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...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Wiley
2022-02-01
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Series: | Geochemistry, Geophysics, Geosystems |
Subjects: | |
Online Access: | https://doi.org/10.1029/2021GC009998 |