Late Holocene slip rate and average recurrence interval of great earthquakes on the Shangzhi segment of the Yilan-Yitong Fault Zone, northeastern China: Constraints from paleo-earthquakes and historical written records-Reference-Cited by-同舟云学术

Late Holocene slip rate and average recurrence interval of great earthquakes on the Shangzhi segment of the Yilan-Yitong Fault Zone, northeastern China: Constraints from paleo-earthquakes and historical written records

Published:2017-11-15 Issue:1 Volume:27 Page:e12231
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

Yu Zhongyuan¹²³^ORCID,Zhang Peizhen⁴,Min Wei²,Wei Qinghai³,Liu Yugang²

Affiliation:

1. Department of Earthquake Science; Institute of Disaster Prevention, Yanjiao Development Zone; Langfang 065201 China

2. Key Laboratory of Active Tectonics and Volcano, Institute of Geology; China Earthquake Administration; Beijing 100029 China

3. Earthquake Administration of Heilongjiang Province; Harbin 150090 China

4. School of Earth Science and Geologic Engineering; Sun Yan-Sen University; Guangzhou 510275 China

Funder

Spark Program of Earthquake Sciences, China Earthquake Administration

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/iar.12231/fullpdf

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3. Structural architecture and tectonic evolution of the Fangzheng sedimentary Basin (NE China), and implications for the kinematics of the Tan-Lu fault zone;Chen;Journal of Asian Earth Science,2015

4. Wrench-related folding: A case study of Bohai Sea Basin, China;Chen;Marine and Petroleum Geology,2010

5. Seismogenic strike-slip faulting and the development of the North China Basin;Chen;Tectonics,1988

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