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Sedimentary facies study for IV sand group of the second member of Qingshankou formation in Daqingzijing area

机译:大庆溪景地区青山沟地区第二次成员IV砂集团沉积相研究

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Sedimentary microfacies of IV sand group of the second member of Qingshankou formation in Daqingzijing area are interpreted jointly with careful core description, sequence and distribution of sandstone. The area also develops delta. Sedimentary microfacies shows that sand body size is becoming smaller and in the transgression period of IV sand groups of the second member of Qingshankou formation in the region. Sedimentary center has better properties, and the lateral margin of sand body is easy to form lithologic reservoir.
机译:大庆朱景地区青山沟地区第二成员沉积微面积,粉碎的核心描述,砂岩序列和分布,共同解释。该地区还开发了三角洲。沉积微缩醛表明,沙体尺寸变得越来越小,在该地区的第二次成员的IV砂组的迁移期。沉积中心具有更好的性质,砂体的横向缘易于形成岩性水库。

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