Analysis of Sedimentary Environment and Ascertainment of Carboniferous-Permian Lithostratigraphic Unit in South Area of Beishan, Xinjiang

XIAO Pei-xi; HUANG Yu-hua; WANG Yu-xi; WANG Xing-an; WANG Shen-qin

Northwestern Geology > 2006 > 39(1): 76-82.

XIAO Pei-xi, HUANG Yu-hua, WANG Yu-xi, et al. Analysis of Sedimentary Environment and Ascertainment of Carboniferous-Permian Lithostratigraphic Unit in South Area of Beishan, Xinjiang[J]. Northwestern Geology, 2006, 39(1): 76-82.

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Analysis of Sedimentary Environment and Ascertainment of Carboniferous-Permian Lithostratigraphic Unit in South Area of Beishan, Xinjiang

1.
Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China
2.
Geology and Mineral Bureau of Shaanxi, Xi'an 710054, China

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Received Date: October 20, 2005
Revised Date: December 16, 2005
Published Date: March 04, 2006

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Abstract

Abstract

Carboniferous-Permian strata distribute widely in south area of Beishan,Xinjiang,which is a suit of slight alterative and strong deformation rock in the mass.The lithostratigraphic unit from old to youth by ascertainment over again as follow:Early Carboniferous Hongliuyuan Formation,Late Carboniferous Shibanshan Formation,Shengliquan Formation and Ganquan Formation,Early Permian Hongliuhe Formation,Middle Permian Luotuogou Formation.Their sedimentary environments go through from seashore facies to alternant sea-and-land facies.They are two quite integrated sedimen tary gyration.The color of the sediment is that the mauve in serts the grayish green and the source piece in the land is the quartz and feld spar for low maturity,which displayed the deposit characteristic of oxidation,anea rsourse and celerity,reflected the basin nature of the rift valley in the land.
- Beishan area of Xinjiang,
- Carboniferous-Permian,
- lithostratigraphic unit,
- sedimentary environment

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Analysis of Sedimentary Environment and Ascertainment of Carboniferous-Permian Lithostratigraphic Unit in South Area of Beishan, Xinjiang

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