岩性油气藏 ›› 2020, Vol. 32 ›› Issue (6): 62–72.doi: 10.12108/yxyqc.20200606

• 油气地质 • 上一篇    下一篇

斜坡背景下沉积物变形构造时空展布规律——以鄂尔多斯盆地镇原地区长7油层组为例

何维领1, 罗顺社2, 李昱东3, 吴悠1, 吕奇奇1, 席明利4   

  1. 1. 长江大学 地球科学学院, 武汉 430100;
    2. 非常规油气湖北省协同创新中心 (长江大学), 武汉 430100;
    3. 中国石油玉门油田分公司 勘探开发研究院, 甘肃 酒泉 735000;
    4. 中国石油长庆油田分公司油田开发事业部, 西安 745000
  • 收稿日期:2020-02-14 修回日期:2020-03-01 出版日期:2020-12-01 发布日期:2020-10-30
  • 第一作者:何维领(1988-),男,长江大学在读博士研究生,研究方向为沉积学、储层地质学及油藏描述。地址:(430100)湖北省武汉市蔡甸区大学路111号。Email:halahwl@163.com。
  • 基金资助:
    国家自然科学基金项目“鄂尔多斯盆地延长组湖泊重力流沉积特征及形成机理研究”（编号：41672099）和国家重点基础研究发展计划“973”项目“淡水湖盆细粒沉积与富有机质页岩形成机理”（编号：2014CB239003）联合资助

Spatio-temporal distribution of soft-sediment deformation structures on slope: a case study of Chang 7 oil reservoir in Zhenyuan area，Ordos Basin

HE Weiling1, LUO Shunshe2, LI Yudong3, WU You1, LYU Qiqi1, XI Mingli4   

  1. 1. School of Geosciences, Yangtze University, Wuhan 430100, China;
    2. Hubei Cooperative Innovation Center of Unconventional Oil and Gas(Yangtze University), Wuhan 430100, China;
    3. Research Institute of Exploration and Development, PetroChina Yumen Oilfield Company, Jiuquan 735000, Gansu, China;
    4. Department of Development, PetroChina Changqing Oilfield Company, Xi'an 745000, China
  • Received:2020-02-14 Revised:2020-03-01 Online:2020-12-01 Published:2020-10-30

PDF (PC)

371

摘要： 为了研究鄂尔多斯盆地长7油层组沉积物变形构造时空展布规律，对盆地西南部镇原地区20口井的岩心进行了精细观察与描述，综合分析了沉积物变形构造的形态特征和形成机制，共识别出7种常见的沉积物变形构造类型，即滑塌变形、液化卷曲变形、泥质撕裂屑、液化砂岩脉、球枕构造、火焰构造和重荷模等。垂向上，沉积物变形构造在长72小层最为发育，长71小层次之，长73小层较少；平面上，在镇原地区中部集中发育，西部和东部局部发育。斜坡背景下沉积物变形构造的形成机制和展布规律为： ①盆山耦合激活了沉积物变形构造的触发因素；②湖进与湖退转换期是沉积物变形构造最为集中发育的阶段；③不同类型沉积物变形构造的分布与坡折带的发育关系密切，随着向半深湖—深湖沉积区推进，其类型发生规律性演化。该研究成果对于探讨沉积物变形构造的分布模式、重力流砂体分布预测及事件沉积等研究具有参考价值。

关键词: 沉积物变形构造, 火焰构造, 分布模式, 长7油层组, 鄂尔多斯盆地

Abstract: In order to study the spatio-temporal distribution of soft-sediment deformation structures of Chang 7 oil reservoir of Upper Triassic Yanchang Formation,the detailed observation and description of core from 20 wells in Zhenyuan area,southwestern Ordos Basin,were carried out. Combined with morphological characteristics and formation mechanism of the soft-sediment deformation structures,seven common types of soft-sediment deformation structures were recognized,including slump deformation,liquefied curled deformation,torn mud intraclasts,liquefaction sandstone dikes,sandy ball-pillow structures,flame structures and load casts. Vertically,softsediment deformation structures are most frequently observed in Chang 72 sublayer,followed by Chang 71 and Chang 73 sublayers. Horizontally,the soft-sediment deformation structures mainly distribute in the deep-water slope-break zone and semi-deep and deep lake where is located in the central and eastern of the study area. The formation mechanism and distribution of soft-sediment deformation structures on slope is that:(1)Basin-mountain coupling has activated triggers for the occurrence of soft-sediment deformation structures.(2)The transition period between the lake transgression and lake regression is the stage when the soft-sediment deformation structures are most concentrated.(3)The distribution of the soft-sediment deformation structures is closely related to the development of slope break zone. From the slope to the semi-deep lake-deep lake environment,various types of softsediment deformation structures have evolved regularly. The results of this study have important reference for the distribution pattern of sedimentary deformation structures,the prediction of gravity flow sand body distribution and the study of sedimentary events.

Key words: soft-sediment deformation structures, flame structure, Distribution pattern, Chang 7 oil reservoir, Ordos Basin

中图分类号: 

  • TE121.3+2
[1] FITCHES W R, MALTMAN A J, et al. Deformation of soft sediments. Journal of the Geological Society, 1978, 135(2):245-251.
[2] MALTMAN A. On the term "soft-sediment deformation". Journal of Structural Geology, 1984, 6(5):589-592.
[3] 邱欣卫,刘池洋,王建强,等. 鄂尔多斯盆地晚三叠世深湖区同沉积变形构造特征及成因. 地质科学, 2013, 48(1):208-220. QIU X W, LIU C Y, WANG J Q, et al. Triggers and characteristics of Late Triassic deep-lacustrine synsedimentary deformation structures in Ordos Basin. Chinese Journal of Geology, 2013, 48(1):208-220.
[4] 杜远生. 中国地震事件沉积研究的若干问题探讨. 古地理学报, 2011, 13(6):581-586. DU Y S. Discussion about studies of earthquake event deposit in China. Journal of Palaeogeography, 2011, 13(6):581-586.
[5] 杜远生, SHI G, 龚一鸣, 等. 东澳大利亚南悉尼盆地二叠系与地震沉积有关的软沉积变形构造. 地质学报, 2007, 81(4):511-518. DU Y S, SHI G, GONG Y M, et al. Permian soft-sediment deformation structures related to earthquake in the southern Sydney Basin, Eastern Australia. Acta Geologica Sinica, 2007, 81(4):511-518.
[6] WALDRON J W F, GAGNON J F. Recognizing soft-sediment structures in deformed rocks of orogens. Journal of Structural Geology, 2011, 33(3):271.
[7] OWEN G, MORETTI M, ALFARO P. Recognising triggers for soft-sediment deformation:Current understanding and future directions. Sedimentary Geology, 2011, 235(3):133-140.
[8] SHANMUGAM G. The seismite problem. Journal of Palaeogeography, 2016, 5(4):318-362.
[9] WHEELER R L. Distinguishing seismic from nonseismic softsediment structures:Criteria from seismic-hazard analysis. Special Paper of the Geological Society of America, 2002, 359(1):1-11.
[10] SHANMUGAM G. Global case studies of soft-sediment deformation structures(SSDS):Definitions, classifications, advances, origins, and problems. Journal of Palaeogeography, 2017, 6(4):251-320.
[11] SEILACHER A. Fault-graded beds interpreted as seismites. Sedimentology, 1969, 13(1/2):155-159.
[12] 宋天锐. 北京十三陵前寒武纪碳酸盐岩地层中的一套可能的地震-海啸序列. 科学通报, 1988, 33(8):609-611. SONG T R. A probable earthquake-tsunami sequence in PreCambrian carbonate strata of Ming tombs district, Beijing. Chinese Science Bulletin, 1988, 33(8):609-611.
[13] 赵青峰,张建国,康文君,等. 辽河坳陷西部凹陷沙四上亚段震积岩特征及地质意义. 岩性油气藏, 2019, 31(5):24-33. ZHAO Q F, ZHANG J G, KANG W J, et al. Characteristics of seismites and their geological significance of the upper fourth member of Shahejie Formation in Western Sag, Liaohe Depression. Lithologic Reservoirs, 2019, 31(5):24-33.
[14] 刘建宁, 何幼斌, 王宁, 等. 济阳坳陷惠民凹陷沙三段地震事件沉积特征及地质意义. 岩性油气藏, 2020, 32(2):14-23. LIU J N, HE Y B, WANG N, et al. Sedimentary characteristics and geological significance of earthquake events of Sha 3 member in Huimin Sag, Jiyang Depression. Lithologic Reservoirs, 2020, 32(2):14-23.
[15] 夏青松, 田景春. 鄂尔多斯盆地南部上三叠统延长组震积岩的发现及地质意义. 沉积学报, 2007, 25(2):246-252. XIA Q S, TIAN J C. Characteristics and geological significance of seismites of the Yanchang Formation, Upper Triassic, Ordos Basin. Acta Sedimentologica Sinica, 2007, 25(2):246-252.
[16] 夏青松, 田景春, 黄昌武. 鄂尔多斯盆地上三叠统延长组震积岩识别标志研究. 成都理工大学学报(自然科学版), 2007, 34(3):312-317. XIA Q S, TIAN J C, HUANG C W. Study on the recognition marks of seismites in Upper Triassic Yanchang Formation, Ordos Basin,China. Journal of Chengdu University of Technology (Science & Technology Edition), 2007, 34(3):312-317.
[17] 李元昊, 刘池洋, 王秀娟. 鄂尔多斯盆地三叠系延长组震积岩特征研究. 沉积学报, 2008, 26(5):772-779. LI Y H, LIU C Y, WANG X J. Discovery and significance of seismites in Late Tertiary Yanchang Formation of Ordos Basin. Acta Sedimentologica Sinica, 2008, 26(5):772-779.
[18] 邵晓岩, 田景春, 张锦泉, 等. 鄂尔多斯盆地上三叠统延长组长4+5油层组中的古地震记录. 古地理学报, 2009, 11(2):177-186. SHAO X Y, TIAN J C, ZHANG J Q, et al. Paleo-seismic records of Chang 4+5 oil-bearing intervals of the Upper Triassic Yanchang Formation in Ordos Basin. Journal of Palaeogeography, 2009, 11(2):177-186.
[19] 李洁, 陈洪德, 林良彪, 等. 鄂尔多斯盆地东南部延长组古地震效应及其地质启迪. 地质论评, 2010, 56(4):480-489. LI J, CHEN H D, LIN L B, et al. Effect of ancient earthquake and its geological significance of Upper Triassic Yanchang Formation in southeast Ordos Basin. Geological Review, 2010, 56(4):480-489.
[20] 田景春, 王文之, 王峰, 等. 鄂尔多斯盆地华池-庆阳地区上三叠统延长组长6油层组古地震变形构造及砂体叠置关系. 古地理学报, 2012, 14(3):303-310. TIAN J C, WANG W Z, WANG F, et al. Palaeoearthquake deformation structures of the Chang 6 interval of Upper Triassic Yanchang Formation and superimposed relationship between sandbodies in Huachi-Qingyang area of Ordos Basin. Journal of Palaeogeography, 2012, 14(3):303-310.
[21] 李元昊, 刘池洋, 王秀娟, 等. 鄂尔多斯盆地三叠系延长组砂岩墙(脉)特征及其地质意义. 中国地质, 2007, 34(3):400-405. LI Y H, LIU C Y, WANG X J, et al. Characteristics and geological significance of sandstone dikes in the Triassic Yanchang Formation of the Ordos Basin. Geology in China, 2007, 34(3):400-405.
[22] 杜芳鹏, 刘池洋, 王建强, 等. 鄂尔多斯盆地南部上三叠统延长组软沉积变形特征及构造意义. 现代地质, 2014, 28(2):314-320. DU F P, LIU C Y, WANG J Q, et al. Characteristics and tectonic sense of soft sedimentary structures in Yanchang Formation, south Ordos Basin. Geoscience, 2014, 28(2):314-320.
[23] 王振, 张元福, 张娜, 等. 鄂尔多斯盆地南部地区延长组深水沉积构造特征及地质意义. 现代地质, 2018, 32(1):121-132. WANG Z, ZHANG Y F, ZHANG N, et al. Deep-water sedimentary structures of Yanchang Formation in southern Ordos Basin and the geological significance. Geoscience, 2018, 32(1):121-132.
[24] 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. 地学前缘, 2012, 19(1):40-50. ZHANG T S, WU Y Y, GUO B C, et al. The characteristics of Late Triassic depositional sequence controlled by foreland thrustfaulting in south-western Ordos Basin. Earth Science Frontiers, 2012, 19(1):40-50.
[25] 邓秀芹, 付金华, 姚泾利, 等. 鄂尔多斯盆地中及上三叠统延长组沉积相与油气勘探的突破. 古地理学报, 2011, 13(4):443-455. DENG X Q, FU J H, YAO J L, et al. Sedimentary facies of the Middle-Upper Triassic Yanchang Formation in Ordos Basin and breakthrough in petroleum exploration. Journal of Palaeogeography, 2011, 13(4):443-455.
[26] 朱筱敏, 刘芬, 朱世发, 等. 鄂尔多斯盆地陇东地区延长组物源区构造属性研究. 高校地质学报, 2015, 21(3):416-425. ZHU X M, LIU F, ZHU S F, et al. On the tectonic property of the provenance area of the Upper Triassic Yanchang Formation in Longdong area, Ordos Basin. Geological Journal of China Universities, 2015, 21(3):416-425.
[27] 杨华, 窦伟坦, 刘显阳, 等. 鄂尔多斯盆地三叠系延长组长7沉积相分析. 沉积学报, 2010, 28(2):254-263. YANG H, DOU W T, LIU X Y, et al. Analysis on sedimentary facies of member 7 in Yanchang Formation of Triassic in Ordos Basin. Acta Sedimentologica Sinica, 2010, 28(2):254-263.
[28] 陈全红, 李文厚, 郭艳琴, 等. 鄂尔多斯盆地南部延长组浊积岩体系及油气勘探意义. 地质学报, 2006, 80(5):656-663. CHEN Q H, LI W H, GUO Y Q, et al. Turbidite systems and the significance of petroleum exploration of Yanchang Formation in the southern Ordos Basin. Acta Geologica Sinica, 2006, 80(5):656-663.
[29] 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.石油勘探与开发, 2014, 41(6):661-670. YANG R C, HE Z L, QIU G Q, et al. Late Triassic gravity flow depositional systems in the southern Ordos Basin. Petroleum Exploration and Development, 2014, 41(6):661-670.
[30] 王起琮, 李文厚, 赵虹, 等. 鄂尔多斯盆地东南部三叠系延长组一段湖相浊积岩特征及意义. 地质科学, 2006, 41(1):54-63. WANG Q Z, LI W H, ZHAO H, et al. Characteristics and significance of lacustrine turbidites in the member 1 of yanchang Formation, Upper Triassic in the southeastern Ordos Basin. Chinese Journal of Geology, 2006, 41(1):54-63.
[31] 廖纪佳, 朱筱敏, 邓秀芹, 等. 鄂尔多斯盆地陇东地区延长组重力流沉积特征及其模式. 地学前缘, 2013, 20(2):29-39. LIAO J J, ZHU X M, DENG X Q, et al. Sedimentary characteristics and model of gravity flow in Triassic Yanchang Formation of Longdong area in Ordos Basin. Earth Science Frontiers, 2013, 20(2):29-39.
[32] 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. 岩性油气藏, 2009, 21(4):73-77. PANG J G, LI W H, SHI S, et al. Sedimentary evolution model and petroleum significance of Chang-7 member turbidite, Ordos Basin. Lithologic Reservoirs, 2009, 21(4):73-77.
[33] 刘芬, 朱筱敏, 李洋, 等. 鄂尔多斯盆地西南部延长组重力流沉积特征及相模式. 石油勘探与开发, 2015, 42(5):577-588. LIU F, ZHU X M, LI Y, et al. Sedimentary characteristics and facies model of gravity flow deposits of Upper Triassic Yanchang Formation in southwestern Ordos Basin, NW China. Petroleum Exploration and Development, 2015, 42(5):577-588.
[34] 崔龙涛, 郝帅, 王春平, 等. 鄂尔多斯盆地镇原北部三叠系延长组长7-长6油层组古地貌与砂体分布特征.古地理学报, 2015, 17(6):805-812. CUI L T, HAO S, WANG C P, et al. Palaeogeomorphology reconstruction and sandbody distribution of the Chang 7-6 intervals of Triassic Yanchang Formation in northern Zhenyuan area, Ordos Basin. Lithologic Reservoirs, 2015, 17(6):805-812.
[35] 崔龙涛, 冯栋, 秦雁群, 等.鄂尔多斯盆地镇北地区延长组长7古地貌与砂体分布特征. 岩性油气藏, 2013, 25(5):65-69. CUI L T, FENG D, QIN Y Q, et al. Palaeogeomorphology reconstruction and sand body distribution of Chang 7 reservoir in Zhenbei area, Ordos Basin. Lithologic Reservoirs, 2013, 25(5):65-69.
[36] 田媛, 钟建华, 王书宝, 等.鄂尔多斯盆地富县探区三叠系延长组震积岩及其地质意义.古地理学报, 2015, 17(4):541-552. TIAN Y, ZHONG J H, WANG S B, et al. Seismites and their geological significances of the Triassic Yanchang Formation in Fuxian exploration area, Ordos Basin. Journal of Palaeogeography, 2015, 17(4):541-552.
[37] 巨银娟, 张小莉. 鄂尔多斯盆地白豹地区三叠系延长组长6段滑塌变形特征研究. 西北大学学报(自然科学版), 2016, 46(1):87-93. JU Y J, ZHANG X L. Slump sedimentary characteristics of the Triassic Chang 6 reservoir from the Baibao area, Ordos Basin. Journal of Northwest University(Natural Science Edition), 2016, 46(1):87-93.
[38] 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. 古地理学报, 2017, 19(5):41-56. YANG R C, YIN W, FAN A P, et al. Fine-grained,lacustrine gravity-flow deposits and their hydrocarbon significance in the Triassic Yanchang Formation in southern Ordos Basin. Journal of Palaeogeography, 2017, 19(5):41-56.
[39] 乔秀夫, 李海兵.枕、球-枕构造:地层中的古地震记录. 地质论评, 2008, 54(6):721-730. QIAO X F, LI H B. Pillow, ball-and-pillow structures:Paleoseismic records within strata. Geological Review, 2008, 54(6):721-730.
[40] 邓秀芹, 罗安湘, 张忠义, 等. 秦岭造山带与鄂尔多斯盆地印支期构造事件年代学对比. 沉积学报, 2013, 31(6):939-953. DENG X Q, LUO A X, ZHANG Z Y, et al. Geochronological comparison on Indosinian tectonic events between Qinling Orogeny and Ordos Basin. Acta Sedimentologica Sinica, 2013, 31(6):939-953.
[41] 王建强, 刘池洋, 李行, 等. 鄂尔多斯盆地南部延长组长7段凝灰岩形成时代、物质来源及其意义. 沉积学报, 2017, 35(4):691-704. WANG J Q, LIU C Y, LI H, et al. Geochronology,potential source and regional implications of tuff intervals in Chang-7 Member of Yanchang Formation, south of Ordos Basin. Acta Sedimentologica Sinica, 2017, 35(4):691-704.
[42] 杨华, 邓秀芹. 构造事件对鄂尔多斯盆地延长组深水砂岩沉积的影响. 石油勘探与开发, 2013, 40(5):513-520. YANG H, DENG X Q. Deposition of Yanchang Formation deepwater sandstone under the control of tectonic events, Ordos Basin. Petroleum Exploration and Development, 2013, 40(5):513-520.
[43] 王建民, 王佳媛. 鄂尔多斯盆地西南部长7深水浊积特征与储层发育. 岩性油气藏, 2017, 29(4):11-19. WANG J M, WANG J Y. Deep-water turbidite characteristics and its reservoir development of Chang 7 oil layers in southwestern Ordos Basin. Lithologic Reservoirs, 2017, 29(4):11-19.
[44] 傅强, 李璟, 邓秀琴, 等.沉积事件对深水沉积过程的影响:以鄂尔多斯盆地华庆地区长6油层组为例. 岩性油气藏, 2019, 31(1):20-29. FU Q, LI J, DENG X Q, et al. Influence of sedimentary events on deep water sedimentation process:a case of Chang 6 reservoir in Huaqing area, Ordos Basin. Lithologic Reservoirs, 2019, 31(1):20-29.
[1] 关蕴文, 苏思羽, 蒲仁海, 王启超, 闫肃杰, 张仲培, 陈硕, 梁东歌. 鄂尔多斯盆地南部旬宜地区古生界天然气成藏条件及主控因素[J]. 岩性油气藏, 2024, 36(6): 77-88.
[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] 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.
[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] 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.
[6] 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.
[7] 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.
[8] 李启晖, 任大忠, 甯波, 孙振, 李天, 万慈眩, 杨甫, 张世铭. 鄂尔多斯盆地神木地区侏罗系延安组煤层微观孔隙结构特征[J]. 岩性油气藏, 2024, 36(2): 76-88.
[9] 雷涛, 莫松宇, 李晓慧, 姜楠, 朱朝彬, 王桥, 瞿雪姣, 王佳. 鄂尔多斯盆地大牛地气田二叠系山西组砂体叠置模式及油气开发意义[J]. 岩性油气藏, 2024, 36(2): 147-159.
[10] 翟咏荷, 何登发, 开百泽. 鄂尔多斯盆地及邻区中—晚二叠世构造-沉积环境与原型盆地演化[J]. 岩性油气藏, 2024, 36(1): 32-44.
[11] 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.
[12] 杜江民, 崔子豪, 贾志伟, 张毅, 聂万才, 龙鹏宇, 刘泊远. 鄂尔多斯盆地苏里格地区奥陶系马家沟组马五5亚段沉积特征[J]. 岩性油气藏, 2023, 35(5): 37-48.
[13] 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.
[14] 尹艳树, 丁文刚, 安小平, 徐振华. 鄂尔多斯盆地安塞油田塞160井区三叠系长611储层构型表征[J]. 岩性油气藏, 2023, 35(4): 37-49.
[15] 薛楠, 邵晓州, 朱光有, 张文选, 齐亚林, 张晓磊, 欧阳思琪, 王淑敏. 鄂尔多斯盆地平凉北地区三叠系长7段烃源岩地球化学特征及形成环境[J]. 岩性油气藏, 2023, 35(3): 51-65.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 段天向, 刘晓梅, 张亚军, 肖述琴. Petrel 建模中的几点认识[J]. 岩性油气藏, 2007, 19(2): 102 -107 .
[2] 张立秋. 南二区东部二类油层上返层系组合优化[J]. 岩性油气藏, 2007, 19(4): 116 -120 .
[3] 张娣，侯中健，王亚辉，王莹，王春联. 板桥—北大港地区沙河街组沙一段湖相碳酸盐岩沉积特征[J]. 岩性油气藏, 2008, 20(4): 92 -97 .
[4] 樊怀才，李晓平，窦天财，吴欣袁. 应力敏感效应的气井流量动态特征研究[J]. 岩性油气藏, 2010, 22(4): 130 -134 .
[5] 田淑芳，张鸿文. 应用生命周期旋回理论预测辽河油田石油探明储量增长趋势[J]. 岩性油气藏, 2010, 22(1): 98 -100 .
[6] 杨凯，郭肖. 裂缝性低渗透油藏三维两相黑油数值模拟研究[J]. 岩性油气藏, 2009, 21(3): 118 -121 .
[7] 翟中喜，秦伟军，郭金瑞. 油气充满度与储层通道渗流能力的定量关系———以泌阳凹陷双河油田岩性油藏为例[J]. 岩性油气藏, 2009, 21(4): 92 -95 .
[8] 戚明辉，陆正元，袁帅，李新华. 塔河油田12 区块油藏水体来源及出水特征分析[J]. 岩性油气藏, 2009, 21(4): 115 -119 .
[9] 李相博,陈启林,刘化清,完颜容,慕敬魁,廖建波,魏立花. 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 .
[10] 刘云， 卢渊，伊向艺，张俊良，张锦良，王振喜. 天然气水合物预测模型及其影响因素[J]. 岩性油气藏, 2010, 22(3): 124 -127 .

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