Petrogenesis of Early Jurassic (ca. 181 Ma) dacitic–rhyolitic volcanic rocks in the Amdo ophiolite mélange, central Tibetan Plateau: Low‐pressure partial melts of Bangong–Nujiang Tethys oceanic crust?
Abstract:The identification of oceanic-crust-derived melts is critical to improving our understanding of oceanic lithosphere subduction in various geodynamic settings. However, low-pressure melts derived from the oceanic crust can be misidentified because their compositions are often indistinguishable from those of typical arc-related rocks. In this study, we report geochronological and geochemical data for the Amdo volcanic rocks in the central Tibetan Plateau. Zircon U-Pb dating indicates that they were generated in … Show more
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