柴西地区下干柴沟组上段湖相碳酸盐岩沉积特征及相模式

doi:10.12108/yxyqc.20180401

岩性油气藏 ›› 2018, Vol. 30 ›› Issue (4): 1–13.doi: 10.12108/yxyqc.20180401

• 油气地质 • 下一篇

柴西地区下干柴沟组上段湖相碳酸盐岩沉积特征及相模式

王建功^1,2, 张道伟³, 易定红¹, 袁剑英^1,2, 石亚军¹, 马新民¹, 高妍芳¹, 张平¹, 王鹏³

1. 中国石油勘探开发研究院西北分院, 兰州 730020;
2. 中国石油集团油藏描述重点实验室, 兰州 730020;
3. 中国石油青海油田分公司, 甘肃敦煌 736200

收稿日期:2018-01-05 修回日期:2018-03-01 出版日期:2018-07-21 发布日期:2018-07-21
作者简介:王建功(1969-),男,博士,高级工程师,主要从事沉积学、层序地层学和油气勘探方面的科研工作。地址:(730020)甘肃省兰州市城关区雁儿湾路535号。Email:wangjg6150@163.com。
基金资助:
国家重大科技专项“柴达木复杂构造区油气成藏、关键勘探技术与新领域目标优选”（编号：2016ZX05003-006）和中国石油天然气股份有限公司重大科技专项“柴达木盆地建设高原大油气田勘探开发关键技术研究与应用”（编号：2016E-01）联合资助

Depositional characteristics and facies model of lacustrine carbonate rocks in the upper member of lower Ganchaigou Formation in western Qaidam Basin

WANG Jiangong^1,2, ZHANG Daowei³, YI Dinghong¹, YUAN jianying^1,2, SHI Yajun¹, MA Xinmin¹, GAO Yanfang¹, ZHANG Ping¹, WANG Peng³

1. PetroChina Research Institute of Petroleum Exploration and Development-Northwest, Lanzhou 730020, China;
2. Key Laboratory of Reservoir Description, CNPC, Lanzhou 730020, China;
3. Research Institute of Exploration and Development, PetroChina Qinghai Oilfield Company, Dunhuang 736200, Gansu, China

Received:2018-01-05 Revised:2018-03-01 Online:2018-07-21 Published:2018-07-21

摘要/Abstract

摘要： 柴达木盆地西部地区下干柴沟组上段为一套含湖相碳酸盐岩地层，在狮子沟地区已发现了高产含油层系和多口日产千吨以上的高产井。为了进一步探索湖相碳酸盐岩油藏特征和分布规律，基于测井、地震以及岩心观察和储层分析化验资料，对湖相碳酸盐岩的元素地球化学特征、结构类型、沉积特征及沉积相展布进行了系统研究。结果表明，柴西地区湖相碳酸盐岩为混合沉积成因，岩性主要为灰云岩和泥灰岩，其次为白云岩和灰岩；碳酸盐岩的结构组分以灰泥为主，其次为颗粒。碳酸盐岩沉积微相主要有泥灰坪和灰云坪，其次为藻滩和颗粒滩。其岩性组合受古地貌、古水介质和古气候的影响，发育有局限性湖泊、半封闭性湖泊与开阔性湖泊等3种碳酸盐岩沉积序列及沉积模式。

关键词: 湖相碳酸盐岩, 咸化湖盆, 下干柴沟组上段, 柴达木盆地

Abstract: Thick and broad lacustrine carbonate sediments developed in the upper member of the lower Ganchaigou Formation(E₃²)in western Qaidam Basin. Multiple oil-bearing series were found in Shizigou area and many oil wells with high yield were drilled. In order to further explore the characteristics and distribution rules of lacustrine carbonate reservoir,the data of logging,seismic,core observation and reservoir test analysis,were used to study the geochemical characteristics,structure types,sedimentary characteristics and main controlling factors of sedimentary facies distribution of lacustrine carbonate rocks. The result shows that the lacustrine carbonate rocks in western Qaidam area are composed of mixed sedimentary rocks,and the lithologies are mainly calcitic dolomite and marl,followed by dolomite and limestone. The structural components of carbonate rocks are mainly mud-crystal and crystallite dominate,followed by particles. The sedimentary microfacies are mainly marl flats and calcite dolomite flats,followed by algal banks and oolitic banks. The lithologic assemblage is mainly affected by palaeogeomorphology,paleo-fluid and paleoclimate. Local salinization lacustrine environment,semi-closed salinization lacustrine environment and open salinization lacustrine environment are developed in the study area. The high-quality carbonate reservoirs are formed by the common action of different sedimentary environments and sedimentary models.

Key words: lacustrine carbonate rocks, salinization lacustrine basin, upper member of lower Ganchaigou Formation, Qaidam Basin

中图分类号:

TE122

王建功, 张道伟, 易定红, 袁剑英, 石亚军, 马新民, 高妍芳, 张平, 王鹏. 柴西地区下干柴沟组上段湖相碳酸盐岩沉积特征及相模式[J]. 岩性油气藏, 2018, 30(4): 1–13.

WANG Jiangong, ZHANG Daowei, YI Dinghong, YUAN jianying, SHI Yajun, MA Xinmin, GAO Yanfang, ZHANG Ping, WANG Peng. Depositional characteristics and facies model of lacustrine carbonate rocks in the upper member of lower Ganchaigou Formation in western Qaidam Basin[J]. Lithologic Reservoirs, 2018, 30(4): 1–13.

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柴西地区下干柴沟组上段湖相碳酸盐岩沉积特征及相模式

Depositional characteristics and facies model of lacustrine carbonate rocks in the upper member of lower Ganchaigou Formation in western Qaidam Basin

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