院研究员,主要从事非常规油气地质研究工作。Email:niehk.syky@sinopec.com
基金资助:
国家重大科技专项（2016ZX05061-001）和国家自然科学基金项目（No.41202103）资助。

Graptolites zone and sedimentary characteristics of Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation in Sichuan Basin and its adjacent areas

Nie Haikuan^1,2,3, Jin Zhijun^1,2,3, Ma Xin⁴, Liu Zhongbao^1,2,3, Lin Tuo⁵, Yang Zhenheng^1,2,3

1. State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Beijing 100083, China;
2. Sinopec Petroleum Exploration and Production Research Institute, Beijing 100083, China;
3. Sinopec Key Laboratory of Shale Oil/Gas Exploration & Production, Beijing 100083, China;
4. School of Energy Resource, China University of Geosciences, Beijing 100083, China;
5. Oil & Gas Survey Center, China Geological Survey, Beijing 100029, China

Received:2016-09-28 Revised:2016-11-25 Online:2017-02-25 Published:2017-03-08

摘要/Abstract

摘要：

根据四川盆地五峰组-龙马溪组主要页岩气井和典型剖面的资料，分析了不同笔石带页岩的沉积环境、厚度等特征，明确了五峰组下部WF2-WF3笔石页岩段（奥陶纪凯迪阶晚期447.62~445.16 Ma）、五峰组观音桥层WF4灰岩/泥质灰岩/灰质泥页岩段（奥陶纪赫南特阶早期445.16~444.43 Ma）和龙马溪组底部LM1-LM4笔石页岩段（奥陶纪赫南特阶晚期444.43~443.83 Ma和志留纪鲁丹阶早中期443.83~441.57 Ma）3个层段的沉积环境、岩性和厚度特征，分析了页岩平面展布特征。研究表明：①五峰组下部WF2-WF3笔石页岩段沉积期，研究区主体上受广西运动的影响较小，沉积环境为广海深水环境，主要沉积了黑色页岩，沉积中心发育在黔东北-川东北和川南2个区域，沉积中心最大厚度为4~6 m。②五峰组观音桥层WF4笔石页岩段沉积期，受全球海平面下降和广西运动增强的影响，研究区沉积环境发生重大变化，川中古隆起、黔中古隆起和江南-雪峰古隆起进一步扩大，沉积盆地面积减小，沉积环境变为以浅海碳酸盐生屑滩沉积为主，少量深水沉积环境为辅（仅分布在川东-川东北地区的石柱-涪陵-巫溪一带和川南地区的长宁-永川一带），浅水沉积物以富含赫南特贝的灰岩、泥质灰岩等沉积为主，深水沉积物主体为含赫南特贝的灰质泥岩、页岩沉积。③龙马溪组底部LM1-LM4笔石页岩段沉积期，受全球海平面上升和广西运动的控制沉积范围比观音桥层沉积期大，主体为滞留的深水沉积环境，沉积了厚度较大的LM1-LM4笔石页岩段黑色页岩，最大厚度超过20 m。进一步分析了川中古隆起、黔中古隆起及江南雪峰古隆起对黑色页岩的控制作用，探讨了自流井水下高地/隆起、华蓥山水下高地、丁山水下高地和湘鄂西水下高地/隆起对黑色页岩沉积与保存的控制作用。

关键词: 页岩气, 笔石带, 五峰组, 龙马溪组, 四川盆地及邻区

Abstract:

According to the data of main shale gas wells and the type sections of Wufeng Formation-Longmaxi Formation in Sichuan Basin, this study analyzes the sedimentary environment, thickness and other characteristics of shale in various graptolite zones. determines the sedimentary environment, lithology and thickness characteristics of the graptolite shale interval WF2-WF3 in the lower part of Wufeng Formation (Late Ordovician Katian, 447.62-445.16 Ma), Guanyinqiao Member WF4 limestone/argillaceous limestone/calcareous shale interval in Wufeng Formation (Early Ordovician Hirnantian, 445.16-444.43 Ma) and the graptolite shale interval LM1-LM4 in the bottom of Longmaxi Formation (Late Ordovician Hirnantian, 444.43-443.83 Ma and Early-Middle Silurian Rhuddanian, 443.83-441.57 Ma), and also explores the plane distribution characteristics of shale. The study results shows:(1) During the deposition period of WF2-WF3 in the lower part of Wufeng Formation, the main study area was less affected by Guangxi movement. The sedimentary environment was characterized by open-sea deep water, where black shale was mainly deposited. The thickness center was developed in Northeast Guizhou-Northeast Sichuan and South Sichuan. The maximum center thickness is 4-6 m. (2) During the deposition period of WF4 in Guanyinqiao Member, Wufeng Formation, the sedimentary environment in the study area had significant changes as influenced by global sea level fall and enhanced Guangxi movement; palaeouplifts in central Sichuan and central Guizhou and Jiangnan-Xuefeng palaeouplift further expanded, and the area of the sedimentary basin decreased; the sedimentary environment changed to be dominated by neritic carbonate clastic shoal and shallow water sedimentary environment, with supplement of deepwater sedimentary environment (only distributed in Shizhu-Fuling-Wuxi area in East Sichuan-Northeast Sichuan and Changning-Yongchuan area in South Sichuan). Shallow water sediments were dominated by limestone abundant in Hirnantia, argillaceous limestone and other lithologic deposits. Deepwater sediments were dominated by Hirnantia-bearing calcareous mudstone and shale deposit. (3) During the deposition period of LM1-LM4 in the bottom of Longmaxi Formation, controlled by global sea level rise and Guangxi movement, the sedimentary range was larger than that in the deposition period of Guanyinqiao Member and the main body was hydropexic deepwater sedimentary environment with thick black shale from LM1-LM4. The maximum thickness is over 20 m. Moreover, the control effect of palaeouplifts in central Sichuan and central Guizhou and Jiangnan-Xuefeng palaeouplift on black shale was further analyzed, and that of underwater highland/uplift in Zhiliujing and western Hubei and Hunan as well as underwater highland in Huaying Mountain and Dingshan on shale deposition and preservation was also explored.

Key words: shale gas, graptolitic zone, Wufeng Formation, Longmaxi Formation, Sichuan Basin and its adjacent areas

中图分类号:

TE122

聂海宽, 金之钧, 马鑫, 刘忠宝, 林拓, 杨振恒. 四川盆地及邻区上奥陶统五峰组-下志留统龙马溪组底部笔石带及沉积特征[J]. 石油学报, 2017, 38(2): 160-174.

Nie Haikuan, Jin Zhijun, Ma Xin, Liu Zhongbao, Lin Tuo, Yang Zhenheng. Graptolites zone and sedimentary characteristics of Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation in Sichuan Basin and its adjacent areas[J]. Acta Petrolei Sinica, 2017, 38(2): 160-174.

参考文献

[1] 张金川,聂海宽,徐波,等.四川盆地页岩气成藏地质条件[J].天然气工业,2008,28(2):151-156.
ZHANG Jinchuan,NIE Haikuan,XU Bo,et al.Geological condition of shale gas accumulation in Sichuan Basin[J].Natural Gas Industry,2008,28(2):151-156.
[2] 聂海宽,唐玄,边瑞康.页岩气成藏控制因素及中国南方页岩气发育有利区预测[J].石油学报,2009,30(4):484-491.
NIE Haikuan,TANG Xuan,BIAN Ruikang.Controlling factors for shale gas accumulation and prediction of potential development area in shale gas reservoir of South China[J].Acta Petrolei Sinica,2009,30(4):484-491.
[3] 金之钧,胡宗全,高波,等.川东南地区五峰组-龙马溪组页岩气富集与高产控制因素[J].地学前缘,2016,23(1):1-10.
JIN Zhijun,HU Zongquan,GAO Bo,et al.Controlling factors on the enrichment and high productivity of shale gas in the Wufeng-Longmaxi Formations,southeastern Sichuan Basin[J].Earth Science Frontiers,2016,23(1):1-10.
[4] 何治亮,聂海宽,张钰莹.四川盆地及其周缘奥陶系五峰组-志留系龙马溪组页岩气富集主控因素分析[J].地学前缘,2016,23(2):8-17.
HE Zhiliang,NIE Haikuan,ZHANG Yuying.The main factors of shale gas enrichment of Ordovician Wufeng Formation-Silurian Longmaxi Formation in the Sichuan Basin and its adjacent areas[J].Earth Science Frontiers,2016,23(2):8-17.
[5] 聂海宽,张金川,包书景,等.四川盆地及其周缘上奥陶统-下志留统页岩气聚集条件[J].石油与天然气地质,2012,33(3):335-345.
NIE Haikuan,ZHANG Jinchuan,BAO Shujing,et al.Shale gas accumulation conditions of the Upper Ordovician-Lower Silurian in Sichuan Basin and its periphery[J].Oil & Gas Geology,2012,33(3):335-345.
[6] LOUCKS R G,RUPPEL S C.Mississippian Barnett Shale:lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin,Texas[J].AAPG Bulletin,2007,91(4):579-601.
[7] WANG Guochang,CARR T R.Organic-rich Marcellus Shale lithofacies modeling and distribution pattern analysis in the Appalachian Basin[J].AAPG bulletin, 2013,97(12):2173-2205.
[8] 聂海宽,金之钧,边瑞康,等.四川盆地及其周缘上奥陶统五峰组-下志留统龙马溪组页岩气"源-盖控藏"富集[J].石油学报,2016,37(5):557-571.
NIE Haikuan,JIN Zhijun,BIAN Ruikang,et al.The "source-cap hydrocarbon-controlling" enrichment of shale gas in Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation of Sichuan Basin and its periphery[J].Acta Petrolei Sinica,2016,37(5):557-571.
[9] 刘树根,马文辛,LUBA J,等.四川盆地东部地区下志留统龙马溪组页岩储层特征[J].岩石学报,2011,27(8):2239-2252.
LIU Shugen,MA Wenxin,LUBA J,et al.Characteristics of the shale gas reservoir rocks in the Lower Silurian Longmaxi Formation,East Sichuan Basin,China[J].Acta Petrologica Sinica,2011,27(8):2239-2252.
[10] 郑和荣,高波,彭勇民,等.中上扬子地区下志留统沉积演化与页岩气勘探方向[J].古地理学报,2013,15(5):645-656.
ZHENG Herong,GAO Bo,PENG Yongmin,et al.Sedimentary evolution and shale gas exploration direction of the Lower Silurian in Middle-Upper Yangtze area[J].Journal of Palaeogeography,2013,15(5):645-656.
[11] 王玉满,董大忠,黄金亮,等.四川盆地及周边上奥陶统五峰组观音桥段岩相特征及对页岩气选区意义[J].石油勘探与开发,2016,43(1):42-50.
WANG Yuman,DONG Dazhong,HUANG Jinliang,et al.Guanyinqiao Member lithofacies of the Upper Ordovician Wufeng Formation around the Sichuan Basin and the significance to shale gas plays,SW China[J].Petroleum Exploration and Development,2016,43(1):42-50.
[12] 陈旭,樊隽轩,陈清,等.论广西运动的阶段性[J].中国科学:地球科学,2014,44(5):842-850.
CHEN Xu,FAN Junxuan,CHEN Qing,et al.Toward a stepwise Kwangsian Orogeny[J].Science China Earth Science s,2014,57(3):379-387.
[13] 戎嘉余,陈旭,王怿,等.奥陶-志留纪之交黔中古陆的变迁:证据与启示[J].中国科学:地球科学,2011,41(10):1407-1415.
RONG Jiayu,CHEN Xu,WANG Yi,et al.Northward expansion of Central Guizhou oldland through the Ordovician and Silurian transition:evidence and implications[J].Scientia Sinica Terrae,2011,41(10):1407-1415.
[14] 苏文博,李志明,ETTENSOHN F R,等.华南五峰组-龙马溪组黑色岩系时空展布的主控因素及其启示[J].地球科学——中国地质大学学报,2007,32(6):819-827.
SU Wenbo,LI Zhiming,ETTENSOHN F R,et al.Distribution of black shale in the Wufeng-Longmaxi formations (Ordovician-Silurian),South China:major controlling factors and implications[J].Earth Science-Journal of China University of Geosciences,2007,32(6):819-827.
[15] CHEN Xu,RONG Jiayu,MITCHELL C E,et al.Late Ordovician to earliest Silurian graptolite and brachiopod biozonation from the Yangtze region,South China,with a global correlation[J].Geological Magazine,2000,137(6):623-650.
[16] 樊隽轩,吴磊,陈中阳,等.四川兴文县麒麟乡五峰组-龙马溪组黑色页岩的生物地层序列[J].地层学杂志, 2013,37(4):513-520.
FAN Junxuan,WU Lei,CHEN Zhongyang,et al.Biostratigraphy of the Wufeng-Lungmachi black shales at Qilin,Xingwen County,Sichuan province[J].Journal of Stratigraphy,2013,37(4):513-520.
[17] 陈旭,樊隽轩,张元动,等.五峰组及龙马溪组黑色页岩在扬子覆盖区内的划分与圈定[J].地层学杂志,2015,39(4):351-358.
CHEN Xu,FAN Junxuan,ZHANG Yuandong,et al.Subdivision and delineation of the Wufeng and Lungmachi black shales in the subsurface areas of the Yangtze platform[J].Journal of Stratigraphy,2015,39 (4):351-358.
[18] 陈旭.论笔石的深度分带[J].古生物学报,1990,29(5):507-526.
CHEN Xu.Graptolite depth zonation[J].Acta Palaeontologica Sinica,1990,29(5):507-526.
[19] 邹才能,董大忠,王玉满,等.中国页岩气特征、挑战及前景(一)[J].石油勘探与开发,2015,42(6):689-701.
ZOU Caineng,DONG Dazhong,WANG Yuman,et al.Shale gas in China:characteristics,challenges and prospects (Ⅰ)[J].Petroleum Exploration and Development,2015,42(6):689-701.
[20] 邹才能,董大忠,王玉满,等.中国页岩气特征、挑战及前景(二)[J].石油勘探与开发,2016,43(2):166-178.
ZOU Caineng,DONG Dazhong,WANG Yuman,et al.Shale gas in China:characteristics,challenges and prospects (Ⅱ)[J].Petroleum Exploration and Development,2016,43(2):166-178.
[21] 王红岩,郭伟,梁峰,等.四川盆地威远页岩气田五峰组和龙马溪组黑色页岩生物地层特征与意义[J].地层学杂志,2015,39(3):289-293.
WANG Hongyan,GUO Wei,LIANG Feng,et al.Biostratigraphy characteristics and scientific meaning of the Wufeng and Longmaxi Formation black shales at Well Wei 202 of the Weiyuan shale gas field,Sichuan Basin[J].Journal of Stratigraphy,2015,39(3):289-293.
[22] NIE Haikuan,JIN Zhijun.Source rock and cap rock controls on the Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation shale gas accumulation in the Sichuan Basin and its peripheral areas[J].Acta Geologica Sinica:English Edition,2016,90(3):1059-1060.
[23] 王秀平,牟传龙,王启宇,等.川南及邻区龙马溪组黑色岩系成岩作用[J].石油学报,2015,36(9):1035-1047.
WANG Xiuping,MOU Chuanlong,WANG Qiyu,et al.Diagenesis of black shale in Longmaxi Formation,southern Sichuan Basin and its periphery[J].Acta Petrolei Sinica,2015,36(9):1035-1047.
[24] 李皎,何登发,梅庆华.四川盆地及邻区奥陶纪构造-沉积环境与原型盆地演化[J].石油学报,2015,36(4):427-445.
LI Jiao,HE Dengfa,MEI Qinghua.Tectonic-depositional environment and proto-type basins evolution of the Ordovician in Sichuan Basin and adjacent areas[J]. Acta Petrolei Sinica,2015,36(4):427-445.
[25] 梁狄刚,郭彤楼,边立曾,等.中国南方海相生烃成藏研究的若干新进展(三):南方四套区域性海相烃源岩的沉积相及发育的控制因素[J].海相油气地质,2009,14(2):1-19.
LIANG Digang,GUO Tonglou,BIAN Lizeng,et al.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,Southern China (Part 3):controlling factors on the sedimentary facies and development of Palaeozoic marine source rocks[J].Marine Origin Petroleum Geology,2009,14(2):1-19.
[26] 张国伟,郭安林,王岳军,等.中国华南大陆构造与问题[J].中国科学:地球科学,2013,43(10):1553-1582.
ZHANG Guowei,GUO Anlin,WANG Yuejun,et al.Tectonics of South China continent and its implications[J].Science China Earth Sciences,2013,56(11):1804-1828.
[27] 王同,杨克明,熊亮,等.川南地区五峰组-龙马溪组页岩层序地层及其对储层的控制[J].石油学报,2015,36(8):915-925.
WANG Tong,YANG Keming,XIONG Liang,et al.Shale sequence stratigraphy of Wufeng-Longmaxi Formation in southern Sichuan and their control on reservoirs[J].Acta Petrolei Sinica,2015,36(8):915-925.
[28] 陈旭,戎嘉余,樊隽轩,等.奥陶-志留系界线地层生物带的全球对比[J].古生物学报,2000,39(1):100-114.
CHEN Xu,RONG Jiayu,FAN Junxuan,et a1.A global correlation of biozones across the Ordovician-Silurian boundary[J].Acta Palaeontologica Sinica,2000,39(1):100-114.
[29] 詹仁斌,刘建波,PERCIVAL I G,等.华南上扬子区晚奥陶世赫南特贝动物群的时空演变[J].中国科学:地球科学,2010,40(9):1154-1163.
ZHAN Renbin,LIU Jianbo,PERCIVAL I G,et al.Biodiversification of Late Ordovician Hirnantia fauna on the Upper Yangtze Platform, South China[J].Science China Earth Sciences,2010,53(12):1800-1810.
[30] 陈旭,戎嘉余,周志毅,等.上扬子区奥陶-志留纪之交的黔中隆起和宜昌上升[J].科学通报,2001,46(12):1052-1056.
CHEN Xu,RONG Jiayu,ZHOU Zhiyi,et al.The Central Guizhou and Yi-chang uplifts,Upper Yangtze region,between Ordovician and Silurian[J].Chinese Science Bulletin,2001,46(18):1580-1584.
[31] 樊隽轩,MELCHIN M J,陈旭,等.华南奥陶-志留系龙马溪组黑色笔石页岩的生物地层学[J].中国科学:地球科学,2012,42(1):130-139.
FAN Junxuan,MELCHIN M J,CHEN Xu,et al.Biostratigraphy and geography of the Ordovician-Silurian Lungmachi black shales in South China[J].Science China Earth Sciences,2011,54(12):1854-1863.
[32] 王怿,戎嘉余,詹仁斌,等.鄂西南奥陶系-志留系交界地层研究兼论宜昌上升[J].地层学杂志,2013,37(3):264-274.
WANG Yi,RONG Jiayu,ZHAN Renbin,et al.On the Ordovician-Silurian boundary strata in Southwestern Hubei,and the Yichang uplift[J].Journal of Stratigraphy,2013,37(3):264-274.
[33] CHEN Xu,RONG Jiayu,LI Yue,et al.Facies patterns and geography of the Yangtze region,South China,through the Ordovician and Silurian transition[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2004,204(3/4):353-372.
[34] WANG Jianpo,DENG Xiaojie,WANG Guan,et al.Types and biotic successions of Ordovician reefs in China[J].Chinese Science Bulletin,2012,57(10):1160-1168.
[35] LÜNING S,CRAIG J,LOYDELL D K,et al.Lower Silurian ‘hot shales’ in North Africa and Arabia:regional distribution and depositional model[J].Earth-Science Reviews,2000,49(1/4):121-200.
[36] ALKHAFAJI M W,ALJUBOURI Z A,ALDOBOUNI I A.Depositional environment of the Lower Silurian Akkas hot shales in the Western Desert of Iraq:results from an organic geochemical study[J].Marine and Petroleum Geology,2015,64:294-303.

四川盆地及邻区上奥陶统五峰组-下志留统龙马溪组底部笔石带及沉积特征

Graptolites zone and sedimentary characteristics of Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation in Sichuan Basin and its adjacent areas

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]	吴建发, 赵圣贤, 范存辉, 夏自强, 季春海, 张成林, 曹埒焰. 川南长宁地区龙马溪组富有机质页岩裂缝发育特征及其与含气性的关系[J]. 石油学报, 2021, 42(4): 428-446.
[2]	糜利栋. 基于产气剖面的页岩气离散裂缝网络反演方法[J]. 石油学报, 2021, 42(4): 481-491.
[3]	何骁, 吴建发, 雍锐, 赵圣贤, 周小金, 张洞君, 张德良, 钟成旭. 四川盆地长宁—威远区块海相页岩气田成藏条件及勘探开发关键技术[J]. 石油学报, 2021, 42(2): 259-272.
[4]	梁兴, 徐政语, 张介辉, 张朝, 李兆丰, 蒋佩, 蒋立伟, 朱斗星, 刘臣. 浅层页岩气高效勘探开发关键技术——以昭通国家级页岩气示范区太阳背斜区为例[J]. 石油学报, 2020, 41(9): 1033-1048.
[5]	陈浩, 周涛, 樊怀才, 张鉴, 杨胜来. 页岩储层人工裂缝岩样制备方法及应力敏感性[J]. 石油学报, 2020, 41(9): 1117-1126.
[6]	李俊乾, 卢双舫, 张鹏飞, 李文镖, 荆铁亚, 冯文俊. 页岩基质孔隙水定量表征及微观赋存机制[J]. 石油学报, 2020, 41(8): 979-990.
[7]	毕海滨, 孟昊, 高日丽, 郑婧, 徐小林, 鞠秀娟, 牛伟, 张劲, 周明庆, 赵丽华. 页岩气未开发区单井可采储量评估方法[J]. 石油学报, 2020, 41(5): 565-573.
[8]	何治亮, 聂海宽, 胡东风, 蒋廷学, 王濡岳, 张钰莹, 张光荣, 卢志远. 深层页岩气有效开发中的地质问题——以四川盆地及其周缘五峰组—龙马溪组为例[J]. 石油学报, 2020, 41(4): 379-391.
[9]	聂海宽, 李东晖, 姜涛, 颜彩娜, 杜伟, 张光荣. 基于笔石带特征的页岩等时地层测井划分方法及意义——以四川盆地及其周缘五峰组—龙马溪组为例[J]. 石油学报, 2020, 41(3): 273-283.
[10]	郭建春, 陶亮, 陈迟, 李鸣, 赵志红. 川南地区龙马溪组页岩混合润湿性评价新方法[J]. 石油学报, 2020, 41(2): 216-225.
[11]	郭彤楼, 何希鹏, 曾萍, 高玉巧, 张培先, 何贵松. 复杂构造区页岩气藏地质特征与效益开发建议——以四川盆地及其周缘五峰组—龙马溪组为例[J]. 石油学报, 2020, 41(12): 1490-1500.
[12]	邱楠生, 冯乾乾, 腾格尔, 申宝剑, 马中良, 俞凌杰, 曹爱强. 川东南丁山地区燕山期—喜马拉雅期差异构造-热演化与页岩气保存[J]. 石油学报, 2020, 41(12): 1610-1622.
[13]	李相方, 冯东, 张涛, 孙政, 何敏侠, 刘庆, 刘文远, 赵文, 李靖. 毛细管力在非常规油气藏开发中的作用及应用[J]. 石油学报, 2020, 41(12): 1719-1733.
[14]	王玉满, 王红岩, 沈均均, 拜文华, 董大忠, 邱振, 李新景, 王灿辉. 川北—鄂西地区下志留统龙马溪组上段厚层斑脱岩的新发现及地质意义[J]. 石油学报, 2020, 41(11): 1309-1323.
[15]	何昌龙, 吕龑, 黄天俊, 李益, 郗诚, 钟光海, 吴仕虎, 杨广广, 干大勇. 基于岩石物理分析的页岩气叠前预测方法在川南威远地区的应用[J]. 石油学报, 2020, 41(10): 1209-1218.