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Formation of an Intracontinental Orogen Above the Permo-Triassic Mantle Convection Cell in the Paleo-Tethys Tectonic Realm due to Far-Field Stress Derived From Continental Margins
The identification of intraplate orogens seemingly poses challenges to the plate tectonic theory. Delineating the formation processes of intraplate orogens can provide clues for the better understandings of the above issue. Although still controversial, the Indosinian (Permo-Triassic) orogeny in the...
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Main Authors: | , , |
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Formato: | Artigo |
Idioma: | Inglês |
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Frontiers Media S.A.
2022-05-01
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Colecção: | Frontiers in Earth Science |
Assuntos: | |
Acesso em linha: | https://www.frontiersin.org/articles/10.3389/feart.2022.892787/full |
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