裂陷盆地构造演化及盆地伸展模式—以东濮凹陷为例

doi:10.11743/ogg20060112

Abstract

Abstract:

Dongpu depression is a typical rifted basin in eastern China. The tectonic evolution of the basin includes an Early Paleozoic-Triassic cratonic basin cycle and a Cenozoic rift basin cycle. The latter can be subdivided into 4 stages, including initial rifting, intense rifting, late rifting and Late Tertiary integral downwar-ping. The basement extension in Dongpu depression increases, as a whole, from north to south. The extensional tectonic deformation is of simple shear extensional pattern in the upper earth crust, and of pure shear extensional pattern in the lower earth crust. The mutation zone of detachment surface might be the main factor causing the lateral tectonic transformation belt from Sangcunji to Qiaokou to Baimiao, and the difference of tectonic activity and the enrichment of oil and gas in the northern and southern parts of Dongpu depression.

Key words: extension, extensional pattern, tectonic evolution, rifted basin, Dongpu depression

CLC Number:

TE111.1

Su Hui, Qu Liping, Zhang Jinchuan, Wang Pingxia, He Feng, Wang Min, Wang Qi, Hu Yujie. Tectonic evolution and extensional pattern of rifted basin:a case study of Dongpu depression[J]. Oil & Gas Geology, 2006, 27(1): 70-77.

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Tectonic evolution and extensional pattern of rifted basin:a case study of Dongpu depression

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