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- W4328115533 abstract "Abstract When modern-style plate tectonics commenced on Earth remains one of fundamental questions in unravelling the evolution of our planet, due to the apparent lack of low-thermal gradients in old metamorphic rocks (< 350 °C/GPa)—a key indicator of modern plate subduction—during the Archaean and Palaeoproterozoic Era. Here we present 2.0 Gyr lawsonite eclogites and associated eclogite-facies garnet-kyanite-chloritoid schists with low-thermal gradients of 265-290°C/GPa from the Kongling Complex in South China through integrated thermodynamic modelling and zircon in situ U-Pb dating. More importantly, a temporally equivalent mafic granulites with high-thermal gradients of ~720 °C/GPa has been also recognized spatially adjacent to those low dT/dP eclogite-facies rocks, integrated as a classic paired metamorphic belt. The results show a new discovery of Paleoproterozoic classic paired metamorphic belts driven by cold deep subduction in South China, indicating that the modern-style plate tectonics was already operative on Earth by the Palaeoproterozoic." @default.
- W4328115533 created "2023-03-22" @default.
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- W4328115533 date "2023-03-21" @default.
- W4328115533 modified "2023-10-17" @default.
- W4328115533 title "Modern-style plate tectonics preserved in the Paleoproterozoic paired metamorphic belts driven by cold deep subduction" @default.
- W4328115533 doi "https://doi.org/10.21203/rs.3.rs-2594860/v1" @default.
- W4328115533 hasPublicationYear "2023" @default.
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