EVOLUTION OF SEDIMENTARY ENVIRONMENT IN THE NORTH HETAO BASIN SINCE 344 Ka

CAI Maotang; YE Peisheng; YANG Xingchen; ZHANG Xujiao; LI Chenglu; ZHOU Wei; LU Jing; WANG Tao

doi:10.12090/j.issn.1006-6616.2018.24.02.027

Volume 24 Issue 2

Apr. 2018

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CAI Maotang, YE Peisheng, YANG Xingchen, et al., 2018. EVOLUTION OF SEDIMENTARY ENVIRONMENT IN THE NORTH HETAO BASIN SINCE 344 Ka. Journal of Geomechanics, 24 (2): 253-262. DOI: 10.12090/j.issn.1006-6616.2018.24.02.027

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EVOLUTION OF SEDIMENTARY ENVIRONMENT IN THE NORTH HETAO BASIN SINCE 344 Ka

doi: 10.12090/j.issn.1006-6616.2018.24.02.027

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

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Received: 2017-09-10
Revised: 2018-01-08
Published: 2018-04-01

Abstract

Abstract

Through analysis of sedimentary facies and grain size characteristics from 377 m drilling cores in the north Hetao Basin, combined with different dating methods, the evolution of sedimentary environment in the north Hetao Basin since late Middle Pleistocene is revealed. According to the characteristics of grain size parameters, sedimentary environment can be divided into 6 stages:lakeshore (344~326 ka)-semi-deep lake (326~165 ka)-lakeshore delta (165~130 ka) -shallow lake (130~100 ka)-lakeshore-fluvial (100~10 ka)-washland (10 ka~now). Comprehensive research shows that a unified paleo-megalake has been existed in the Hetao Basin from middle Pleistocene to late Pleistocene. After late Pleistocene, the paleo-megalake disintegrated and disappeared.
- grain size,
- sedimentary environment,
- paleolake evolution,
- the Hetao Basin

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EVOLUTION OF SEDIMENTARY ENVIRONMENT IN THE NORTH HETAO BASIN SINCE 344 Ka

doi: 10.12090/j.issn.1006-6616.2018.24.02.027

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EVOLUTION OF SEDIMENTARY ENVIRONMENT IN THE NORTH HETAO BASIN SINCE 344 Ka

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