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Using detrital zircons from late Permian to Triassic sedimentary rocks in the south-eastern Central Asian Orogenic Belt (NE China) to constrain the timing of the final closure of the Paleo-Asian Ocean

Detrital ZirconsMarine GeologyEngineeringEast Asian StudiesNe ChinaTectonic EvolutionEast Asian LanguagesGeologyIndia-asia CollisionLanguage StudiesGeochronologyOrogenyLate PermianEarth ScienceTectonics