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Permian dyke swarm with bimodal affinity from the Hegenshan ophiolite-arc-accretionary belt, Central Inner Mongolia: Implications on lithospheric extension in a Carboniferous continental arc

Permian Dyke SwarmEngineeringGeographyTectonic EvolutionGeologyBimodal AffinityEarth ScienceRegional GeologyCentral Inner MongoliaTectonics