THE NEOTECTONIC RESTRICTS TO QUATERNARY DEPOSITION ENVIRONMENT EVOLUTION OF JIANGHAN BASIN

YANG Qing-xiong; TIAN Wang-xue; LI Qi-wen; KONG Ling-yao

Volume 22 Issue 3

Sep. 2016

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Article Navigation > Journal of Geomechanics > 2016 > 22(3): 631-641

YANG Qing-xiong, TIAN Wang-xue, LI Qi-wen, et al., 2016. THE NEOTECTONIC RESTRICTS TO QUATERNARY DEPOSITION ENVIRONMENT EVOLUTION OF JIANGHAN BASIN. Journal of Geomechanics, 22 (3): 631-641.

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YANG Qing-xiong, TIAN Wang-xue, LI Qi-wen, et al., 2016. THE NEOTECTONIC RESTRICTS TO QUATERNARY DEPOSITION ENVIRONMENT EVOLUTION OF JIANGHAN BASIN. Journal of Geomechanics, 22 (3): 631-641.

Citation:

YANG Qing-xiong, TIAN Wang-xue, LI Qi-wen, et al., 2016. THE NEOTECTONIC RESTRICTS TO QUATERNARY DEPOSITION ENVIRONMENT EVOLUTION OF JIANGHAN BASIN. Journal of Geomechanics, 22 (3): 631-641.

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THE NEOTECTONIC RESTRICTS TO QUATERNARY DEPOSITION ENVIRONMENT EVOLUTION OF JIANGHAN BASIN

Geological Survey of Hubei Province, Wuhan 430034, China

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Received: 2016-04-22
Published: 2016-09-01

Abstract

Abstract

Through the transverse contrast of Quaternary strata, combining with the data of outcrop profiles in periphery area of Jianghan Basin and Quaternary drilling cores in sedimentary central area, we restored the sedimentary environment of Jianghan Basin in different period of Quaternary, and discussed the neotectonic characteristics and its control functions to Quaternary sedimentary environment evolution. The result shows that most part of Jianghan Basin is in a lift condition in early and Middle Pleistocene, the periphery of the basin is in a state of erosion. The amount of crust exercise is unequal in late Pleistocene, from north west to south central the basin is slowly rising and sinking. In Holocene, rising in periphery of basin and undulating terrain and sinking in low plain area are more significant, and the area of the lake reached the maximum in middle and late Holocene.
- Jianghan Basin,
- neotectonics,
- Quaternary,
- sedimentary environment

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References(20)

References

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