Spatial Variations of Late Quaternary Slip Rates along the Ganzi–Xianshuihe Fault Zone in the Eastern Tibet

The Ganzi–Xianshuihe Fault Zone is a large-scale sinistral strike-slip fault zone on the eastern Tibet. As the boundary fault zone of the Bayankala Block and the Chuandian Block, it controls the clockwise rotation of the southeastern Tibet. However, there is still controversy regarding the activity...

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Autores principales:	Kai Sun, Chuanyou Li, Mingjian Liang, Xinnan Li, Quanxing Luo, Guangxue Ren, Feipeng Huang, Junjie Li
Formato:	Artigo
Lenguaje:	Inglês
Publicado:	MDPI AG 2024-07-01
Colección:	Remote Sensing
Materias:	Ganzi–Xianshuihe fault zone the eastern Tibet late quaternary slip rate consistent
Acceso en línea:	https://www.mdpi.com/2072-4292/16/14/2612
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