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首页» 过刊浏览» 2021» Vol.6» Issue(4) 553-565     DOI : 10.3969/j.issn.2096-1693.2021.04.038
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饶阳凹陷西6区块沙一上段沉积微相及其含油气性
吕传炳,庞雄奇,庞宏,付亮亮 ,郑定业,刘本芬 ,耿荣燕
1 中国石油华北油田分公司,河北任丘 062552 2 中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249 3 中国石油大学(北京)地球科学学院,北京 102249
Sedimentary microfacies and oil/gas-bearing ability of the upper member of Es1 in the Xi-6 area, Raoyang sag
LYU Chuanbing, PANG Xiongqi, PANG Hong, FU Liangliang, ZHENG Dingye, LIU Benfen, GENG Rongyan
1 Huabei Oilfield company of PetroChina, Renqiu 062552, China 2 State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum-Beijing, Beijing 102249, China 3 College of Geoscience, China University of Petroleum-Beijing, Beijing 102249, China

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摘要  利用岩心、录井及测井等资料,对饶阳凹陷南马庄地区西 6 区块沙 一上段单砂体沉积微相进行刻画,并对各类微相中砂体含油气性进 行分析,基于各小层沉积微相与含油层的结合,剖析了沙一上段沉 积微相与油气分布关系,指出油气聚集的有利相带,为饶阳凹陷的 油气增储上产提供了理论支持。
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关键词 : 饶阳凹陷;西 6 区块;沙一上段;沉积微相;含油气性;油气聚集有利区
Abstract

The Raoyang sag is an old exploration area and the annual oil and gas production is decreasing each year. It is urgent  to find new oil and gas reserves to meet the needs of national strategic development. Limited by the early production technology  

and the theoretical model, the stratigraphic framework is roughly divided, and the evaluation target is mainly concentrated on the   member or sub-member level, and the oil group is the main one with higher accuracy. Single sand body scale reservoirs are affected by  heterogeneity, which leads to the inaccurate division of sedimentary microfacies, which brings challenges to the increase of reserves and   production, and seriously restricts the development of oil and gas exploration and development. Based on this, using the core, logging,   and logging data, this paper takes the Xi-6 block in the Nanmazhuang area of the Raoyang sag as an example to characterize the sedi mentary microfacies of each small layer (single sand body) in the upper member of Es1, and analyzes the oil and gas bearing properties   of sand bodies in various microfacies. The results show that the upper SHA-1 member of block Xi-6 is divided into 3 oil formations   and 9 sub-layers; the lithology is mainly composed of mudstone from a partially oxidizing environment and sandstone from a partially   reducing environment, which is characterized by water oscillation during deposition; the type of sedimentary subfacies is delta plain   with three microfacies: distributary channel, natural dike, and river swamp; the distribution range of sedimentary microfacies controls   the distribution characteristics of sand bodies, specifically, the distributary channel controls the ratio of sand and sand infiltration   thickness distribution of the sublayer, among which the ratio of sand of sublayer II1 and II2 is the largest, up to 0.75 and 0.85, and the  sand infiltration thickness of sublayer I and II1 is the largest, up to 30 m and 25 m. Under the control of distributary channel microfacies  
of each small layer in oil group III, the overall oil-bearing property of reservoir sand bodies is relatively high, and the largest proportion  of oil-bearing layers in II4 and III2 is 69.6 % and 65.5 % . Based on the combination of sedimentary microfacies and oil-bearing layers,   the relationship between sedimentary microfacies and oil-gas distribution in the upper Es1 member is analyzed, and it is pointed out   that the favorable oil-gas accumulation area is where the thickness of permeable sand in the superimposed area of microfacies such as   distributary channels and natural dikes is more than 5 m.


Key words: Raoyang sag; Xi-6 area; upper member of Es1; sedimentary microfacies; oil/gas bearing ability; favorable area for oil/gas accumulation
收稿日期: 2021-12-29     
PACS:    
基金资助:中国石油天然气股份有限公司科技重大专项“富油气区带整体再评价关键技术攻关研究与应用”(2017E-1504) 资助
通讯作者: panghong19820107@126.com
引用本文:   
LYU Chuanbing, PANG Xiongqi, PANG Hong, FU Liangliang, ZHENG Dingye, LIU Benfen, GENG Rongyan. Sedimentary microfacies and oil/gas-bearing ability of the upper member of Es1 in the Xi-6 area, Raoyang sag. Petroleum Science Bulletin, 2021, 04: 553-565. doi: 10.3969/j.issn.2096-1693.2021.04.038
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