东营凹陷古近纪控盆断层演化特征及盆地结构类型

doi:10.11743/ogg20080302

Abstract

Abstract:

The shape of the Palaeogene basin-controlling faults of Dongying sag had evolved from planar in the early period(basically corresponding to the deposition of the Kongdian Formation),to listric in the middle period(deposition of the fourth member to the Lower third member of Shahejie Formation),and finally to slope-flat in the late period(deposition of the second member of Shahejie Formation to Dongying Formation).The intensity of basin-controlling fault activity in Dongying sag shows a left-lateral feature.The spatial distribution of deposits is basically consistent with the strike of main faults in different evolutionary stages of the Palaeogene rifted basin.The fault activities controlled the sedimentary process.Corresponding with the evolution of boundary faults,the Palaeogene basin in Dongying sag had gone through the early rotation half-graben,middle rolling half-graben,and late compound half-graben.

Key words: basin architecture, structural evolution, basin-controlling fault, Palaeogene, Dongying Sag

CLC Number:

TE121.2

Sheng Wenbo, Cao Yingchang, Liu Hui, Zhang Yu. Evolutionary characteristics of the Palaeogene basin-controlling boundary faults and types of basin architectures in the Dongying Sag[J]. Oil & Gas Geology, 2008, 29(3): 290-296,289.

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Evolutionary characteristics of the Palaeogene basin-controlling boundary faults and types of basin architectures in the Dongying Sag

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