The Mesozoic magmatic, metamorphic, and tectonic evolution of the eastern Gangdese magmatic arc, southern Tibet
Magmatic arcs are natural laboratories for studying the growth of continental crusts. The Gangdese arc, southern Tibet, is an archetypal continental magmatic arc that formed due to Mesozoic subduction of the Neo-Tethyan oceanic lithosphere; however, its formation and evolution remain controversial....
| Main Authors: | , , , , , , , , , , |
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| Formato: | Journal article |
| Idioma: | English |
| Publicado: |
Geological Society of America
2021
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