岩性油气藏 ›› 2022, Vol. 34 ›› Issue (2): 116–130.doi: 10.12108/yxyqc.20220211

• 地质勘探 • 上一篇    下一篇

四川盆地开江—梁平海槽东侧三叠系飞仙关组鲕滩沉积特征

李阳1,2, 王兴志1,2, 蒲柏宇3, 徐昌海3, 杨西燕1,2, 朱逸青4, 黄梓桑1,2, 康家豪1,2   

  1. 1. 油气藏地质及开发工程国家重点实验室, 成都 610500;
    2. 西南石油大学 地球科学与技术学院, 成都 610500;
    3. 中国石油西南油气田公司 勘探开发研究院, 成都 610041;
    4. 中国石油西南油气田公司 页岩气研究院, 成都 610051
  • 收稿日期:2021-09-05 修回日期:2021-12-08 出版日期:2022-03-01 发布日期:2022-03-14
  • 第一作者:李阳(1997-),男,西南石油大学在读硕士研究生,研究方向为沉积学与储层地质学。地址:(610500)四川省成都市新都区新都大道8号。Email:1538336275@qq.com
  • 通信作者: 王兴志(1964-),男,博士,教授,主要从事储层沉积学等方面的教学与研究工作。Email:wxzswpi@163.com。
  • 基金资助:
    国家科技重大专项“大型油气田及煤层气开发”的子课题“全球性海侵与气候变化对大型地层油气藏形成的控制作用”（编号：7ZX05001001-002）和中国石油西南油气田分公司2019年开发前期评价项目“铁山坡、七里北、渡口河飞仙关组气藏鲕滩及优质储层分布规律研究”（编号：XNS勘研院JS2020-109）联合资助

Sedimentary characteristics of oolitic beach of Triassic Feixianguan Formation in eastern Kaijiang-Liangping trough, Sichuan Basin

LI Yang1,2, WANG Xingzhi1,2, PU Baiyu3, XU Changhai3, YANG Xiyan1,2, ZHU Yiqing4, HUANG Zisang1,2, KANG Jiahao1,2   

  1. 1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu 610500, China;
    2. School of Geoscienceand Technology, Southwest Petroleum University, Chengdu 610500, China;
    3. Research Institute of Exploration and Development, PetroChina Southwest Oil and Gas Field Company, Chengdu 610041, China;
    4. Shale Gas Research Institute, PetroChina Southwest Oil and Gas Field Company, Chengdu 610051, China
  • Received:2021-09-05 Revised:2021-12-08 Online:2022-03-01 Published:2022-03-14

PDF (PC)

228

摘要： 为了厘清四川盆地开江—梁平海槽东侧三叠系飞仙关组层序地层格架下鲕滩的时空分布特征，明确海平面变化对鲕滩迁移的控制机理，开展了岩性特征分析、沉积构造标志识别、层序界面层序地层格架划分等。结果表明：①开江—梁平海槽东侧飞仙关组在持续海退背景下发育2个三级层序（SQ1和SQ2），可进一步细分出5个四级层序（Ⅰ—Ⅴ）。②研究区飞仙关组鲕滩主要分布于Ⅰ—Ⅳ层序，Ⅱ层序内的鲕滩最为发育，单体厚度大、连续性好，而Ⅲ，Ⅰ和Ⅳ层序内的滩体发育程度依次减弱，最差呈不连续的零星状分布。③鲕滩在垂向加积的同时也具有明显的侧向迁移特征，整体由台地内部向斜坡方向迁移，其中Ⅰ层序至Ⅱ层序鲕滩侧向迁移特征最明显。④局部地貌高地发生的高频旋回与碳酸盐岩生产速率协同变化，导致研究区飞仙关组鲕滩呈现垂向加积和多期次叠置现象，而海平面下降到基准面以下时，适合滩体生长的水动力条件由局部高地向局部洼地变迁，使得鲕滩由垂向生长演化为侧向进积。⑤平面上，研究区飞仙关组鲕滩主要沿北西—南东（即台地边缘一带）方向展布，以铁山坡、普光地区最为发育，其次为渡口河、七里北以及罗家寨等地。该研究成果可为开江—梁平海槽地区飞仙关组优质滩相储层勘探提供依据。

关键词: 鲕滩, 层序, 海平面升降, 飞仙关组, 三叠系, 开江—梁平海槽, 四川盆地

Abstract: In order to clarify the temporal and spatial distribution characteristics of oolitic beach under the sequence stratigraphic framework of Triassic Feixianguan Formation in eastern Kaijiang-Liangping trough in Sichuan Basin, and the control mechanism of sea-level change on oolitic beach migration, lithologic characteristics analysis, identification of sedimentary structural markers and division of sequence stratigraphic framework of sequence boundary were carried out.The results show that:(1) Two third-order sequences(SQ1 and SQ2) are developed in Feixianguan Formation in eastern Kaijiang-Liangping trough under the background of continuous regression, which can be further subdivided into five fourth-order sequences(Ⅰ to Ⅴ) (. 2) The oolitic beach of Feixianguan Formation is mainly developed in sequenceⅠ to Ⅳ, and the oolitic beach in sequence Ⅱ is the most developed, with large single thickness and good continuity, while the sedimentary thickness of oolitic beach in sequence Ⅲ, Ⅰ and Ⅳ decreases in turn, and the least developed oolitic beach is with discontinuous and sporadic distribution.(3) Besides vertical aggradation, oolitic beach has obvious lateral migration characteristics, migrating from the interior of the platform to the slope as a whole, and the lateral migration of oolitic beach in sequence I to is the most obvious. (4) The high-frequency cycles in local highlands and the production rate of carbonate rocks change synergistically, resulting in vertical aggradation and multi-stage superposition of oolitic beach of Feixianguan Formation in the study area. When the sea level drops below the base level, the hydrodynamic conditions suitable for beach growth change from local highlands to local depressions, resulting in the change of oolitic beaches from vertical growth to lateral progradation.(5) On the plane, the oolitic beach of Feixianguan Formation in the study area is mainly distributed along NW-SE direction(platform edge), most developed in Tieshanpo and Puguang areas, followed by Dukouhe, Qilibei and Luojiazhai areas. The research results can provide a basis for the exploration of highquality beach facies reservoirs of Feixianguan Formation in Kaijiang-Liangping trough.

Key words: oolitic beach, sequence, sea-level change, Feixianguan Formation, Triassic, Kaijiang-Liangping trough, Sichuan Basin

中图分类号: 

  • TE122.2
[1] 马永生.四川盆地普光超大型气田的形成机制[J].石油学报, 2007, 28(2):9-14. MA Yongsheng. Generation mechanism of Puguang gas field in Sichuan Basin[J]. Acta Petrolei Sinica, 2007, 28(2):9-14.
[2] 吴婷婷, 王兴志, 冯仁蔚.普光气田飞仙关组成岩作用对滩相储层的影响[J].岩性油气藏, 2012, 24(6):94-100. WU Tingting, WANG Xingzhi, FENG Renwei. Influence of diagenesis on beach reservoirs of Feixianguan Formation in Puguang gas field[J]. Lithologic Reservoirs, 2012, 24(6):94-100.
[3] 郭旭升, 胡东风, 李宇平, 等.四川盆地元坝气田发现与理论技术[J].石油勘探与开发, 2018, 45(1):14-26. GUO Xusheng, HU Dongfeng, LI Yuping, et al. Discovery and theoretical and technical innovations of Yuanba gas field in Sichuan Basin, SW China[J]. Petroleum Exploration and Development, 2018, 45(1):14-26.
[4] 邵晓州, 秦启荣, 范晓丽, 等.川东北黄龙场构造飞仙关组四段底部裂缝预测研究[J].岩性油气藏, 2011, 23(5):96-100. SHAO Xiaozhou, QIN Qirong, FAN Xiaoli, et al. Fracture prediction of bottom T 1f 4 in Huanglongchang structure, northeastern Sichuan Basin[J]. Lithologic Reservoirs, 2011, 23(5):96-100.
[5] 胡东风, 王良军, 黄仁春, 等.四川盆地中国石化探区油气勘探历程与启示[J].新疆石油地质, 2021, 42(3):283-290. HU Dongfeng, WANG Liangjun, HUANG Renchun, et al. Petroleum exploration history and enlightenment in Sichuan Basin:A case study on Sinopec exploration areas[J]. Xinjiang Petroleum Geology, 2021, 42(3):283-290.
[6] 杨雨, 王一刚, 文应初, 等.川东飞仙关组沉积相与鲕滩气藏的分布[J].天然气勘探与开发, 2001, 4(3):18-21. YANG Yu, WANG Yigang, WEN Yingchu, et al. Feixianguan Formation and oolitic beach reservoirs distribution in east of Sichuan Basin[J]. Natural Gas Exploration and Development, 2001, 4(3):18-21.
[7] 谭先锋, 李洁, 何金平, 等.开江-梁平海槽区带南段飞仙关组层序-岩相古地理特征[J].中国地质, 2012, 39(3):612-622. TAN Xianfeng, LI Jie, HE Jinping, et al. Sequence-lithofacies paleogeographic characteristics of Feixianguan Formation in southern section of Kaijiang-Liangping ocean trough[J]. Geology in China, 2012, 39(3):612-622.
[8] 乔占峰.川东北地区普光气田飞仙关组层序地层与储层精细研究[D].成都:成都理工大学, 2008. QIAO Zhanfeng. Fine study on sequence stratigraphy and reservoir of Feixianguan Formation in Puguang gas field, northeast Sichuan[D]. Chengdu:Chengdu University of Technology, 2008.
[9] 李文茂.川东北元坝地区飞仙关组层序地层与储层特征研究[D].成都:成都理工大学, 2010. LI Wenmao. Sequence stratigraphy and reservoir characteristics of Feixianguan Formation in Yuanba area, northeastern Sichuan Basin[D]. Chengdu:Chengdu University of Technology, 2010.
[10] 唐丹.川东北龙岗地区飞仙关组层序地层与储层特征研究[D].成都:西南石油大学, 2012. TANG Dan. Study on sequence stratigraphy and reservoir characteristics of Feixianguan Formation of Longgang area in northeast Sichuan Basin[D]. Chengdu:Southwest Petroleum University, 2012.
[11] 黄仁春, 邢凤存, 范小军, 等.四川盆地元坝地区长兴组-飞仙关组高精度层序地层格架的建立及礁滩储集层预测[J].古地理学报, 2019, 21(2):369-378. HUANG Renchun, XING Fengcun, FAN Xiaojun, et al. Establishment of high-precision sequence stratigraphic framework of the Changxing-Feixianguan formations and prediction of reefshoal reservoirs in Yuanba area, Sichuan Basin[J]. Journal of Palaeogeography, 2019, 21(2):369-378.
[12] 马永生, 牟传龙, 郭彤楼, 等.四川盆地东北部飞仙关组层序地层与储层分布[J].矿物岩石, 2005, 25(4):73-79. MA Yongsheng, MU Chuanlong, GUO Tonglou, et al. Sequence stratigraphy and reservoir distribution of the Changxing Formation in northeastern Sichuan Basin[J]. Earth Science Frontiers, 2005, 25(4):73-79.
[13] 郑雅丽, 丁国生, 张险峰.层序地层学在碳酸盐岩气藏开发早期地质评价阶段的应用-以川东北罗家寨鲕滩气藏为例[J].石油勘探与开发, 2006, 33(4):466-469. ZHENG Yalin, DING Guosheng, ZHANG Xianfeng. Application of sequence stratigraphy to early geological evaluation of carbonate gas reser-voir development:An example from Luojiazhai oolitic bank gas reservoir in NE Sichuan Basin[J]. Petroleum Exploration and Development, 2006, 33(4):466-469.
[14] 李国军, 郑荣才, 唐玉林, 等.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. LI Guojun, ZHENG Rongcai, TANG Yulin, et al. Sequence-based lithofacies paleogeography of Lower Triassic Feixianguang Formation in northeast Sichuan Basin[J]. Lithologic Reservoirs, 2007, 19(4):64-70.
[15] 孙春燕, 胡明毅, 胡忠贵.川东北达川-万县地区下三叠统飞仙关组层序地层研究[J].岩性油气藏, 2017, 29(4):30-37. SUN Chunyan, HU Minyi, HU Zhonggui. Characteristics of sequence stratigraphy of the Lower Triassic Feixianguan Formation in Dachuan-Wanxian area, northeastern Sichuan Basin[J]. Lithologic Reservoirs, 2017, 29(4):30-37.
[16] 任婕, 胡忠贵, 胡明毅, 等.涪陵地区下三叠统飞仙关组沉积相特征及有利储集体分布[J].岩性油气藏, 2021, 33(6):70-80. REN Jie, HU Zhonggui, HU Minyi, et al. Sedimentary facies characteristics and favorable reservoir distribution of Feixianguan Formation of Lower Triassic in Fuling area[J]. Lithologic Reservoirs, 2021, 33(6):70-80.
[17] 黄梓桑, 王兴志, 杨西燕, 等.沉积环境对页岩中有机质富集的约束-以蜀南地区五峰组-龙马溪组为例[J].沉积学报, 2021, 39(3):631-644. HUANG Zisang, WANG Xingzhi, YANG Xiyan, et al. Constraints of sedimentary environment on organic matter accumulation in shale:A case study of the Wufeng-Longmaxi Formations in the southern Sichuan Basin[J]. Acta Sedimentologica Sinica, 2021, 39(3):631-644.
[18] 王兴志, 李博, 杨西燕, 等.四川盆地北部中二叠世晚期"广元-旺苍"海槽特征及其油气地质意义[J].石油勘探与开发, 2021, 48(3):562-574. WANG Xingzhi, LI Bo, YANG Xiyan, et al. Characteristics of the "Guangyuan-Wangcang" trough during late Middle Permian and its petroleum geological significance in the northern Sichuan Basin[J]. Petroleum Exploration and Development, 2021, 48(3):562-574.
[19] 黄仁春.四川盆地二叠纪-三叠纪开江-梁平陆棚形成演化与礁滩发育[J].成都理工大学学报(自然科学版), 2014, 41 (4):452-457. HUANG Renchun.Formation and evolution of Permian-Triassic Kaijiang-Liangping shelf and development of reef-shoal reservoirs in Sichuan Basin[J]. Journal of Chengdu University of Technology(Science & Technology Edition), 2014, 41(4):452-457.
[20] 王一刚, 文应初, 张帆, 等.川东地区上二叠统长兴组生物礁分布规律[J].天然气工业, 1998, 18(6):10-15. WANG Yigang, WEN Yingchu, ZHANG Fan, et al. Distribution of organic reefs in the Upper Permian Changxing Formation, eastern Sichuan Basin[J]. Natural Gas Industry, 1998, 18(6):10-15.
[21] 姚军辉, 罗志立, 孙玮, 等.峨眉地幔柱与广旺-开江-梁平等拗拉槽形成关系[J].新疆石油地质, 2011, 32(1):97-101. YAO Junhui, LUO Zhili, SUN Wei, et al. Relationship between Emei mantle plume and aulacogens of Guangwang-Kaijiang-Liangping[J]. Xinjiang Petroleum Geology, 2011, 32(1):97-101.
[22] 杨雨, 文应初.川东北开江-梁平海槽发育对 T1f鲕粒岩分布的控制[J].天然气工业, 2002, 22(增刊):30-32. YANG Yu, WEN Yingchu. Control of Kaijiang-Liangping trough growing on T1f oolitic distribution in northeastern Sichuan Basin[J]. Natural Gas Industry, 2002, 22(Suppl 1):30-32.
[23] 冯仁蔚, 王兴志, 张帆, 等.四川盆地东北部下三叠统飞一-飞三段孤立碳酸盐岩台地沉积相及相关研究[J].中国地质, 2008, 35(1):54-66. FENG Renwei, WANG Xingzhi, ZHANG Fan, et al. Sedimentary facies of isolated carbonate platform of the first to third members of the Lower Triassic Feixianguan Formation in the northeastern part of the Sichuan Basin and other related aspects[J]. Geology in China, 2008, 35(1):54-66.
[24] 蒋裕强, 谷一凡, 徐昌海, 等.开江-梁平海槽东侧飞仙关组岩相分区及地质意义[J].天然气地球科学, 2018, 29(8):1067-1077. JIANG Yuqiang, GU Yifan, XU Changhai, et al. Feixianguan Formation lithofacies zoning and its geological significance of eastern side of Kaijiang-Liangping Trough, NE Sichuan Basin[J]. Natural Gas Geoscience, 2018, 29(8):1067-1077.
[25] 李文汉.层序地层学基础和关键定义[J].岩相古地理, 1989, 4 (6):32-39. LI Wenhan. Basis and key definitions of sequence stratigraphy[J]. Sedimentary Facies and Palaeogeography, 1989, 4(6):32-39.
[26] 徐怀大, 魏魁生, 洪卫东.层序地层学原理(海平面变化综合分析)[M].北京:石油工业出版社, 1995. XU Huaida, WEI Kuisheng, HONG Weidong. Principle of sequence stratigraphy(comprehensive analysis of sea level change)[M]. Beijing:Petroleum Industry Press, 1995.
[27] MITCHUM R M, JR M, VAN WAGONER J C. High-frequency sequence and their stacking pattern:Sequence-stratigraphic evidence of high-frequency eustatic cycles[J]. Sedimentary Geology, 1991, 70(2/3/4):131-160.
[28] SARG J F.The sequence stratigraphy, sedimentology, and economic importance of evaporite-carbonate transitions:A review[J]. Sedimentary Geology, 2001, 140(1):9-34.
[29] 梅冥相.从沉积层序到海平面变化层序-层序地层学一个重要的新进展[J].地层学杂志, 2015, 39(1):58-73. MEI Mingxiang. From sedimentary sequence to sea-level change sequence:An important new advance in sequence stratigraphy[J]. Journal of Stratigraphy, 2015, 39(1):58-73.
[30] SLOSS L L. Forty years of sequence stratigraphy[J]. Geological Society of America Bulletin, 1988, 100(11):1661-1665.
[31] MIALL A D. Sequence stratigraphy and their chrono stratigraphical correlation[J]. Journal of Sedimentary Petrology, 1991, 61(4):497-505.
[32] EINSELE G.Sedimentary basins:Evolution, facies, and sediment budget[M]. Berlin:Springer-Verlag, 1992.
[33] BOLILA S, GALBRUN B, MILLER K G, et al. On the origin of Cenozoic and Mesozoic "third-order" eustatic sequences[J]. Earth-Science Reviews, 2011, 109(3/4):94-112.
[34] 王鸿祯, 史晓颖.沉积层序及海平面旋回的分类级别-旋回周期的成因讨论[J].现代地质, 1998, 12(1):2-17. WANG Hongzhen, SHI Xiaoying. Hierarchy of depositional sequences and eustatic cycles:A discussion on the mechanism of sedimentary cycles[J]. Geoscience, 1998, 12(1):2-17.
[35] 殷鸿福, 童金南, 丁梅华, 等.扬子区晚二叠世-中三叠世海平面变化[J].地球科学, 1994, 19(5):627-632. YIN Hongfu, TONG Jinnan, DING Meihua, et al. Sea level changes in Yangtze from the Late Permian to the Middle Triassic[J]. Earth Science, 1994, 19(5):627-632.
[36] 王成善, 李祥辉, 陈洪德.中国南方二叠纪海平面变化及升降事件[J].沉积学报, 1999, 17(4):39-44. WANG Chengshan, LI Xianghui, CHEN Hongde. Permian sealevel changes and rising-falling events in South China[J]. Acta Sedimentologica Sinica, 1999, 17(4):39-44.
[37] 王兴志, 张帆, 马青.四川盆地东部晚二叠世-早三叠世飞仙关期礁、滩特征与海平面变化[J].沉积学报, 2002, 20(2):249-254. WANG Xingzhi, ZHANG Fan, MA Qing. The characteristic of reef and bank and the fluctuation of sea level in Feixianguang period of Late Permain-Early Triassic, east Sichuan Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2):249-254.
[38] 朱筱敏.沉积岩石学[M].第 4版.北京:石油工业出版社, 2008:395-396. ZHU Xiaomin. Sedimentary petrology[M]. 4th ed. Beijing:Petroleum Industry Press, 2008:395-396.
[39] 刘建强.川东北地区飞仙关组鲕滩分布规律[D].成都:西南石油大学, 2012. LIU Jiangqiang. Distribution law of oolitic shoal of Feixianguan Formation in northeast Sichuan[D]. Chengdu:Southwest Petroleum University, 2012.
[1] 赵军, 李勇, 文晓峰, 徐文远, 焦世祥. 基于斑马算法优化支持向量回归机模型预测页岩地层压力[J]. 岩性油气藏, 2024, 36(6): 12-22.
[2] 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.
[3] 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.
[4] 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.
[5] 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.
[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] 王子昕, 柳广弟, 袁光杰, 杨恒林, 付利, 王元, 陈刚, 张恒. 鄂尔多斯盆地庆城地区三叠系长7段烃源岩特征及控藏作用[J]. 岩性油气藏, 2024, 36(5): 133-144.
[8] 尹虎, 屈红军, 孙晓晗, 杨博, 张磊岗, 朱荣幸. 鄂尔多斯盆地东南部三叠系长7油层组深水沉积特征及演化规律[J]. 岩性油气藏, 2024, 36(5): 145-155.
[9] 牟蜚声, 尹相东, 胡琮, 张海峰, 陈世加, 代林锋, 陆奕帆. 鄂尔多斯盆地陕北地区三叠系长7段致密油分布特征及控制因素[J]. 岩性油气藏, 2024, 36(4): 71-84.
[10] 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.
[11] 曹江骏, 王茜, 王刘伟, 李诚, 石坚, 陈朝兵. 鄂尔多斯盆地合水地区三叠系长7段夹层型页岩油储层特征及主控因素[J]. 岩性油气藏, 2024, 36(3): 158-171.
[12] 宋志华, 李垒, 雷德文, 张鑫, 凌勋. 改进的U-Net网络小断层识别技术在玛湖凹陷玛中地区三叠系白碱滩组的应用[J]. 岩性油气藏, 2024, 36(3): 40-49.
[13] 张文播, 李亚, 杨田, 彭思桥, 蔡来星, 任启强. 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[J]. 岩性油气藏, 2024, 36(2): 136-146.
[14] 白雪峰, 李军辉, 张大智, 王有智, 卢双舫, 隋立伟, 王继平, 董忠良. 四川盆地仪陇—平昌地区侏罗系凉高山组页岩油地质特征及富集条件[J]. 岩性油气藏, 2024, 36(2): 52-64.
[15] 岑永静, 梁锋, 王立恩, 刘倩虞, 张鑫哲, 丁熊. 四川盆地蓬莱—中江地区震旦系灯影组二段成藏特征[J]. 岩性油气藏, 2024, 36(2): 89-98.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 黄思静,黄培培,王庆东,刘昊年,吴　萌,邹明亮. 胶结作用在深埋藏砂岩孔隙保存中的意义[J]. 岩性油气藏, 2007, 19(3): 7 -13 .
[2] 刘震, 陈艳鹏, 赵阳,, 郝奇, 许晓明, 常迈. 陆相断陷盆地油气藏形成控制因素及分布规律概述[J]. 岩性油气藏, 2007, 19(2): 121 -127 .
[3] 丁超，郭兰，闫继福. 子长油田安定地区延长组长6 油层成藏条件分析[J]. 岩性油气藏, 2009, 21(1): 46 -50 .
[4] 李彦山，张占松，张超谟，陈鹏. 应用压汞资料对长庆地区长6 段储层进行分类研究[J]. 岩性油气藏, 2009, 21(2): 91 -93 .
[5] 罗 鹏,李国蓉,施泽进,周大志,汤鸿伟,张德明. 川东南地区茅口组层序地层及沉积相浅析[J]. 岩性油气藏, 2010, 22(2): 74 -78 .
[6] 左国平，屠小龙，夏九峰. 苏北探区火山岩油气藏类型研究[J]. 岩性油气藏, 2012, 24(2): 37 -41 .
[7] 王飞宇. 提高热采水平井动用程度的方法与应用[J]. 岩性油气藏, 2010, 22(Z1): 100 -103 .
[8] 袁云峰，才业，樊佐春，姜懿洋，秦启荣，蒋庆平. 准噶尔盆地红车断裂带石炭系火山岩储层裂缝特征[J]. 岩性油气藏, 2011, 23(1): 47 -51 .
[9] 袁剑英，付锁堂，曹正林，阎存凤，张水昌，马达德. 柴达木盆地高原复合油气系统多源生烃和复式成藏[J]. 岩性油气藏, 2011, 23(3): 7 -14 .
[10] 耿燕飞，张春生，韩校锋，杨大超. 安岳—合川地区低阻气层形成机理研究[J]. 岩性油气藏, 2011, 23(3): 70 -74 .

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