塔里木盆地中奥陶世一间房组沉积时期构造-沉积环境与原型盆地特征<sup>*</sup>

doi:10.7605/gdlxb.2016.06.075

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Abstract Proto-type basin analysis is of great use to uncover the tectonics-lithofacies palaeogeography and restore the basin-mountain coupling process and is of great significance for the guiding of petroleum exploration. Based on the newest data of drillings,seismic profiles and outcrops,with the analysis of sedimentary facies and the combination of basins and orogenic belts,this paper reconstructed tectonic-depositional environment during the depositional period of Middle Ordovician Yijianfang Formation in Tarim Basin and analyzed the features and properties of the basin,by employing the method of “point → line → planar”. During the depositional period of Yijianfang Formation,the Bachu-Tazhong and Tangnan intra-platform uplifts were the denuded zones;low-energy micrite facies were developed in the Shunnan-Tanggubasi-Yudong intra-platform sag;carbonate shoals facies were widely distributed in the Tabei and Gucheng platforms;deep-water nodular limestone and black shale facies were developed in the Kalpin intra-platform basin;the Tadong deep water basin transformed from black shale facies to terrigenous clastic turbidite facies and open platform facies were developed in Kuruktag-Luoxi area. The tectonic-depositional pattern of the Tarim Basin had the interim transition feature from the platform-basin pattern of the Early Ordovician to the uplift-depression pattern of the Late Ordovician,behaving as the palaeogeography differentiation of the Taxi platform and the reversal of the sedimentary properties of the Tadong deep water basin. We suggested that the Tarim Basin had a composite property of intracratonic and craton-margin depressions during the depositional period of Yijianfang Formation,yet overlapped by the foreland basin(Tangnan forbulge and Shunnan-Tanggubasi-Yudong back-bulge)at the southern part of the Taxi intracratonic depression and the extension basin(Kalpin craton-margin extension basin)at the northwestern part of the Taxi intracratonic depression. The tectonic-depositional environment and proto-type basin during the depositional period of Middle Ordovician Yijianfang Formation in Tarim Basin was a response to peripheral tectonic movements.

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	Gao Huahua
	He Dengfa
	Tong Xiaoguang
	Wen Zhixin
	Wang Zhaoming
	He Jinyou

Key words： proto-type basin tectonic-depositional environment Yijianfang Formation Ordovician Tarim Basin

Received: 12 June 2016 Published: 01 December 2016

ZTFLH:

P618.3

Fund:[Co-funded by the National Program on Key Basic Research Project(No.2011CB201101), National Science and Technology Major Project (No. 2016ZX05029)and Geological Survey Project of China Geological Survey(No.1212011220761)]

Corresponding Authors: He Dengfa,born in 1967,is a professor of China University of Geosciences(Beijing). He is mainly engaged in basin structure. E-mail: hedengfa282@263.net.

About author: Gao Huahua,born in 1989,is a Ph.D. candidate. He is engaged in basin structure and petroleum geology. E-mail: gaohuacugb@126.com.

Cite this article:

Gao Huahua,He Dengfa,Tong Xiaoguang et al. Tectonic-depositional environment and proto-type basins during the depositional period of Middle Ordovician Yijianfang Formation in Tarim Basin[J]. JOPC, 2016, 18(6): 986-1001.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2016.06.075 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2016/V18/I6/986

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