Strong earthquake recurrence interval in the southern segment of the Red River Fault, southwestern China

Along the southeastern margin of the Tibetan Plateau, an important boundary fault, known as the Red River Fault (RRF), formed during the extrusion of mantle and lower crustal materials beneath the Tibetan Plateau. The characteristics of RRF activity are important for understanding the tectonic evolu...

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Bibliographic Details
Main Authors: Qingyun Zhou, Xi Li, Yuqiao Chang, Jiang Yu, Weidong Luo, Xianfu Bai
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-12-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2023.1280787/full