Thermal state and evolving geodynamic regimes of the Meso- to Neoarchean North China Craton
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DOI: 10.1038/s41467-021-24139-z
Abstract: Constraining thickness and geothermal gradient of Archean continental crust are crucial to understanding geodynamic regimes of the early Earth. Archean crust-sourced tonalitic–trondhjemitic–granodioritic gneisses are ideal lithologies for reconstructing the thermal state of early continental crust.… read more here.
Keywords: thermal state; china craton; north china; geodynamic regimes ... See more keywords