Two‐stage Cenozoic evolution of NW–SE‐trending faults in the coastal area of southeast China controlled the fan‐shaped Zhangzhou basin-Reference-Cited by-同舟云学术

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Two‐stage Cenozoic evolution of NW–SE‐trending faults in the coastal area of southeast China controlled the fan‐shaped Zhangzhou basin

Published:2019-07-15 Issue:5 Volume:31 Page:445-457
ISSN:0954-4879
Container-title:Terra Nova
language:en
Short-container-title:Terra Nova

Author:

Chen Wei¹²^ORCID,Hu Xiangyun¹,Zhuang Qingxiang²,Chen Qi³

Affiliation:

1. Institute of Geophysics & Geomatics China University of Geosciences Wuhan China

2. Fujian Xianghe Geothermal Development Co., Ltd. Zhangzhou China

3. Three Gorges Geotechnical Consultants Co., Ltd. Wuhan China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12414

Reference43 articles.

1. Aki K. &Richards P. G.(1980).Quantitative Seismology 1980. WR Freeman and Co.

2. Correction of common lead in U–Pb analyses that do not report 204Pb

3. Bi F. Yuan Y. &Fang G.(1990).The latest NWW‐trending tectonic zones and tectonic background of large earthquake in Fujian‐Guangdong‐Taiwan coastal area. Seismology and Geology 2.

4. Study of active rift in Zhangzhou‐Longhai area, Fujian Province;Chen Y.;South China Journal of Seismology,1988

5. Discussion on neotectonic movement in Zhangzhou basin, Fujian Province;Chen Y.;South China Journal of Seismology,1987

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