济阳坳陷及鲁西隆起区中、新生代伸展与断裂活动特征

doi:10.11743/ogg20080117

Abstract

Abstract:

Jiyang depression and Luxi uplift share the same type of crystalline basement.Three typical deep seismic reflection profiles acquired in these two regions during recent years were used to reconstruct the depositional burial history of the basin.By repeatedly matching the tectonic features of the basin,kinematic parameters during each main tectonic evolution stage were quantitatively calculated and the extensional process of the basement was analyzed in detail.The results show that both basement extension and fault activity are in temporal and spatial non-equilibrium in Jiyang depression and Luxi uplift,and the intensity of extensional deformation during Paleogene is much stronger than that during the Mesozoic for both of the regions.For Jiyang depression,both the ratio and rate of the Paleogene extension in N-S direction are two times bigger than those in E-W direction.This article provides an important basis for the further study of the tectonic evolution and crustal extensional deformation of the Great North China in Eastern China during the Meso-Cenozoic.

Key words: basement extension, fault activity, Jiyang Depression, Luxi Uplift

CLC Number:

TE121.2

Ding Zengyong, Wang Liangshu, Zhang Peng, Zhong Kai, Liu Shaowen. Crustal extension and fault activity during the Mesozoic-Cenozoic in the Jiyang Depression and the Luxi Uplift,East China[J]. Oil & Gas Geology, 2008, 29(1): 107-112,140.

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Crustal extension and fault activity during the Mesozoic-Cenozoic in the Jiyang Depression and the Luxi Uplift,East China

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