蔺毓秀
Lin Yuxiu(The Oil and Gas Reservoir Comprehensive Research Department ofthe Scientific Research and Design Institute of Daqing Oil Field);

• 1:大庆油田科学研究设计院综合室

摘要(Abstract)：

本文通过分析姚一段北安-杏树岗三角洲，提出湖进三角洲的概念，其沉积层序为三层结构的正旋回组合，在湖进过程中，三角洲体随湖岸线向陆地方向迁移，层位由老变新。湖进三角洲的骨架砂体呈指状展布，砂体的分布模式是：河口堆积砂体——水下分流河道条带砂体——分流间透镜砂体——席状砂体，而主骨架砂体是分流条带砂体。
Abstract By analyzing the delta of Beian-Xingshugang formed in member 1 of Yaojia formation, the concept of lacustrine progressive delta, in which its depositional sequence was positive cycle combination with three layers structure, is proposed. During the progress of the lake, the body of the delta was shifted landward with the lake shoreline, and the horizons were changed from old to new. The matrix sandbodies in the lacustrine progressive delta arc distributed as fingers. The distributive model of the sandbodies is river mouth accumulational sandbody-subaqueous distributary channel elongated sandbody-intcrdistributary lenticular sandbody-sheet sandbody. But the main matrix sandbody is distributary elongated sandbody.

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Abstract:

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作者(Authors): 蔺毓秀
Lin Yuxiu(The Oil and Gas Reservoir Comprehensive Research Department ofthe Scientific Research and Design Institute of Daqing Oil Field);

DOI: 10.19597/j.issn.1000-3754.1983.02.004

参考文献(References)：

• 〔1〕陈景山、陈昌明译：《三角洲沉积与油气勘探》，石油工业出版社，1981年
• 〔2〕陈昌明、李继亮译：《陆源碎屑沉积环境》，石油工业出版社，1979年
• 〔3〕F．J．佩蒂庄等：《砂和砂岩》，科学出版社，1977年
• 〔4〕陕西省水利科学研究所河渠研究室、清华大学水利工程系泥沙研究室合编：《水库泥沙》，水利电力出版社，1979年