Volume 94, Issue 1 pp. 176-188
Original Article
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Typical Soft–Sediment Deformation Structures Induced by Freeze/Thaw Cycles: A Case Study of Quaternary Alluvial Deposits in the Northern Qiangtang Basin, Tibetan Plateau

Ning ZHONG

Ning ZHONG

Key Laboratory of Deep–Earth Dynamics, Ministry of Natural Resources, Beijing, 100037 China

Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037 China

Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081 China

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Haibing LI

Corresponding Author

Haibing LI

Key Laboratory of Deep–Earth Dynamics, Ministry of Natural Resources, Beijing, 100037 China

Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037 China

Corresponding author. E-mail: [email protected]Search for more papers by this author
Hanchao JIANG

Hanchao JIANG

State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing, 100029 China

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Haijian LU

Haijian LU

Key Laboratory of Deep–Earth Dynamics, Ministry of Natural Resources, Beijing, 100037 China

Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037 China

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Yong ZHENG

Yong ZHENG

Key Laboratory of Deep–Earth Dynamics, Ministry of Natural Resources, Beijing, 100037 China

Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037 China

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Shuai HAN

Shuai HAN

Key Laboratory of Deep–Earth Dynamics, Ministry of Natural Resources, Beijing, 100037 China

Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037 China

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Jiachan YE

Jiachan YE

Key Laboratory of Deep–Earth Dynamics, Ministry of Natural Resources, Beijing, 100037 China

Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037 China

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First published: 22 July 2019
Citations: 14

About the first author:

ZHONG Ning, male, born in 1986 in Henan Province; Graduated from Institute of Geology, China Earthquake Administration. Doctor ZHONG Ning is currently a postdoctor at the Institute of Geology, Chinese Academy of Geological Science. His current research interest focuses on the Active tectonics, paleoearthquake and Soft–sediment Deformational Structures. Email: [email protected]; phone: 010-68990581.

About the corresponding author:

LI Haibing, male, born in 1966 in Anhui Province; doctor; graduated from Institute of Geology, Chinese Academy of Geological Sciences. He is now interested in the study on tectonic geomorphology and paleoearthquake. Email: [email protected]; phone: 010-68990581.

Abstract

With the objective of establishing a distinction between deformation structures caused by freeze/thaw cycles and those resulting from seismic activity, we studied three well–exposed alluvial deposits in a section at Dogai Coring, northern Qiangtang Basin, Tibetan Plateau. Deformation is present in the form of plastic structures (diapirs, folds and clastic dykes), brittle structures (micro–faults) and cryogenic wedges. These soft–sediment deformation features (except the micro–faults) are mainly characterized by meter–scale, non–interlayered, low–speed and low–pressure displacements within soft sediments, most commonly in the form of plastic deformation. Taking into account the geographic setting, lithology and deformation features, we interpret these soft–sediment deformation features as the products of freeze/thaw cycles, rather than of earthquake–induced shock waves, thus reflecting regional temperature changes and fluctuations of hydrothermal conditions in the uppermost sediments. The micro–faults (close to linear hot springs) are ascribed to regional fault activity; however, we were unable to identify the nature of the micro–faults, perhaps due to disturbance by subsequent freeze/thaw cycles. This study may serve as a guide to recognizing the differences between deformation structures attributed to freeze/thaw cycles and seismic processes.

 

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