Granulometric feature and depositional environment of Cretaceous period sandstone of Fenghuoshan basin in the Hoh Xil, Qinghai-Tibet plateau

SONG Zhong-bao; LI Wen-ming; LI Chang-an; LI Zhu-cang; LIU Zhi-yong; LIU Yong-cheng; LI Hong-pu; XUE Wan-wen

Northwestern Geology > 2004 > 37(2): 1-6.

SONG Zhong-bao, LI Wen-ming, LI Chang-an, et al. Granulometric feature and depositional environment of Cretaceous period sandstone of Fenghuoshan basin in the Hoh Xil, Qinghai-Tibet plateau[J]. Northwestern Geology, 2004, 37(2): 1-6.

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Granulometric feature and depositional environment of Cretaceous period sandstone of Fenghuoshan basin in the Hoh Xil, Qinghai-Tibet plateau

1.
Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China;Changan University, Xi'an 710054, China
2.
Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China
3.
Changan University, Xi'an 710054, China
4.
Geological Survey of Qinghai Province, Xining, 830000, China

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Received Date: June 17, 2003
Revised Date: February 16, 2004
Published Date: June 04, 2004

Graphical Abstract

Abstract

Abstract

By the granulometric analysis of Cretaceous period sand stone of Fenghuo shan basin,three probability cumulative curve,that delegated three sedimentary facies,eg.delta,river and lake have been divided. Not only have important geologic significance for research Fenghuo shan basin,but also have importan tactuality significance.
- Cretaceous period sand stone,
- granulometric analysis feature,
- depositional environment,
- Tibet plateau,
- Fenghuo shan basin

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Granulometric feature and depositional environment of Cretaceous period sandstone of Fenghuoshan basin in the Hoh Xil, Qinghai-Tibet plateau

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