Recycling of Paleo-oceanic crust: Geochemical evidence from early Paleozoic mafic igneous rocks in the Tongbai orogen, Central China
Lithos, pp. 312-327, 2019.
Abstract Crustal subduction generally develops from oceanic to continental subduction in collisional orogens, with the disappearance of previously subducted paleo-oceanic crust. However, it is not straightforward to trace the fate of subducted paleo-oceanic crust due to modification by subsequent continental collision. In this study, we...More
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