A TEST OF THE OBLIQUE-RIFTING MODEL FOR TRANSFER ZONE DEFORMATION IN THE NORTHERN FEN-WEI RIFT: IMPLICATIONS FROM THE 1989 M 6.1 DATONG-YANGGAO EARTHQUAKE SWARM

Tectonophysical experiments show that the evolution of the Fen-Wei Rift is controlled by oblique rifting. A key characteristic of the model in our study is that the western and eastern borders of the transfer zone between the adjacent NEE-striking extensional basins tend to form right-lateral strike...

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Principais autores:	Yan-Qun Zhuo, Yanshuang Guo, S. A. Bornyakov, Jin Ma
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2019-03-01
coleção:	Геодинамика и тектонофизика
Assuntos:	oblique rifting model current tectonic activity transfer zone focal mechanism solution earthquake relocation
Acesso em linha:	https://www.gt-crust.ru/jour/article/view/768
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