Publication | Closed Access
Southward trench migration at ∼130–120 Ma caused accretion of the Neo-Tethyan forearc lithosphere in Tibetan ophiolites
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Citations
48
References
2016
Year
Tibetan OphiolitesIndia-asia Collision ZoneEngineeringNeo-tethyan ForearcGeographyTectonic EvolutionIndia-asia CollisionGeologySouthward Trench MigrationEarth ScienceTibetan PlateauTectonics
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