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Late Cenozoic to recent transtensional deformation across the Southern part of the Gaoligong shear zone between the Indian plate and SE margin of the Tibetan plateau and its tectonic origin

India-asia Collision ZoneEngineeringEast Asian StudiesSe MarginTectonic EvolutionEast Asian LanguagesGeologyIndian PlateIndia-asia CollisionLanguage StudiesEarth ScienceTibetan PlateauTectonics