Typical Soft–Sediment Deformation Structures Induced by Freeze/Thaw Cycles: A Case Study of Quaternary Alluvial Deposits in the Northern Qiangtang Basin, Tibetan Plateau-Reference-Cited by-同舟云学术

Typical Soft–Sediment Deformation Structures Induced by Freeze/Thaw Cycles: A Case Study of Quaternary Alluvial Deposits in the Northern Qiangtang Basin, Tibetan Plateau

Published:2020-02 Issue:1 Volume:94 Page:176-188
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica ‐ English Edition

Author:

ZHONG Ning¹²³,LI Haibing¹²,JIANG Hanchao⁴,LU Haijian¹²,ZHENG Yong¹²,HAN Shuai¹²,YE Jiachan¹²

Affiliation:

1. Key Laboratory of Deep–Earth DynamicsMinistry of Natural Resources Beijing 100037 China

2. Institute of GeologyChinese Academy of Geological Sciences Beijing 100037 China

3. Institute of GeomechanicsChinese Academy of Geological Sciences Beijing 100081 China

4. State Key Laboratory of Earthquake DynamicsInstitute of Geology, China Earthquake Administration Beijing 100029 China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14345

Reference86 articles.

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3. Soft-sediment deformation within seismogenic slumps of the Dead Sea Basin

4. Coversand and Pleistocene palaeosols in the Landes region, southwestern France

5. Hydraulic conductivity in frozen soils

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