上扬子地区震旦纪沉积古地理

doi:10.7605/gdlxb.2015.06.061

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Abstract

Based on the analysis of wells,loggings,seismic information and other materials of synthetic study,palaeogeography of different formations or members of the Sinian in Upper Yangtze Region was mapped,sedimentation and reservoirs were systematically studied. It indicated that the Upper Yangtze Platform was a semi-platform during the Sinian,and the process of sedimentation could be divided into three stages of pre-platform deposition,carbonate platform deposition and restricted sea basin deposition. The Chuan-Dian great rift adjoining to the western margin of the Upper Yangtze Platform played an important role in the platform evolution,formation of sedimentary palaeogeography framework and facies distribution of the Upper Yangtze Region. During the period of the Upper Sinian Dengying Formation,the Upper Yangtze Platform had ever undergone a fast subsidence caused by rifting,going through an ephemeral change from platform to basin. The evolution of the lithofacies palaeogeography controlled the formation and distribution of reservoirs of the Sinian in Sichuan Basin,and also controlled the formation and distribution of conventional petroleum and shale gas in this region.

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	Articles by authors
	Liu Jingjiang
	Li Wei
	Zhang Baomin
	Zhou Hui
	Yuan Xiaohong
	Shan Xiuqin
	Zhang Jing
	Deng Shenghui
	Gu Zhidong
	Fan Ru
	Wang Yongjun
	Li Xin

Key words： Upper Yangtze Platform Sinian palaeogeography semi-platform carbonate platform Panxi Rift lime mud mound restricted sea basin

Received: 05 June 2015 Published: 01 December 2015

ZTFLH:

P531

About author: Liu Jingjiang,born in 1968,obtained his Ph.D. degree from Northwest University in 2010. He is mainly engaged in the study of carbonate sedimentary reservoir and reservoir evaluation. E-mail: liujj6@petroChina.com.cn

Cite this article:

Liu Jingjiang,Li Wei,Zhang Baomin et al. Sedimentary palaeogeography of the Sinianin Upper Yangtze Region[J]. JOPC, 2015, 17(6): 735-754.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2015.06.061 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2015/V17/I6/735

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