Wedge‐Shaped Southern Indian Continental Margin Without Proper Weakness Hinders Subduction Initiation

Abstract The closure of a subduction zone with continental terrane collision and accretion is generally thought to be followed by the initiation of a new subduction zone in the neighboring oceanic plate, which is suggested to happen repeatedly during the evolution of Tethyan system. Although the Ind...

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Bibliographic Details
Main Authors: Xinyi Zhong, Zhong‐Hai Li
Format: Article
Language:English
Published: Wiley 2022-02-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2021GC009998