吐哈盆地鄯善弧形带三间房组二段重矿物物源分析

doi:10.3969/j.issn.1673-8926.2014.06.006

Lithologic Reservoirs ›› 2014, Vol. 26 ›› Issue (6): 34-39.doi: 10.3969/j.issn.1673-8926.2014.06.006

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Provenance analysis of heavy minerals of the second member of Sanjianfang Formation in Shanshan arcuate belt, Tuha Basin

ZHANG Jingqi¹^，²， HAN Xiaofeng³， YANG Zhanlong²

1. College of Geosciences ， China University of Petroleum ， Beijing 102249 ， China ； 2. PetroChina Research Institute of Petroleum Exploration & Development-Northwest ， Lanzhou 730020 ， China ； 3. Xi ’ an Center of Geological Survey ， China Geological Survey ， Xi ’ an 710054 ， China

Online:2014-11-20 Published:2014-11-20

Abstract

Abstract:

Based on the analyses of correlation, factor, Q type cluster, stability coefficient, plane assemblage features and paleogeomorphology, this paper studied the heavy mineral components of the second member of Sanjianfang Formation in Shanshan arcuate belt. The result shows that the source rock types are mainly sedimentary rock and metamorphic rock, which respectively responds to the primary provenance in Takequan uplift in the north and the secondary provenance in Liaodun uplift in the southeast. The provenance in Takequan uplift controls the sedimentation of braided delta fan in hill country, and the provenance in Liaodun uplift controls the sedimentation of braided delta fan in Wenjisang area. The eastern hill country is the intersection of Takequan uplift provenance and Liaodun uplift provenance.

Key words: pore evolution , diagenesis , reservoir properties , YanchangFormation , Qilicun Oilfield , Ordos Basin

ZHANG Jingqi， HAN Xiaofeng， YANG Zhanlong. Provenance analysis of heavy minerals of the second member of Sanjianfang Formation in Shanshan arcuate belt, Tuha Basin[J].Lithologic Reservoirs, 2014, 26(6): 34-39.

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/ / Recommend heavy mineral； provenance analysis； Shanshan arcuate belt； Tuha Basin
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