蒙古国东方省海塔盆地塔南凹陷断裂特征及其油气意义

doi:10.7605/gdlxb.2013.04.043

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Abstract Based on structural geometry data compiled by interpretation of 3D seismic data in Tanan Sag of Haita Basin，the faults characteristics and evolution，and their controls on sedimentation and hydrocarbon source rocks，trap，and accumulation were analyzed in this paper.It is found that the Tanan Sag had gone through three big basin historical periods，that is，composite faulted stage(K_1t-K_1n)，the composite fault-depression transition stage(K1d)and reverse depression stage(K_1y-K_2q)，and normal fault system and strike-slip normal fault system formed during the Cretaceous.Affected by faults movement，the subsidence centers in sub-sag were differentiated and migrated distinctly in different stages.The subsidence center distributed along the hanging wall of the boundary faults during the composite faulted stage，and moved to the center of the sag during the composite fault-depression transition stage.The strength and style of the faults controlled the distribution of sedimentary facies and hydrocarbon accumulation conditions.

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	Articles by authors
	Chen Weichang
	Qi Jiafu
	Jiang Hongfu
	Liu Xue
	Sun Jiahua
	Xin Shiwei

Key words： Mongolia Haita Basin Tanan Sag fault structure tectonic evolution Cretaceous

Received: 30 July 2012 Published: 01 August 2013

ZTFLH:

TE121.2

Corresponding Authors: Qi Jiafu，born in 1957，is a professor of China University of Petroleum(Beijing)，and is mainly engaged in researches of oil structure analysis and petroliferous basin analysis. Email: qijiafu@cup.edu.cn

About author: Chen Weichang，born in 1983，is a Ph.D.candidate of China University of Petroleum(Beijing)，and is mainly engaged in research of oil structure analysis. E-mail: chenwc1983@163.com

Cite this article:

Chen Weichang,Qi Jiafu,Jiang Hongfu et al. Characteristics of fault structure in Tanan Sag, Haita Basin in Dornod Aymag, Mongolia and its hydrocarbon significance[J]. JOPC, 2013, 15(4): 539-550.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2013.04.043 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2013/V15/I4/539

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