Crustal evolution of a continental magmatic arc from subduction to collision: a case study in the Gangdese arc, southern Tibetan Plateau
Magmatic arcs are the main environment where continental crust is created on the post-Archean Earth; however, how juvenile arc crust evolves into mature continental crust is still controversial. In this study, we report new bulk-rock major and trace elements, Sr-Nd isotopes, and zircon U-Pb ages and...
Príomhchruthaitheoirí: | , , , , , |
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Formáid: | Journal article |
Teanga: | English |
Foilsithe / Cruthaithe: |
Geological Society of America
2024
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