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The role of subduction channel mélanges and convergent subduction systems in the petrogenesis of post-collisional K-rich mafic magmatism in NW Tibet

Magmatic ProcessIndia-asia Collision ZoneEarth ScienceEngineeringIgneous PetrogenesisSubduction Channel MélangesEast Asian LanguagesGeologyIndia-asia CollisionNw TibetConvergent Subduction SystemsPetrologyTibetan PlateauTectonics