Characteristics of sedimentary microfacies of Upper Triassic Chang 6 reservoir in Weibei area of Ordos Basin

LI Qingzhong

doi:10.3969/j.issn.1673-8926.2008.03.014

Lithologic Reservoirs >

2008 , Vol. 20 >Issue 3: 69 - 73

DOI: https://doi.org/10.3969/j.issn.1673-8926.2008.03.014

Characteristics of sedimentary microfacies of Upper Triassic Chang 6 reservoir in Weibei area of Ordos Basin

LI Qingzhong

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(1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China; 2. State Key Laboratory ofOil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China

Online published: 2008-09-15

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Abstract

Chang 6 reservoir of Yanchang Formation in Weibei area is mainly composed of gray fine sandstone and siltstone. Based on core observation, single well facies and logging data analysis, the characteristics of sedimentary microfacies and the distribution ofmicrofacies in each sublayer ofUpper Jurassic are systematically studied. The results show that braided river delta front and turbidite are the main deposits in Chang 6 reservoir in Weibei area. The subaqueous distributary channel, mouth bar, distal bar, sand sheet and interdistributary bay are the main sedimentary microfacies of the braided river delta front. The study results settle a strong base for the prediction of favorable reservoir facies belts and the further exploration.

Key words： sand shale interbed’ seismic exploration’ vertical resolution’ model’ lithologic reservoirs

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LI Qingzhong . Characteristics of sedimentary microfacies of Upper Triassic Chang 6 reservoir in Weibei area of Ordos Basin[J]. Lithologic Reservoirs, 2008 , 20(3) : 69 -73 . DOI: 10.3969/j.issn.1673-8926.2008.03.014

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