岩性油气藏 ›› 2024, Vol. 36 ›› Issue (5): 145–155.doi: 10.12108/yxyqc.20240514

• 地质勘探 • 上一篇    下一篇

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

尹虎1,2, 屈红军1, 孙晓晗1, 杨博1, 张磊岗1, 朱荣幸1   

  1. 1. 西北大学地质学系, 大陆动力学国家重点实验室, 西安 710069;
    2. 延长油田股份有限公司 富县采油厂, 陕西 富县 727500
  • 收稿日期:2023-08-03 修回日期:2024-03-20 出版日期:2024-09-01 发布日期:2024-09-04
  • 第一作者:尹虎（1987—），男，高级工程师，西北大学在读博士研究生，研究方向为沉积学及油田开发。地址：（710069）陕西省西安市碑林区太白北路229号。Email：2475632171@qq.com。
  • 通信作者: 屈红军（1967—），男，教授，博士生导师，主要从事沉积学方面的研究。Email：hongjun@nwu.edu.cn。
  • 基金资助:
    国家自然科学基金“华北南缘与西缘早古生代等深流沉积特征类比及地质意义”（编号：41172101）和国家自然科学基金重大项目专题“致密气储层地质评价方法”（编号：41390451）联合资助。

Characteristics of deep-water deposits and evolution law of Triassic Chang 7 reservoir in southeastern Ordos Basin

YIN Hu1,2, QU Hongjun1, SUN Xiaohan1, YANG Bo1, ZHANG Leigang1, ZHU Rongxing1   

  1. 1. State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China;
    2. Fuxian Oil Production Plant, Yanchang Oilfield Co., Ltd., Fuxian 727500, Shaanxi, China
  • Received:2023-08-03 Revised:2024-03-20 Online:2024-09-01 Published:2024-09-04

PDF (PC)

130

摘要： 以沉积学理论为指导，利用野外露头、钻井岩心、测井等资料，对鄂尔多斯盆地东南部三叠系长7油层组深水沉积特征包括相标志、沉积微相类型等进行了研究，并揭示了其沉积演化规律。研究结果表明：①鄂尔多斯盆地东南部三叠系长7油层组深水沉积的相标志包括：岩石中常见水平层理、鲍马序列、槽模沟模、滑动与滑塌构造、撕裂屑、泥包砾等沉积构造，含有深水双壳类和鱼类动物化石，粒度概率曲线中悬浮总体含量大且分选差，测井曲线上可见锯齿状、齿化箱形-钟形-指形、泥岩基线等特征。②研究区长7物源主要来自东北和南部2个方向，发育深湖—半深湖、湖底扇、浅湖沉积，湖底扇包括浊流和砂质碎屑流2种重力流类型，可进一步划分为重力流主水道、溢流沉积、重力流分支水道、分支水道间、朵叶体等微相。湖底扇主水道主要为砂质碎屑流沉积，分支水道和朵叶体主要为浊流沉积。③研究区长7沉积期，中南部主体发育深湖—半深湖、湖底扇沉积，东北部发育浅湖沉积；其中，东北方向发育4个湖底扇体，南部发育2个湖底扇体，半深湖/浅湖界线呈北西向延伸于延安—甘泉一带。长73亚段沉积期，深湖—半深湖范围最大，仅局部发育湖底扇；长72、长71亚段沉积期，湖底扇逐步增多，深湖—半深湖范围有所缩小，整体呈深湖—半深湖与湖底扇交互沉积态势。

关键词: 相标志, 深水沉积, 浊流, 砂质碎屑流, 湖底扇, 长7, 三叠系, 鄂尔多斯盆地东南部

Abstract: Guided by the theory of sedimentology，the data of outcrops，drilling cores and logging were used to study the characteristics of deep-water deposits，including facies markers and sedimentary microfacies types，of Triassic Chang 7 reservoir in southeastern Ordos Basin，and the evolution law was revealed. The results show that：（1）Facies markers of deep-water deposits of Triassic Chang 7 reservoir in southeastern Ordos Basin include sedimentary structures such as horizontal bedding，Bouma sequence，trough mode，sliding and slump structure， tearing debris，mud-clad gravel，containing deep-water bivalves and fish fossils. The total suspended content in the grain size probability curve is large and the sorting is poor，and the features of zigzag，teethed box-bell-finger shaped and mudstone baseline can be seen on the logging curve.（2）The provenance of Chang 7 reservoir in the study area mainly comes from the northeast and south，with the development of deep to semi-deep lake，sublacustrine fan and shallow lake，and shallow lake sediment. The sublacustrine fan includes two types of gravity flow: turbidity flow and sandy debris flow. It can be further divided into microfacies such as gravity flow main channels，overflow deposits，gravity flow branch channels，inter branch channels，and lobes. The main channels of the sublacustrine fan mainly developed sandy debris flow deposits，while the branch channels and lobes are mainly developed turbidite deposits.（3）The sedimentary evolution law of Chang 7 reservoir in the study area is as follows: deep to semi-deep lake and sublacustrine fan deposits were developed in the central and southern parts of the study area，and shallow lake deposits were developed in the northeastern part. Four sublacustrine fans from the northeast direction were developed in the study area and two sublacustrine fans from the south were developed. The boundary between semi-deep lake and shallow lake extends along Yan’an-Ganquan belt from northwest direction. During the sedimentary period of Chang 73，the range of deep to semi-deep lake was the largest，and the sublacustrine fan was locally developed. During the sedimentary period of Chang 72 and Chang 71，the development of sublacustrine fan gradually increased，while the range of deep lake to semi-deep lake gradually lessened，showing an overall trend of interactive sedimentation between deep lake to semi-deep lake and lacustrine fans.

Key words: facies mark, deep water sedimentation, turbidity current, sandy debris flow, sublacustrine fan, Chang 7 reservoir, Triassic, southeastern Ordos Basin

中图分类号: 

  • TE121.3
[1] PETTINGILL S H, WEIMER P. Worldwide deepwater exploration and production:Past, present, and future[J]. The Leading edge, 2002, 21(4):371-376.
[2] 张功成, 屈红军, 赵冲, 等. 全球深水油气勘探40年大发现及未来勘探前景[J]. 天然气地球科学, 2017, 28(10):1447-1477. ZHANG Gongcheng, QU Hongjun, ZHAO Chong, et al. Giant discoveries of oil and gas exploration in global deepwaters in 40 years and the prospect of exploration[J]. Natural Gas Geoscience, 2017, 28(10):1447-1477.
[3] 张功成, 米立军, 屈红军, 等. 全球深水盆地群分布格局与油气特征[J]. 石油学报, 2011, 32(3):369-378. ZHANG Gongcheng, MI Lijun, QU Hongjun, et al. A basic distributional framework of global deepwater basins and hydrocarbon characteristics[J]. Acta Petrolei Sinica, 2011, 32(3):369-378.
[4] 操应长, 金杰华, 刘海宁, 等. 中国东部断陷湖盆深水重力流沉积及其油气地质意义[J]. 石油勘探与开发, 2021, 48(2):247-257. CAO Yingchang, JIN Jiehua, LIU Haining, et al. Deep-water gravity flow deposits in a lacustrine rift basin and their oil and gas geological significance in eastern China[J]. Petroleum Exploration and Development, 2021, 48(2):247-257.
[5] 张家强, 李士祥, 李宏伟, 等. 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. ZHANG Jiaqiang, LI Shixiang, LI Hongwei, et al. Gravity flow deposits in the distal lacustrine basin of the 7th reservoir group of Yanchang Formation and deepwater oil and gas exploration in Ordos Basin:A case study of Chang 73 sublayer of Chengye horizontal well region[J]. Acta Petrolei Sinica, 2021, 42(5):570-587.
[6] KUENEN P H, MIGLIORINI C I. Turbidity Currents as a cause of Graded Bedding[J]. The Journal of Geology, 1950, 58(2):91-127.
[7] BOUMA A H. A graphic presentation of the facies model of salt marsh deposits[J]. Sedimentology, 1963, 2:122-129.
[8] MUTTI E, LUCCHI F R. Turbidites of the northern Apennines:Introduction to facies analysis[J]. International Geology Review, 1972, 20(2):125-166.
[9] AALTO K R. Deep-water sandstone facies and ancient submarine fans:Models for exploration for stratigraphic traps[J]. AAPG Bulletin, 1979, 63(5):810-815.
[10] LOWE D R. Sediment gravity flows:Ⅱ. Depositional models with special reference to the deposits of high-density turbidity currents[J]. Journal of Sedimentary Petrology, 1982, 52(1):279-297.
[11] SHANMUGAM G. The Bouma Sequence and the turbidite mind set[J]. Earth-Science Reviews, 1997, 42(4):201-229.
[12] SHANMUGAM G. 50 years of the turbidite paradigm(1950-1990 s):Deep-water processes and facies models:A critical perspective[J]. Marine and Petroleum Geology, 2000, 17:285-342.
[13] SHANMUGAM G. Ten turbidite myths[J]. Earth-Science Reviews, 2002, 58(3):311-341.
[14] SHANMUGAM G. 深水砂体成因研究新进展[J]. 石油勘探与开发, 2013, 40(3):294-301. SHANMUGAM G. New perspectives on deep-water sandstones:Implications[J]. Petroleum Exploration and Development, 2013, 40(3):294-301.
[15] FUGELLI E M G, OLSEN T R. Risk assessment and play fairway analysis in frontier basins:Part 2-Examples from offshore mid-Norway[J]. AAPG Bulletin, 2005, 89(7):883-896.
[16] BROOKS H L, HODGSON D M, BRUNT R L, et al. Deep-water channel-lobe transition zone dynamics:Processes and depositional architecture, an example from the Karoo Basin, South Africa[J]. Geological Society of America Belletin, 2018, 130(1/10):1723-1746.
[17] MULDER T, SYVITSKI J P M, MIGEON S, et al. et al. Marine hyperpycnal flows:Initiation, behavior and related deposits. A review[J]. Marine and Petroleum Geology, 2003, 20:861-882.
[18] 杨仁超, 金之钧, 孙冬胜, 等. 鄂尔多斯晚三叠世湖盆异重流沉积新发现[J]. 沉积学报, 2015, 33(1):10-20. YANG Renchao, JIN Zhijun, SUN Dongsheng, et al. Discovery of hyperpycnal flow deposits in the Late Triassic lacustrine Ordos Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1):10-20.
[19] ZAVALA C, 潘树新. 异重流成因和异重岩沉积特征[J]. 岩性油气藏, 2018, 30(1):1-18. ZAVALA C, PAN Shuxin. Hyperpycnal flows and hyperpycnites:Origin and distinctive characteristics[J]. Lithologic Reservoirs, 2018, 30(1):1-18.
[20] 操应长, 杨田, 王艳忠, 等. 超临界沉积物重力流形成演化及特征[J]. 石油学报, 2017, 38(6):607-621. CAO Yingchang, YANG Tian, WANG Yanzhong, et al. Formation, evolution and sedimentary characteristics of supercritical sediment gravity-flow[J]. Acta Petrolei Sinica, 2017, 38(6):607-621.
[21] POSTMA G, LANG J, HOYAL D C, et al. Reconstruction of bedform dynamics controlled by supercritical flow in the channellobe transition zone of a deep-water delta(Sant Llorenc del Munt, north-east Spain, Eocene)[J]. Sedimentology, 2021, 68(4):1674-1697.
[22] YANG Tian, CAO Yingchang, LIU Keyu. Depositional elements and evolution of gravity-flow deposits on Lingshan Island(Eastern China):An integrated outcrop-subsurface study[J]. Marine and Petroleum Geology, 2022, 138:105566.
[23] 杨田, 操应长, 王艳忠, 等. 深水重力流类型、沉积特征及成因机制:以济阳坳陷沙河街组三段中亚段为例[J]. 石油学报, 2015, 36(9):1048-1059. YANG Tian, CAO Yingchang, WANG Yanzhong, et al. Types, sedimentary characteristics and genetic mechanisms of deepwater gravity flows:A case study of the middle submember in member 3 of Shahejie Formation in Jiyang Depression[J]. Acta Petrolei Sinica, 2015, 36(9):1048-1059.
[24] 杨仁超, 何治亮, 邱桂强, 等. 鄂尔多斯盆地南部晚三叠世重力流沉积体系[J]. 石油勘探与开发, 2014, 41(6):661-670. YANG Renchao, HE Zhiliang, QIU Guiqiang, et al. Late Triassic gravity flow depositional systems in the southern Ordos Basin[J]. Petroleum Exploration and Development, 2014, 41(6):661-670.
[25] 李相博, 刘化清, 潘树新, 等. 中国湖相沉积物重力流研究的过去、现在与未来[J]. 沉积学报, 2019, 37(5):904-921. LI Xiangbo, LIU Huaqing, PAN Shuxin, et al. The past, present and future of research on deep-water sedimentary gravity flow in lake basins of China[J]. Acta Sedimentologica Sinica, 2019, 37(5):904-921.
[26] 杨华, 李士祥, 刘显阳. 鄂尔多斯盆地致密油、页岩油特征及资源潜力[J]. 石油学报, 2013, 34(1):1-11. YANG Hua, LI Shixiang, LIU Xianyang. Characteristics and resource prospects of tight oil and shale oil in Ordos Basin[J]. Acta Petrolei Sinica, 2013, 34(1):1-11.
[27] 付金华, 刘显阳, 李士祥, 等. 鄂尔多斯盆地三叠系延长组长7段页岩油勘探发现与资源潜力[J]. 中国石油勘探, 2021, 26(5):1-11. FU Jinhua, LIU Xianyang, LI Shixiang, et al. Discovery and resource potential of shale oil of Chang 7 member, Triassic Yanchang Formation, Ordos Basin[J]. China Petroleum Exploration, 2021, 26(5):1-11.
[28] 李士祥, 郭芪恒, 周新平, 等. 鄂尔多斯盆地延长组7段3亚段页岩型页岩油储层特征及勘探方向[J]. 石油学报, 2022, 43(11):1509-1519. LI Shixiang, GUO Qiheng, ZHOU Xinping, et al. Reservoir characteristics and exploration direction of pure shale-type shale oil in the 3rd sub-member, 7th member of Yanchang Formation in Ordos Basin[J]. Acta Petrolei Sinica, 2022, 43(11):1509-1519.
[29] 付金华, 李士祥, 牛小兵, 等. 鄂尔多斯盆地三叠系长7段页岩油地质特征与勘探实践[J]. 石油勘探与开发, 2020, 47(5):870-883. FU Jinhua, LI Shixiang, NIU Xiaobing, et al. Geological characteristics and exploration of shale oil in Chang 7 member of Triassic Yanchang Formation, Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2020, 47(5):870-883.
[30] 冯娟萍, 李文厚, 欧阳征健. 鄂尔多斯盆地黄陵地区上三叠统延长组长7、长6油层组浊积岩沉积特征及地质意义[J]. 古地理学报, 2012, 14(3):295-302. FENG Juanping, LI Wenhou, OUYANG Zhengjian. Sedimentary characters and geological implication of turbidite of the Chang 6 and Chang 7 intervals of upper Triassic Yanchang Formation in Huangling area, Ordos Basin[J]. Journal of Palaeogeography (Chinese Edition), 2012, 14(3):295-302.
[31] 庞军刚, 李文厚, 石硕, 等. 鄂尔多斯盆地长7段浊积岩沉积演化模式及石油地质意义[J]. 岩性油气藏, 2009, 21(4):73-77. PANG Jungang, LI Wenhou, SHI Shuo, et al. Sedimentary evolution model and petroleum significance of Chang-7 member turbidite, Ordos Basin[J]. Lithologic Reservoirs, 2009, 21(4):73-77.
[32] YANG Bo, QU Hongjun, SHI Jianchao, et al. The lithological features of sublacustrine fans and significance to hydrocarbon exploration:A case study of the Chang 7 interval of the Yanchang Formation, southeastern Ordos Basin, North China[J]. Geofluids, 2021, 22:5583191.
[33] 李相博, 刘化清, 完颜容, 等. 鄂尔多斯盆地三叠系延长组砂质碎屑流储集体的首次发现[J]. 岩性油气藏, 2009, 21(4):19-21. LI Xiangbo, LIU Huaqing, WANYAN Rong, et al. First discovery of the sandy debris flow from the Triassic Yanchang Formation, Ordos Basin[J]. Lithologic Reservoirs, 2009, 21(4):19-21.
[34] 孙宁亮, 钟建华, 王书宝, 等. 鄂尔多斯盆地南部三叠系延长组深水重力流沉积特征及其石油地质意义[J]. 古地理学报, 2017, 19(2):299-314. SUN Ningliang, ZHONG Jianhua, WANG Shubao, et al. Sedimentary characteristics and petroleum geologic significance of deep-water gravity flow of the Triassic Yanchang Formation in southern Ordos Basin[J]. Journal of Palaeogeography(Chinese Edition), 2017, 19(2):299-314.
[35] 张倚安, 李士祥, 田景春, 等. 鄂尔多斯盆地上三叠统延长组长7段深水重力流沉积类型[J]. 沉积学报, 2021, 39(2):297-309. ZHANG Yian, LI Shixiang, TIAN Jingchun, et al. Sedimentation types of deep-water gravity flow, Chang 7 member, Upper Triassic Yanchang Formation, Ordos Basin[J]. Acta Sedimentologica Sinica, 2021, 39(2):297-309.
[36] 李相博, 刘化清, 张忠义, 等. 深水块状砂岩碎屑流成因的直接证据:"泥包砾"结构:以鄂尔多斯盆地上三叠统延长组研究为例[J]. 沉积学报, 2014, 32(4):611-622. LI Xiangbo, LIU Huaqing, ZHANG Zhongyi, et al. "Argillaceous parcel" structure:A direct evidence of debris flow origin of deep-water massive sandstone of Yanchang Formation, Upper Triassic, the Ordos Basin[J]. Acta Sedimentologica Sinica, 2014, 32(4):611-622.
[37] 杨仁超, 尹伟, 樊爱萍, 等. 鄂尔多斯盆地南部三叠系延长组湖相重力流沉积细粒岩及其油气地质意义[J]. 古地理学报, 2017, 19(5):791-806. YANG Renchao, YIN Wei, FAN Aiping, et al. Fine-grained, lacustrine gravity-flow deposits and their hydrocarbon significance in the Triassic Yanchang Formation in southern Ordos Basin[J]. Journal of Palaeogeography(Chinese Edition), 2017, 19(5):791-806.
[38] 田荣恒, 鲜本忠, 晁储志, 等. 湖相重力流水道沉积特征与沉积模式:以鄂尔多斯盆地瑶曲铁路桥剖面三叠系延长组为例[J]. 古地理学报, 2021, 23(5):967-982. TIAN Rongheng, Xian Benzhong, CHAO Chuzhi, et al. Sedimentary characteristics and model of lacustrine gravity flow channels:A case study of the Triassic Yanchang Formation of Yaoqu railway-bridge section in Ordos Basin[J]. Journal of Palaeogeograpphy(Chinese Edition), 2021, 23(5):967-982.
[39] 李相博, 陈启林, 刘化清, 等. 鄂尔多斯盆地延长组3种沉积物重力流及其含油气性[J]. 岩性油气藏, 2010, 22(3):16-21. LI Xiangbo, CHEN Qilin, LIU Huaqing, et al. Three types of sediment gravity flows and their petroliferous of Yanchang Formation in Ordos Basin[J]. Lithologic Reservoirs, 2010, 22(3):16-21.
[40] 刘显阳, 郭雯, 刘江艳, 等. 鄂尔多斯盆地湖盆中部长73亚段深水砂质沉积特征及勘探前景[J]. 地球科学, 2023, 48(1):279-292. LIU Xianyang, GUO Wen, LIU Jiangyan, et al. Characteristics and exploration prospects of deep-water sandstone reservoir of Chang 73 sub-member, Ordos Basin[J]. Earth Science, 2023, 48(1):279-292.
[41] 李凤杰, 杨承锦, 代廷勇, 等. 鄂尔多斯盆地华池地区长6油层组重力流特征及控制因素[J]. 岩性油气藏, 2014, 26(1):18-24. LI Fengjie, YANG Chengjin, DAI Tingyong, et al. Characteristics of gravity flow and controlling factors of Chang 6 oil reservoir set in Huachi area, Ordos Basin[J]. Lithologic Reservoirs, 2014, 26(1):18-24.
[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] 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.
[3] 周洪锋, 吴海红, 杨禹希, 向红英, 高吉宏, 贺昊文, 赵旭. 二连盆地巴音都兰凹陷B51井区白垩系阿四段扇三角洲前缘沉积特征[J]. 岩性油气藏, 2024, 36(4): 85-97.
[4] 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.
[5] 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.
[6] 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.
[7] 牛成民, 惠冠洲, 杜晓峰, 官大勇, 王冰洁, 王启明, 张宏国. 辽中凹陷西斜坡古近系东三段湖底扇发育模式及大油田发现[J]. 岩性油气藏, 2024, 36(2): 33-42.
[8] 王天海, 许多年, 吴涛, 关新, 谢再波, 陶辉飞. 准噶尔盆地沙湾凹陷三叠系百口泉组沉积相展布特征及沉积模式[J]. 岩性油气藏, 2024, 36(1): 98-110.
[9] 尹路, 许多年, 乐幸福, 齐雯, 张继娟. 准噶尔盆地玛湖凹陷三叠系百口泉组储层特征及油气成藏规律[J]. 岩性油气藏, 2024, 36(1): 59-68.
[10] 龙盛芳, 侯云超, 杨超, 郭懿萱, 张杰, 曾亚丽, 高楠, 李尚洪. 鄂尔多斯盆地西南部庆城地区三叠系长7段—长3段层序地层特征及演化规律[J]. 岩性油气藏, 2024, 36(1): 145-156.
[11] 孙辉, 范国章, 王红平, 丁梁波, 左国平, 马宏霞, 庞旭, 许小勇. 东非鲁伍马盆地中始新统深水沉积特征及层序界面识别方法[J]. 岩性油气藏, 2023, 35(6): 106-116.
[12] 李恒萱, 温志新, 宋成鹏, 刘祚冬, 季天愚, 沈一平, 耿珂. 塞内加尔盆地演化过程与岩性油气藏勘探前景[J]. 岩性油气藏, 2023, 35(6): 45-53.
[13] 窦立荣, 李志, 杨紫, 张兴阳, 康海亮, 张明军, 张良杰, 丁梁波. 中国石油海外岩性地层油气藏勘探进展与前景展望[J]. 岩性油气藏, 2023, 35(6): 1-9.
[14] 史卜庆, 丁梁波, 马宏霞, 孙辉, 张颖, 许小勇, 王红平, 范国章. 东非海域大型深水沉积体系及油气成藏特征[J]. 岩性油气藏, 2023, 35(6): 10-17.
[15] 魏嘉怡, 王红伟, 刘刚, 李涵, 曹茜. 鄂尔多斯盆地西缘冲断带石炭系羊虎沟组沉积特征[J]. 岩性油气藏, 2023, 35(5): 120-130.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 庞雄奇, 陈冬霞, 张　俊. 隐蔽油气藏的概念与分类及其在实际应用中需要注意的问题[J]. 岩性油气藏, 2007, 19(1): 1 -8 .
[2] 魏钦廉, 郑荣才, 肖玲, 王成玉, 牛小兵. 鄂尔多斯盆地吴旗地区长6 储层特征及影响因素分析[J]. 岩性油气藏, 2007, 19(4): 45 -50 .
[3] 杨秋莲, 李爱琴, 孙燕妮, 崔攀峰. 超低渗储层分类方法探讨[J]. 岩性油气藏, 2007, 19(4): 51 -56 .
[4] 张杰, 赵玉华. 鄂尔多斯盆地三叠系延长组地震层序地层研究[J]. 岩性油气藏, 2007, 19(4): 71 -74 .
[5] 雷卞军，张吉，王彩丽，王晓蓉，李世临，刘斌. 高分辨率层序地层对微相和储层的控制作者用——以靖边气田统5井区马五段上部为例[J]. 岩性油气藏, 2008, 20(1): 1 -7 .
[6] 杨杰，卫平生，李相博. 石油地震地质学的基本概念、内容和研究方法[J]. 岩性油气藏, 2010, 22(1): 1 -6 .
[7] 杨占龙, 张正刚, 陈启林, 郭精义,沙雪梅, 刘文粟. 利用地震信息评价陆相盆地岩性圈闭的关键点分析[J]. 岩性油气藏, 2007, 19(4): 57 -63 .
[8] 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 .
[9] 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 .
[10] 代黎明, 李建平, 周心怀, 崔忠国, 程建春. 渤海海域新近系浅水三角洲沉积体系分析[J]. 岩性油气藏, 2007, 19(4): 75 -81 .

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