鄂尔多斯盆地西南部长7深水浊积特征与储层发育

doi:10.3969/j.issn.1673-8926.2017.04.002

岩性油气藏 ›› 2017, Vol. 29 ›› Issue (4): 11–19.doi: 10.3969/j.issn.1673-8926.2017.04.002

鄂尔多斯盆地西南部长7深水浊积特征与储层发育

王建民¹, 王佳媛^2,3

1. 西安石油大学地球科学与工程学院, 西安 710065;
2. 中国科学院地球环境研究所气溶胶化学与物理重点实验室, 西安 710061;
3. 中国科学院地球环境研究所黄土与第四纪地质国家重点实验室, 西安 710061

收稿日期:2016-09-13 修回日期:2016-11-10 出版日期:2017-07-21 发布日期:2017-07-21
作者简介:王建民(1962-),男,博士,教授,主要从事沉积、储层、油气成藏及开发地质等方面的教学与科研工作。地址:(710065)陕西省西安市雁塔区电子二路东段18号西安石油大学地球科学与工程学院。Email:wangjm@xsyu.edu.cn。
基金资助:
陕西省自然科学基金项目“陕北中生界延长组特低渗低阻油层识别与评价”（编号：2010JM5003）与“连续型油藏砂岩疏导体系与石油运移时效性探讨”（编号：2013JM5006）及西安石油大学青年科技创新基金项目“鄂尔多斯盆地伊陕斜坡上的低幅度构造与油气成藏特征研究”（编号：2012BS010）联合资助。

Deep-water turbidite characteristics and its reservoir development of Chang 7 oil layers in southwestern Ordos Basin

WANG Jianmin¹, WANG Jiayuan^2,3

1. School of Earth Science and Engineering, Xi'an Shiyou University, Xi'an 710065, China;
2. Key Laboratory of Aerosol Chemistry & Physics, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China;
3. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China

Received:2016-09-13 Revised:2016-11-10 Online:2017-07-21 Published:2017-07-21

摘要/Abstract

摘要： 为了进一步探讨深水湖盆储层成因及油气勘探潜力问题，依据录井、测井、实验及试采等资料，对鄂尔多斯盆地西南部LM井区长7油层组深水浊积相的发育特征及其对储层发育的影响进行了研究。结果表明， LM井区长7油层组自上而下可划分为3个亚油层组和4个小层，下部长7₃亚油层组发育大套油页岩，中上部长7₂和长7₁亚油层组发育大套浊积岩和典型的鲍马序列，构成了一个完整的深水浊积层序，且可划分出浊积中扇、浊积下扇及深水盆地共3个亚相，以及浊积水道、水道间漫流、水道前缘漫流、浊积末梢、泥页岩及油页岩等6个沉积微相。该大型浊积扇体以浊积中扇为主体，且受西南单一物源及水系控制，砂体的连续性、连通性及复合性均较好，成为长7深水有效储层发育的主要成因类型；油气显示及产能良好，勘探开发潜力较大，是深水相区油气勘探开发的有效目标。

关键词: 油藏带, 空间展布, 沉积特征, 布曲组, 南羌塘坳陷

Abstract: Aiming at the genesis of the deep-water reservoir in lacustrine basin and the potential of petroleum exploration, the deep-water turbidite characteristics and its influence on the reservoirs development of Chang 7 oil layers in LM well field in the southwestern Ordos Basin were studied according to logging,testing,experiments and producing test data, based on single well facies and logging facies analysis. The results show that Chang 7 oil layers can be divided into three sub oil layers and four sub-layers. Chang 7³ sub oil layers in the lower Chang 7 developed a large set of oil shale,and Chang 7² and Chang 7¹ sub oil layers in the middle and upper Chang 7 developed a large set of turbidite and typical Bouma sequence,all of which constituted a complete deep-water turbi-dite facies sequence. The sedimentation can be sequentially divided into three subfacies including turbidite middle fan, turbidite lower fan and deep-water basin, as well as six microfacies types including turbidite channel, interchannel overflow,front channel overflow, turbidite endings, mud shale and oil shale. This large deep-water turbidite fan is dominated by turbidite middle fan and controlled by the southwest provenance and drainage system,with good sandbody continuity,connectivity and composition,and became the major genetic types for Chang 7 effective deep-water reservoir. With good oil show,and great exploration potential, the turbidite fan is an effective prospect for petroleum exploration on deep-water sediments.

Key words: oil reservoir zones, spatial distribution, sedimentary characteristic, Buqu Formation, southern Qiangtang Depression

中图分类号:

TE111.3

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[J]. 岩性油气藏, 2017, 29(4): 11–19.

WANG Jianmin, WANG Jiayuan. Deep-water turbidite characteristics and its reservoir development of Chang 7 oil layers in southwestern Ordos Basin[J]. Lithologic Reservoirs, 2017, 29(4): 11–19.

参考文献

[1] 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.
[2] 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.
[3] 赵俊兴, 李凤杰, 申晓莉, 等.鄂尔多斯盆地南部长6和长7油层浊流事件的沉积特征及发育模式.石油学报, 2008, 29(3):389-394. ZHAO J X, LI F J, SHEN X L, et al. Sedimentary characteristics and development pattern of turbidity event of Chang 6 and Chang 7 oil reservoirs in the southern Ordos Basin. Acta Petrolei Sinica, 2008, 29(3):389-394.
[4] 付金华, 郭正权, 邓秀芹.鄂尔多斯盆地西南地区上三叠统延长组沉积相及石油地质意义.古地理学报, 2005, 7(1):34-44. FU J H, GUO Z Q, DENG X Q. Sedimentary facies of the Yan-chang Formation of Upper Triassic and petroleum geological implication in southwestern Ordos Basin. Journal of Palaeogeography, 2005, 7(1):34-44.
[5] 郑荣才, 文华国, 韩永林, 等.鄂尔多斯盆地白豹地区长6油层组湖底滑塌浊积扇沉积特征及其研究意义.成都理工大学学报(自然科学版), 2006, 33(6):566-575. ZHENG R C, WEN H G, HAN Y L, et al. Discovery and significance of sublacustrine slump turbidite fans in Chang 6 oilbearing formation of Baibao region in Ordos Basin,China. Journal of Chengdu University of Technology(Science & Technology Edition), 2006, 33(6):566-575.
[6] 尚婷, 陈刚, 李文厚, 等.鄂尔多斯盆地富黄探区延长组浊流沉积与油气聚集关系.西北大学学报(自然科学版), 2013, 43(1):81-88. SHANG T, CHEN G, LI W H, et al. Turbidity current deposit and its relation to the hydrocarbon accumulation of Yanchang Formation in Fuhuang exploration area, Ordos Basin. Journal of Northwest University(Natural Science Edition), 2013, 43(1):81-88.
[7] 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.
[8] 张伟, 刘建朝, 高志亮, 等.鄂尔多斯盆地吴堡地区长6段浊积特征及其石油地质意义.地球科学与环境学报, 2012, 34(2):64-71. ZHANG W, LIU J C, GAO Z L, et al. Turbidity characteristics and petroleum geological significance of chang-6 section in Wubu area of Ordos Basin. Journal of Earth Sciences and Environment, 2012, 34(2):64-71.
[9] 傅强, 吕苗苗, 刘永斗.鄂尔多斯盆地晚三叠世湖盆浊积岩发育特征及地质意义.沉积学报, 2008, 26(2):186-192. FU Q, LYU M M, LIU Y D. Developmental characteristics of turbidite and its implication on petroleum geology in Late-Triassic Ordos Basin. Acta Sedimentologica Sinica, 2008, 26(2):186-192.
[10] 田景春, 隆昊, 苏楠, 等.鄂尔多斯盆地白豹-华池地区长6-3厚层块状砂岩成因.成都理工大学学报(自然科学版), 2010, 37(4):359-365. TIAN J C, LONG H, SU N, et al. Genesis of Chang 6-3 sandstone of Upper Triassic Yanchang Formation in Baibao-Huachi area of Ordos Basin, China. Journal of Chengdu University of Technology(Science & Technology Edition), 2010, 37(4):359-365.
[11] 袁珍, 李文厚, 范萌萌, 等.深水块状砂岩沉积特征及其成因机制探讨:以鄂尔多斯盆地东南缘上三叠统长6油层组为例. 地质科技情报, 2011, 30(4):43-49. YUAN Z, LI W H, FAN M M, et al. Genetic mechanism and sedimentary features of deep water massive sandstone:a case study of the Upper Triassic sandstones of Chang 6 Formation in the southeast of Ordos Basin. Geological Science and Technology Information, 2011, 30(4):43-49.
[12] 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.岩性油气藏, 2010, 22(3):16-21. LI X B, CHEN Q L, LIU H Q, et al. Three types of sediment gravity flows and their petroliferous features of Yanchang Formation in Ordos Basin. Lithologic Reservoirs, 2010, 22(3):16-21.
[13] 邹才能, 赵政璋, 杨华, 等.陆相湖盆深水砂质碎屑流成因机制与分布特征——以鄂尔多斯盆地为例.沉积学报, 2009, 27(6):1065-1075. ZOU C N, ZHAO Z Z, YANG H, et al. Genetic mechanism and distribution of sandy debris flows in terrestrial lacustrine basin. Acta Sedimentologica Sinica, 2009, 27(6):1065-1075.
[14] 李相博, 卫平生, 刘化清, 等.浅谈沉积物重力流分类与深水沉积模式.地质评论, 2013, 59(4):607-614. LI X B, WEI P S, LIU H Q, et al. Discussion on the classification of sediment gravity flow and the deep-water sedimentary model. Geological Review, 2013, 59(4):607-614.
[15] 赵文智, 胡素云, 汪泽成, 等.鄂尔多斯盆地基底断裂在上三叠统延长组石油聚集中的控制作用.石油勘探与开发, 2003, 30(5):1-5. ZHAO W Z, HU S Y, WANG Z C, et al. Key role of basement fault control on oil accumulation of Yanchang Formation, Upper Triassic, Ordos Basin. Petroleum Exploration and Development, 2003, 30(5):1-5.
[16] 刘化清, 袁剑英, 李相博, 等.鄂尔多斯盆地延长期湖盆演化及其成因分析.岩性油气藏, 2007, 19(1):52-56. LIU H Q, YUAN J Y, LI X B, et al. Lake basin evolution of Ordos basin during Middle-Late Triassic and its origin analysis. Lithologic Reservoirs, 2007, 19(1):52-56.
[17] 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.
[18] 王若谷, 李文厚, 廖友运, 等.鄂尔多斯盆地三叠系延长组长7段物源区分析.地质通报, 2013, 32(4):671-784. WANG R G, LI W H, LIAO Y Y, et al. Provenance analysis of Chang 7 member of Triassic Yanchang Formation in Ordos Basin. Geological Bulletin of China, 2013, 32(4):671-684.
[19] 王多云, 辛补社, 杨华, 等.鄂尔多斯盆地延长组长7底部凝灰岩锆石SHRIMPU-Pb年龄及地质意义.中国科学:地球科学, 2014, 44(10):2160-2171. WANG D Y, XIN B S, YANG H, et al. Zircon SHRIMP U-Pb age and geological implications of tuff at the bottom of Chang-7 member of Yanchang Formation in the Ordos Basin. Science China:Earth Sciences, 2014, 44(10):2160-2171.
[20] 王建民.陕北志丹地区长6-长2油层组水退型三角洲沉积演化特征.石油勘探与开发, 2008, 35(2):182-187. WANG J M. Sedimentary and evolutionary characteristics of dereliction deltas in Chang 6-Chang 2 oily members, Zhidan region, northern Shaanxi. Petroleum Exploration and Development, 2008, 35(2):182-187.
[21] 卢进才, 李玉宏, 魏仙样, 等.鄂尔多斯盆地三叠系延长组长7油层组油页岩沉积环境与资源潜力研究.吉林大学学报(地球科学版), 2006, 36(6):928-932. LU J C, LI Y H, WEI X Y, et al. Research on the depositional environment and resources potential of the oil shale in the Chang 7 member, Triassic Yanchang Formation in the Ordos Basin. Journal of Jilin University(Earth Science Edition), 2006, 36(6):928-932.
[22] SHANMUGAM G. 深水砂体成因研究新进展.石油勘探与开发, 2013, 40(3):294-301. SHANMUGAM G. New perspectives on deep-water sandstones:implications. Petroleum Exploration and Development, 2013, 40(3):294-301.

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鄂尔多斯盆地西南部长7深水浊积特征与储层发育

Deep-water turbidite characteristics and its reservoir development of Chang 7 oil layers in southwestern Ordos Basin

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