岩性油气藏 ›› 2017, Vol. 29 ›› Issue (2): 59–67.doi: 10.3969/j.issn.1673-8926.2017.02.008

• 油气地质 • 上一篇    下一篇

冀中坳陷饶阳凹陷浅水曲流河三角洲沉积体系——以赵皇庄—肃宁地区沙一段为例

朱茂1, 朱筱敏2, 曾洪流3, 董艳蕾2, 刘畅2, 郑荣华4   

  1. 1. 中国石油杭州地质研究院, 杭州 310023;
    2. 中国石油大学(北京)地球科学学院, 北京 102249;
    3. Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, Austin TX 78713-8924, USA;
    4. 中国石油华北油田分公司 勘探开发研究院, 河北 任丘 062552
  • 收稿日期:2016-11-18 修回日期:2016-12-18 出版日期:2017-03-21 发布日期:2017-03-21
  • 第一作者:朱茂(1988-),男,硕士,工程师,主要从事石油地质及地震沉积学方面的研究工作。地址:(310023)浙江省杭州市西湖区西溪路920号杭州地质研究院。Email:zhum_hz@petrochina.com.cn。
  • 基金资助:
    国家自然科学基金项目“陆相坳陷湖盆浅水三角洲地震沉积学模型”（编号：41272133）和华北油田校企合作项目“2012 年饶阳凹陷赵皇庄东-肃宁地区地震沉积学工业化应用研究”（编号：HBYT-2012-JS-188）联合资助

Depositional system of shallow-water meandering river delta:a case from the first member of Shahejie Formation in Zhaohuangzhuang-Suning area of Raoyang Sag, Jizhong Depression

ZHU Mao1, ZHU Xiaomin2, ZENG Hongliu3, DONG Yanlei2, LIU Chang2, ZHENG Ronghua4   

  1. 1. PetroChina Hangzhou Institute of Geology, Hangzhou 310023, China;
    2. College of Geosciences, China University of Petroleum(Beijing), Beijing 102249, China;
    3. Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, Austin TX 78713-8924, USA;
    4. Research Institute of Exploration and Development, PetroChina Huabei Oilfield Company, Renqiu 062552, Hebei, China
  • Received:2016-11-18 Revised:2016-12-18 Online:2017-03-21 Published:2017-03-21

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摘要： 冀中坳陷饶阳凹陷沙河街组沙一段是该区主要含油层系之一。为了落实沙一段砂体展布特征，明确该区下一步勘探方向，综合岩心、测井及三维地震等资料，开展饶阳凹陷赵皇庄—肃宁地区沙一段沉积体系研究。结果表明：沙一段沉积时期，赵皇庄—肃宁地区主要发育浅水曲流河三角洲，湖盆面积小，水体浅、能量弱，湖岸线迁移频繁；湖平面的周期振荡造成了岩性呈砂泥岩互层状、泥岩颜色为红黑相间的特征；浅水曲流河三角洲的水下分流河道极为发育，并且三角洲前缘分流河道易遭受不同程度的席状砂化，平面上呈网状分布。整体而言，沙一段发育的分流河道砂体平面分布广、纵横叠置，是有利的储集体。

Abstract: The first member of Shahejie Formation(Es1)is one of the main oil-bearing series in Raoyang Sag, Jizhong Depression. In order to define the reservoir distribution and exploration prospects,The sedimentary system of Es1 in Zhaohuangzhuang-Suning area of Raoyang Sag were studied based on the data of cores,logging and seismic. The results show that shallow-water meandering river delta is widely developed during the Es1 depositional stage,which is characterized by small lake basin,shallow water,low water energy and frequent migration of lake strandline. Periodic oscillation of lake level resulted in the interbeds of sandstone and mudstone,and the alternation of red and black mudstones. The sheeted net-shaped subaqueous distributary channel is well developed in the shallow-water meandering river delta. The distributary channel sandbodies are widely distributed and vertically superimposed. These features are favorable for reservoir space.

中图分类号: 

  • TE121.3
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