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...
المؤلفون الرئيسيون: | Zhang, Z-M, Ding, H-X, Palin, RM, Dong, X, Tian, Z-L, Li, X-W |
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التنسيق: | Journal article |
اللغة: | English |
منشور في: |
Geological Society of America
2024
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مواد مشابهة
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The lower crust of the Gangdese magmatic arc, southern Tibet, implication for the growth of continental crust
حسب: Zhang, Z, وآخرون
منشور في: (2019) -
The Mesozoic magmatic, metamorphic, and tectonic evolution of the eastern Gangdese magmatic arc, southern Tibet
حسب: Zhang, Z-M, وآخرون
منشور في: (2021) -
Early Cenozoic partial melting of meta-sedimentary rocks of the eastern Gangdese arc, southern Tibet, and its contribution to syn-collisional magmatism
حسب: Jiang, Y-Y, وآخرون
منشور في: (2021) -
Late cretaceous metamorphism and anatexis of the gangdese magmatic arc, south tibet: implications for thickening and differentiation of juvenile crust
حسب: Ding, H, وآخرون
منشور في: (2022) -
Intraoceanic subduction system within the Neo-Tethys: evidence from Late Cretaceous arc magmatic rocks of the eastern Himalaya
حسب: Zhang, Z, وآخرون
منشور في: (2023)