Original Research
Published on 10 May 2022
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
in Geochemistry
Frontiers in Earth Science
doi 10.3389/feart.2022.892787
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- 7 citations


