岩性油气藏 ›› 2024, Vol. 36 ›› Issue (2): 136–146.doi: 10.12108/yxyqc.20240213

• 地质勘探 • 上一篇    下一篇

四川盆地简阳地区二叠系火山碎屑岩储层特征与成岩演化

张文播1, 李亚2, 杨田1, 彭思桥2, 蔡来星1, 任启强1   

  1. 1. 成都理工大学 沉积地质研究院, 成都 610059;
    2. 中国石油西南油气田公司 勘探开发研究院, 成都 610041
  • 收稿日期:2023-01-31 修回日期:2023-02-17 出版日期:2024-03-01 发布日期:2024-03-06
  • 第一作者:张文播（1993—），女，成都理工大学在读硕士生，研究方向为油气储层地质学。地址：（610059）四川省成都市成华区二仙桥街道东三路1号成都理工大学。Email：1930271989@qq.com。
  • 通信作者: 杨田（1989—），男，研究员，博士生导师，主要从事沉积学和油气储层地质学相关的科研和教学工作。Email：yangtian9645@126.com/yangtian19@cdut.edu.cn。
  • 基金资助:
    自然资源部沉积盆地与油气资源重点实验室开放基金（编号：cdcgs2020003）资助。

Characteristics and diagenetic evolution of Permian pyroclastic reservoirs in Jianyang area，Sichuan Basin

ZHANG Wenbo1, LI Ya2, YANG Tian1, PENG Siqiao2, CAI Laixing1, REN Qiqiang1   

  1. 1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China;
    2. Research Institute of Exploration and Development, PetroChina Southwest Oil & Gas Field Company, Chengdu 610041, China
  • Received:2023-01-31 Revised:2023-02-17 Online:2024-03-01 Published:2024-03-06

PDF (PC)

212

摘要： 火山碎屑岩油气藏作为重要的非常规油气藏，对油气增储上产具有重要的意义。通过岩心观察，综合薄片鉴定、QEMSCAN扫描、X射线衍射、物性分析、包裹体测温及碳氧同位素分析等资料，系统分析了四川盆地简阳地区二叠系火山碎屑岩储层特征及其成岩演化过程。研究结果表明：①简阳地区二叠系火山碎屑岩储层岩石类型主要包括火山角砾熔岩、凝灰熔岩和熔结火山角砾岩，整体物性都较好，孔隙度为0.78%～32.00%，平均为16.67%，渗透率为0.001～2.680 mD，平均为0.125 mD，属于高孔低渗储层，储集空间以次生孔隙和裂缝为主，包括脱玻化孔、基质溶蚀孔及溶蚀缝等类型。②研究区发育多种成岩作用，主要有熔结、压实、脱玻化、胶结及溶蚀作用等。③研究区经历了同生成岩、表生成岩与埋藏成岩3个阶段，成岩演化受深部热液、大气淡水及有机酸流体的共同影响，一方面流体活动造成热液矿物或碳酸盐胶结物的沉淀对储层物性起破坏性作用；另一方面热液流体促进油气运移，酸性流体的溶蚀改造作用对储层孔隙发育起建设性作用。

关键词: 火山碎屑岩储层, 高孔低渗储层, 深部热液流体, 大气淡水, 有机酸流体, 二叠系, 简阳地区, 四川盆地

Abstract: As important unconventional reservoirs，pyroclastic reservoirs are of great significance for increasing oil and gas storage and production. Based on core observation，thin section identification，QEMSCAN scanning， X-ray diffraction，physical property analysis，inclusion temperature and carbon and oxygen isotope analysis，the characteristics and diagenetic evolution of Permian pyroclastic reservoirs in Jianyang area of Sichaun Basin were systematically analyzed. The results show that：（1）The rocks of Permian pyroclastic reservoirs in Jianyang area are mainly composed of volcanic breccia lava，tuff lava and melt-bonded volcanic breccia，with overall good physical properties，porosity ranging from 0.78% to 32.00%，average of 16.67%，permeability ranging from 0.001 to 2.680 mD，average of 0.125 mD，belonging to high porosity and low permeability reservoirs. The reservoir space is dominated by secondary pores and fractures，including devitrified pores，matrix dissolved pores and dissolved fractures.（2）Various diagenetic processes are developed in the study area，including fusion， compaction，devitrification，cementation and dissolution. （3）The study area experienced three diagenetic stages：syndiagenetic stage，epidiagenetic stage and burial diagenetic stage. The diagenetic evolution was influenced by deep hydrothermal fluids，atmospheric fresh water and organic acid fluids. On the one hand，fluid activities cause the precipitation of hydrothermal minerals or carbonate cements，which has a destructive effect on reservoir physical properties. On the other hand，hydrothermal fluids promote oil and gas migration，and the dissolution and transformation of acidic fluids play a constructive role in the development of reservoir pores.

Key words: pyroclastic reservoir, high porosity and low permeability reservoir, deep hydrothermal fluid, atmospheric fresh water, organic acid fluid, Permian, Jianyang area, Sichuan Basin

中图分类号: 

  • TE122.2
[1] 唐华风,王璞珺,边伟华,等. 火山岩储层地质研究回顾[J]. 石油学报,2020,41(12):1744-1773. TANG Huafeng,WANG Pujun,BIAN Weihua,et al. Review of volcanic reservoir geology[J]. Acta Petrolei Sinica,2020,41(12):1744-1773.
[2] 黄玉龙,王璞珺,邵锐. 火山碎屑岩的储层物性:以松辽盆地营城组为例[J]. 吉林大学学报(地球科学版),2010,40(2):227-236. HUANG Yulong,WANG Pujun,SHAO Rui. Porosity and permeability of pyroclastic rocks of the Yingcheng Formation in Songliao Basin[J]. Journal of Jilin University(Earth Science Edition),2010,40(2):227-236.
[3] 马新华,杨雨,张健,等. 四川盆地二叠系火山碎屑岩气藏勘探重大发现及其启示[J]. 天然气工业,2019,39(2):1-8. MA Xinhua,YANG Yu,ZHANG Jian,et al. A major discovery in Permian volcanic rock gas reservoir exploration in the Sichuan Basin and its implications[J]. Natural Gas Industry,2019,39(2):1-8.
[4] 谢继容,李亚,杨跃明,等. 川西地区二叠系火山碎屑岩规模储层发育主控因素与天然气勘探潜力[J]. 天然气工业,2021, 41(3):48-57. XIE Jirong,LI Ya,YANG Yueming,et al. Main controlling factors and natural gas exploration potential of Permian scale volcanoclastic reservoirs in the western Sichuan Basin[J]. Natural Gas Industry,2021,41(3):48-57.
[5] 朱如凯,崔景伟,毛治国,等. 地层油气藏主要勘探进展及未来重点领域[J]. 岩性油气藏,2021,33(1):12-24. ZHU Rukai,CUI Jingwei,MAO Zhiguo,et al. Main exploration progress and future key fields of stratigraphic reservoirs[J]. Lithologic Reservoirs,2021,33(1):12-24.
[6] 程日辉,沈艳杰,颜景波,等. 海拉尔盆地火山碎屑岩的成岩作用[J]. 岩石学报,2010,26(1):47-54. CHENG Rihui,SHEN Yanjie,YAN Jingbo,et al. Diagenesis of volcaniclastc rocks in Hailaer Basin[J]. Acta Petrologica Sinica, 2010,26(1):47-54.
[7] 张丽媛,纪友亮,刘立,等. 海拉尔-塔木察格盆地南贝尔凹陷下白垩统火山碎屑岩储集层成岩演化及控制因素[J]. 古地理学报,2013,15(2):261-274. ZHANG Liyuan,JI Youliang,LIU Li,et al. Diagenetic evolution and controlling factors of pyroclastic reservoirs of the Lower Cretaceous in Nanbeier Sag,Hailar-Tamtsag Basin[J]. Journal of Palaeogeography(Chinese Edition),2013,15(2):261-274.
[8] 刘小洪,王委委,冯明友,等. 准噶尔盆地克拉美丽气田滴西14井区石炭系蚀变凝灰岩储层热液作用过程及时限[J]. 地球科学,2022,47(5):1694-1710. LIU Xiaohong,WANG Weiwei,FENG Mingyou,et al. Hydrothermal process and duration of Carboniferous altered tuff reservoir in well Dixi 14 area of Kelameili gas field(Junggar Basin), NW China[J]. Earth Science,2022,47(5):1694-1710.
[9] 罗冰,马羚,刘冉,等. 川西简阳地区二叠纪火山岩成岩作用及其对储集性能的影响[J]. 成都理工大学学报(自然科学版),2020,47(6):711-723. LUO Bing,MA Ling,LIU Ran,et al. Diagenesis of Permian volcanic rocks and its influence on reservoir performance in Jianyang area,Sichuan,China[J]. Journal of Chengdu University of Technology(Science & Technology Edition),2020,47(6):711-723.
[10] 李蓉,汤晶,李素华,等. 川西二叠系火山碎屑岩储层特征及发育有利区[J]. 科学技术与工程,2022,22(19):8262-8270. LI Rong,TANG Jing,LI Suhua,et al. Pyroclastic reservoir characteristics and favorable reservoir zone of Permian in western Sichuan[J]. Science Technology and Engineering,2022,22(19):8262-8270.
[11] 何登发,李德生,张国伟,等. 四川多旋回叠合盆地的形成与演化[J]. 地质科学,2011,46(3):589-606. HE Dengfa,LI Desheng,ZHANG Guowei,et al. Formation and evolution of multi-cycle superposed Sichuan Basin,China[J]. Chinese Journal of Geology,2011,46(3):589-606.
[12] 何斌,徐义刚,王雅玫,等. 东吴运动性质的厘定及其时空演变规律[J]. 地球科学,2005,30(1):89-96. HE Bin,XU Yigang,WANG Yamei,et al. Nature of the Dongwu movement and its temporal and spatial evolution[J]. Earth Science,2005,30(1):89-96.
[13] 何斌,徐义刚,肖龙,等. 峨眉山地幔柱上升的沉积响应及其地质意义[J]. 地质论评,2006,52(1):30-37. HE Bin,XU Yigang,XIAO Long,et al. Sedimentary responses to uplift of emeishan mantle plume and its implications[J]. Geological Review,2006,52(1):30-37.
[14] 田景春,林小兵,郭维,等. 四川盆地二叠纪玄武岩喷发事件的油气地质意义[J]. 成都理工大学学报(自然科学版),2017, 44(1):14-20. TIAN Jingchun,LIN Xiaobing,GUO Wei,et al. Geological significance of oil and gas in the Permian basalt eruption event in Sichuan Basin,China[J]. Journal of Chengdu University of Technology(Science & Technology Edition),2017,44(1):14-20.
[15] HE Bin,XU Yigang,CHUNG Sunling,et al. Sedimentary evidence for a rapid,kilometer-scale crustal doming prior to the eruption of the Emeishan flood basalts[J]. Earth and Planetary Science Letters,2003,213(3/4):391-405.
[16] 刘冉,罗冰,李亚,等. 川西地区二叠系火山岩展布与茅口组岩溶古地貌关系及其油气勘探意义[J]. 石油勘探与开发, 2021,48(3):575-585. LIU Ran,LUO Bing,LI Ya,et al. Relationship between Permian volcanic rocks distribution and karst paleogeomorphology of Maokou Formation and its significance for petroleum exploration in western Sichuan Basin,SW China[J]. Petroleum Exploration and Development,2021,48(3):575-585.
[17] COURTILLOT V,JAUPART C,MANIGHETTI I,et al. On causal links between flood basalts and continental breakup[J]. Earth and Planetary Science Letters,1999,166(3):177-195.
[18] XU Yiang,CHUNG Sunling,JAHN B M,et al. Petrologic and geochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwestern China[J]. Lithos,2001, 58(3/4):145-168.
[19] 杨毅,张本健,蒋德生,等. 四川盆地西南部上二叠统峨眉山玄武岩成藏模式初探[J]. 天然气工业,2010,30(5):46-49. YANG Yi,ZHANG Benjian,JIANG Desheng,et al. A preliminary study on hydrocarbon pooling patterns of the Upper Permian Emeishan basalts in southwestern Sichuan Basin[J]. Natural Gas Industry,2010,30(5):46-49.
[20] 彭浩,尹成,何青林,等. 川西地区二叠系热碎屑流火山岩发育特征及其油气地质意义[J]. 石油勘探与开发,2022,49(1):56-67. PENG Hao,YIN Cheng,HE Qinglin,et al. Development characteristics and petroleum geological significance of Permian pyroclastic flow volcanic rocks in western Sichuan Basin,SW China[J]. Petroleum Exploration and Development,2022,49(1):56-67.
[21] 孙善平,刘永顺,钟蓉,等. 火山碎屑岩分类评述及火山沉积学研究展望[J]. 岩石矿物学杂志,2001,20(3):313-317. SUN Shanping,LIU Yongshun,ZHONG Rong,et al. Classification of pyroclastic rocks and trend of volcanic sedimentology:A Review[J]. Acta Petrologica et Mineralogica,2001,20(3):313-317.
[22] 马新华,李国辉,应丹琳,等. 四川盆地二叠系火成岩分布及含气性[J]. 石油勘探与开发,2019,46(2):216-225. MA Xinhua,LI Guohui,YING Danlin,et al. Distribution and gas-bearing properties of Permian igneous rocks in Sichuan Basin,SW China[J]. Petroleum Exploration and Development, 2019,46(2):216-225.
[23] 中国石油天然气总公司. 火山岩储集层描述方法:SY/T5830- 93[S]. 北京:中国标准出版社,1994:2-10. China National Petroleum Corporation. Description method ofvolcanic rock reservoir:SY/T5830-93[S]. Beijing:China Standards Press,1994:2-10.
[24] 赵海玲,黄微,王成,等. 火山岩中脱玻化孔及其对储层的贡献[J]. 石油与天然气地质,2009,30(1):47-52. ZHAO Hailing,HUANG Wei,WANG Cheng,et al. Micropores from devitrification in volcanic rocks and their contribution to reservoirs[J]. Oil & Gas Geology,2009,30(1):47-52.
[25] 马剑,黄志龙,刘再振,等. 三塘湖盆地条湖组含沉积有机质凝灰岩致密储层特征[J]. 地学前缘,2015,22(6):185-196. MA Jian,HUANG Zhilong,LIU Zaizhen,et al. Tight reservoir characteristics of sedimentary organic matter-bearing tuff in Tiaohu Formation of Santanghu Basin[J]. Earth Science Frontiers, 2015,22(6):185-196.
[26] 刘豇瑜,郗爱华,冉启全,等. 准噶尔盆地滴西地区石炭系火山岩储层次生孔隙的岩相学特征及主控因素[J]. 岩性油气藏,2012,24(3):51-55. LIU Jiangyu,XIA Aihua,RAN Qiquan,et al. Petrography characteristics and main controlling factors of secondary pores in Carboniferous volcanic reservoir in Dixi area,Junggar Basin[J]. Lithologic Reservoirs,2012,24(3):51-55.
[27] 陈小丹,陈振宇,程彦博,等. 热液石英中微量元素特征及应用:认识与进展[J]. 地质论评,2011,57(5):707-717. CHEN Xiaodan,CHEN Zhenyu,CHENG Yanbo,et al. Distribution and application of trace elements in hydrothermal quartz:Understanding and prospecting[J]. Geological Review,2011, 57(5):707-717.
[28] 尤丽,范彩伟,吴仕玖,等. 莺歌海盆地乐东区储层碳酸盐胶结物成因机理及与流体活动的关系[J]. 地质学报,2021,95(2):578-587. YOU Li,FAN Caiwei,WU Shijiu,et al. Genesis of carbonate cement and its relationship with fluid activity in the Ledong area,Yinggehai Basin[J]. Acta Geologica Sinica,2021,95(2):578-587.
[29] 王尉,赵路子,罗冰,等. 川西地区二叠系火山岩异常高压演化与天然气成藏的关系[J]. 石油学报,2021,42(11):1437-1445. WANG Wei,ZHAO Luzi,LUO Bing,et al. Relationship between abnormal high pressure evolution of Permian volcanic rocks and natural gas accumulation in the western Sichuan Basin[J]. Acta Petrolei Sinica,2021,42(11):1437-1445.
[30] 刘小洪,冯明友,郗爱华,等. 克拉美丽气田滴西地区石炭系火山岩储层成岩作用及孔隙演化[J]. 岩性油气藏,2016,28(1):38-48. LIU Xiaohong,FENG Mingyou,XI Aihua,et al. Diagenesis and pore evolution of Carboniferous volcanic reservoirs in Dixi area, Kelameili gas field[J]. Lithologic Reservoirs,2016,28(1):38-48.
[31] 刘四兵,黄思静,沈忠民,等. 砂岩中碳酸盐胶结物成岩流体演化和水岩作用模式:以川西孝泉-丰谷地区上三叠统须四段致密砂岩为例[J]. 中国科学:地球科学,2014,44(7):1403-1417. LIU Sibing,HUANG Sijing,SHEN Zhongmin,et al. Diagenetic fluid evolution and water-rock interaction model of carbonate cements in sandstone:An example from the reservoir sandstone of the Fourth member of the Xujiahe Formation of the XiaoquanFenggu area,Sichuan Province,China[J]. Science China:Earth Sciences,2014,44(7):1403-1417.
[32] 杨田. 东营凹陷沙三段深水重力流砂岩与泥岩协同成岩演化及优质储层成因[D]. 青岛:中国石油大学(华东),2017. YANG Tian. Synergistic diagenetic evolution of deep-water gravity flow sandstones-mudstones and genesis of high quality reservoirs in the third member of the Shahejie Formation, Dongying Depression[D]. Qingdao:China University of Petroleum(East China),2017.
[33] KEITH M L,WEBER J N. Carbon and oxygen isotopic composition of selected limestones and fossils[J]. Geochimica et Cosmochimica Acta,1964,28(10/11):1787-1816.
[34] 王大锐. 油气稳定同位素地球化学[M]. 北京:石油工业出版社,2000:295. WANG Darui. Stable isotope geochemistry of oil and gas[M]. Beijing:Petroleum Industry Press,2000:295.
[35] 杨楷乐,何胜林,杨朝强,等. 高温-超压-高CO2背景下致密砂岩储层成岩作用特征:以莺歌海盆地LD10区新近系梅山组- 黄流组为例[J]. 岩性油气藏,2023,35(1):83-95. YANG Kaile,HE Shenglin,YANG Zhaoqiang,et al. Diagenesis characteristics of tight sandstone reservoirs with high temperature,overpressure and high CO2 content:A case study of Neogene Meishan-Huangliu Formation in LD10 area,Yinggehai Basin[J]. Lithologic Reservoirs,2023,35(1):83-95.
[36] BAI Haiqiang,XIE Xiaojun,ZHANG Gongcheng,et al. Mechanism of carbonate cementation and its influence on reservoir in Pinghu Formation of Xihu Sag[J]. Acta Oceanologica Sinica, 2023,42(3):65-75.
[37] FRIEDMAN I,O'NEIL J R. Compilation of stable isotope fractionation factors of geochemical interest[M]. Washington:USGPO,1977.
[38] 强子同. 碳酸盐岩储层地质学[M]. 东营:石油大学出版社, 1998:470. QIANG Zitong. Carbonate reservoir geology[M]. Dongying:Petroleum University Press,1998:470.
[39] 钟金银,何苗,周韬,等. 鄂尔多斯盆地东南缘长8油层组碳酸盐胶结物成因分析[J]. 岩性油气藏,2011,23(4):65-69. ZHONG Jinyin,HE Miao,ZHOU Tao,et al. Origin analysis of carbonate cements in Chang 8 reservoir in southeastern margin of Ordos Basin[J]. Lithologic Reservoirs,2011,23(4):65-69.
[40] YANG Zhi,ZOU Caineng,HE Sheng,et al. Formation mechanism of carbonate cemented zones adjacent to the top overpressured surface in the central Junggar Basin,NW China[J]. Science China(Earth Sciences),2010,53(4):529-540.
[41] 于文修,陆建林,张庆龙,等. 长岭断陷火山岩储层内碳酸盐矿物碳氧同位素组成及其成因[J]. 矿物岩石地球化学通报, 2012,31(1):82-88. YU Wenxiu,LU Jianlin,ZHANG Qinglong,et al. Carbon and oxygen isotopic compositions and genesis of carbonate minerals in a volcanic reservoir from the Changling rift[J]. Bulletin of Mineralogy,Petrology and Geochemistry,2012,31(1):82-88.
[42] 李欣,杜德道,蔡郁文,等. 松辽盆地徐家围子地区火山岩储层主要次生矿物研究[J]. 岩性油气藏,2014,26(6):98-105. LI Xin,DU Dedao,CAI Yuwen,et al. Study on major secondary minerals in volcanic reservoir in Xujiaweizi area,Songliao Basin[J]. Lithologic Reservoirs,2014,26(6):98-105.
[43] 杨献忠,杨祝良,陶奎元,等. 含油玄武岩中绿泥石的形成温度[J]. 矿物学报,2002,22(4):365-371. YANG Xianzhong,YANG Zhuliang,TAO Kuiyuan,et al. Formation temperature of chloritein oil-bearing basalt[J]. Acta Mineralogica Sinica,2002,22(4):365-371.
[44] 王尉,赵路子,张本健,等. 火山岩储层沥青发育特征与天然气富集规律:以川西凹陷带二叠系火山岩为例[J]. 中国矿业大学学报,2021,50(6):1169-1180. WANG Wei,ZHAO Luzi,ZHANG Benjian,et al. Bitumen development characteristics and gas enrichment laws in volcanic rock reservoir:A case study of the Permian volcanic rocks in the Western Sichuan Depression[J]. Journal of China University of Mining & Technology,2021,50(6):1169-1180.
[45] 夏茂龙,文龙,李亚,等. 四川盆地简阳地区二叠系火山喷发旋回、环境与模式[J]. 天然气工业,2020,40(9):11-22. XIA Maolong,WEN Long,LI Ya,et al. Permian volcanic eruption cycle,environment and model in the Jianyang area of the Sichuan Basin[J]. Natural Gas Industry,2020,40(9):11-22.
[1] 白玉彬, 李梦瑶, 朱涛, 赵靖舟, 任海姣, 吴伟涛, 吴和源. 玛湖凹陷二叠系风城组烃源岩地球化学特征及页岩油“甜点”评价[J]. 岩性油气藏, 2024, 36(6): 110-121.
[2] 王义凤, 田继先, 李剑, 乔桐, 刘成林, 张景坤, 沙威, 沈晓双. 玛湖凹陷西南地区二叠系油气藏相态类型及凝析油气地球化学特征[J]. 岩性油气藏, 2024, 36(6): 149-159.
[3] 闫雪莹, 桑琴, 蒋裕强, 方锐, 周亚东, 刘雪, 李顺, 袁永亮. 四川盆地公山庙西地区侏罗系大安寨段致密油储层特征及高产主控因素[J]. 岩性油气藏, 2024, 36(6): 98-109.
[4] 魏成林, 张凤奇, 江青春, 鲁雪松, 刘刚, 卫延召, 李树博, 蒋文龙. 准噶尔盆地阜康凹陷东部深层二叠系超压形成机制及演化特征[J]. 岩性油气藏, 2024, 36(5): 167-177.
[5] 杨海波, 冯德浩, 杨小艺, 郭文建, 韩杨, 苏加佳, 杨皩, 刘成林. 准噶尔盆地东道海子凹陷二叠系平地泉组烃源岩特征及热演化史模拟[J]. 岩性油气藏, 2024, 36(5): 156-166.
[6] 陈康, 戴隽成, 魏玮, 刘伟方, 闫媛媛, 郗诚, 吕龑, 杨广广. 致密砂岩AVO属性的贝叶斯岩相划分方法——以川中地区侏罗系沙溪庙组沙一段为例[J]. 岩性油气藏, 2024, 36(5): 111-121.
[7] 杨学锋, 赵圣贤, 刘勇, 刘绍军, 夏自强, 徐飞, 范存辉, 李雨桐. 四川盆地宁西地区奥陶系五峰组—志留系龙马溪组页岩气富集主控因素[J]. 岩性油气藏, 2024, 36(5): 99-110.
[8] 周刚, 杨岱林, 孙奕婷, 严威, 张亚, 文华国, 和源, 刘四兵. 四川盆地及周缘寒武系沧浪铺组沉积充填过程及油气地质意义[J]. 岩性油气藏, 2024, 36(5): 25-34.
[9] 张晓丽, 王小娟, 张航, 陈沁, 关旭, 赵正望, 王昌勇, 谈曜杰. 川东北五宝场地区侏罗系沙溪庙组储层特征及主控因素[J]. 岩性油气藏, 2024, 36(5): 87-98.
[10] 申有义, 王凯峰, 唐书恒, 张松航, 郗兆栋, 杨晓东. 沁水盆地榆社—武乡区块二叠系煤系页岩储层地质建模及“甜点”预测[J]. 岩性油气藏, 2024, 36(4): 98-108.
[11] 徐田录, 吴承美, 张金凤, 曹爱琼, 张腾. 吉木萨尔凹陷二叠系芦草沟组页岩油储层天然裂缝特征与压裂模拟[J]. 岩性油气藏, 2024, 36(4): 35-43.
[12] 计玉冰, 郭冰如, 梅珏, 尹志军, 邹辰. 四川盆地南缘昭通示范区罗布向斜志留系龙马溪组页岩储层裂缝建模[J]. 岩性油气藏, 2024, 36(3): 137-145.
[13] 王宏波, 张雷, 曹茜, 张建伍, 潘星. 鄂尔多斯盆地二叠系盒8段河流扇沉积模式及勘探意义[J]. 岩性油气藏, 2024, 36(3): 117-126.
[14] 邵威, 周道容, 李建青, 章诚诚, 刘桃. 下扬子逆冲推覆构造后缘凹陷油气富集关键要素及有利勘探方向[J]. 岩性油气藏, 2024, 36(3): 61-71.
[15] 段逸飞, 赵卫卫, 杨天祥, 李富康, 李慧, 王嘉楠, 刘钰晨. 鄂尔多斯盆地延安地区二叠系山西组页岩气源储特征及聚集规律[J]. 岩性油气藏, 2024, 36(3): 72-83.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 旷红伟，高振中，王正允，王晓光. 一种独特的隐蔽油藏——夏9井区成岩圈闭油藏成因分析及其对勘探的启迪[J]. 岩性油气藏, 2008, 20(1): 8 -14 .
[2] 李国军, 郑荣才,唐玉林,汪洋,唐楷. 川东北地区飞仙关组层序- 岩相古地理特征[J]. 岩性油气藏, 2007, 19(4): 64 -70 .
[3] 蔡佳. 琼东南盆地长昌凹陷新近系三亚组沉积相[J]. 岩性油气藏, 2017, 29(5): 46 -54 .
[4] 章惠, 关达, 向雪梅, 陈勇. 川东北元坝东部须四段裂缝型致密砂岩储层预测[J]. 岩性油气藏, 2018, 30(1): 133 -139 .
[5] 付广，刘博，吕延防. 泥岩盖层对各种相态天然气封闭能力综合评价方法[J]. 岩性油气藏, 2008, 20(1): 21 -26 .
[6] 马中良，曾溅辉，张善文，王永诗，王洪玉，刘惠民. 砂岩透镜体油运移过程模拟及成藏主控因素分析[J]. 岩性油气藏, 2008, 20(1): 69 -74 .
[7] 王英民. 对层序地层学工业化应用中层序分级混乱问题的探讨[J]. 岩性油气藏, 2007, 19(1): 9 -15 .
[8] 卫平生, 潘树新, 王建功, 雷　明. 湖岸线和岩性地层油气藏的关系研究 —— 论“坳陷盆地湖岸线控油”[J]. 岩性油气藏, 2007, 19(1): 27 -31 .
[9] 易定红, 石兰亭, 贾义蓉. 吉尔嘎朗图凹陷宝饶洼槽阿尔善组层序地层与隐蔽油藏[J]. 岩性油气藏, 2007, 19(1): 68 -72 .
[10] 杨占龙, 彭立才, 陈启林, 郭精义, 李在光, 黄云峰. 吐哈盆地胜北洼陷岩性油气藏成藏条件与油气勘探方向[J]. 岩性油气藏, 2007, 19(1): 62 -67 .

陇ICP备17006252号
版权所有© 2018 中国石油集团西北地质研究所有限公司《岩性油气藏》编辑部

地址：甘肃省兰州市城关区雁儿湾路535号(陇ICP备17006252号)    电话：0931-8686158;8686058;8686288    邮箱：yxyqc@petrochina.com.cn

甘公网安备 62010202002827号

本系统由北京玛格泰克科技发展有限公司设计开发