引用本文:孟元库, 汪新文, 陈杰, 黄鹂.埕海油田张东地区沙河街组沉积特征分析[J].沉积与特提斯地质,2015,(2):45-53.[点击复制]
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埕海油田张东地区沙河街组沉积特征分析
孟元库,汪新文,陈杰,黄鹂
0
(1. 中国地质科学院地质研究所 大陆构造与动力学国家重点实验室, 北京 100037;
2. 中国地质大学 地球科学与资源学院, 北京 100083;
3. 山东省第八地质矿产勘查院, 山东 日照 276826)
摘要:
本文通过粒度、岩性、沉积构造、测井曲线以及沉积微相平面图等资料的综合分析,结合区域地质背景,对埕海油田张东地区沙河街组沙三段、沙二段、沙一段进行了详细的划分、描述。研究区沙三段沉积呈典型的正粒序结构,上细下粗,为三角洲前缘亚相,主要砂体类型包括河口坝、水下分流河道及前缘席状砂。储层特征表现为中孔-中渗、中孔-低渗、低孔-特低渗,孔隙以粒间、颗粒和粒内溶孔为主,于晚成岩A阶段形成;沙二段形成于三角洲沉积环境(滨浅湖),属于低位体系域,砂体发育,规模大,为张东地区最为有利的储集层,是今后勘探的重点靶区;沙一段主要为白云岩、泥灰岩、和油页岩的互层沉积,局部地区发育薄层粉砂岩,可以作为很好的盖层和烃源岩,沉积环境为比较闭塞的静水澙湖环境。
关键词:  张东地区  沙河街组  沉积特征  砂体类型
DOI:
附件
投稿时间:2014-04-10修订日期:2014-04-16
基金项目:国家自然科学基金委创新群体项目(40921001)资助
Sedimentary characteristics of the Shahejie Formation in the Zhangdong district, Chenghai Oil Field, Hebei
MENG Yuan-ku, WANG Xin-wen, CHEN Jie, HUANG Li
(1. State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;
2. School of Geosciences and Resources, China University of Geosciences, Beijing 100083, China;
3. No.8 Research Institute of Geology and Mineral Resources of Shandong, Rizhao 276826, Shandong, China)
Abstract:
The Zhangdong district, Chenghai Oil Field, Hebei is very complicated in geological structures and thus less explored in petroleum exploration. The authors in the present paper give a detailed division and description for the Shahejie Formation as main oil-bearing rock series in the Zhangdong district on the basis of grain sizes, lithology, sedimentary structures, sedimentary microfacies and well logs. The third member of the Shahejie Formation displays the typical normal graded structures, and belongs to the delta front subfacies including the channel mouth bar, subaqueous distributary channel and delta front sheet sands microfacies. The sandstone reservoirs are characterized by moderate porosity to moderate permeability, moderate porosity to low permeability, low porosity to extra-low permeability, and intergranular, granular and intragranular solution openings generated during the A stage of late diagenesis. The second member of the Shahejie Formation is organized in the delta (littoral to shallow-lake)environment in the lowstand tracts system, and occurs as the best favourable hydrocarbon reservoirs and target area in the Zhangdong district. The first member of the Shahejie Formation is built up of the dolostone-marl-oil shale couplets, locally with thin-bedded siltstones as good cap rocks and source rocks deposited in the relatively enclosed stationary lagoon environment.
Key words:  Zhangdong district  Shahejie Formation  sedimentary characteristics  sandstone type

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