From oceanic subduction to continental collision: Revisiting the Permian–Triassic magmatism of the Indosinian orogenic belt, Vietnam
Résumé
Indosinian orogenic belt resulted from the Early Mesozoic collision between the South China block and the Indochina block, driven by the closure of Eastern Paleo-Tethys Ocean. In this study, we revisit Early Permian to Middle Triassic magmatic rocks in the Western Ailaoshan-Truong Son-Sam Nua magmatic unit (North Vietnam segment), Indosinian orogenic belt. New petrological, geochronological, geochemical, and zircon
