Transition in tectonic regime from the Paleo-Asian Ocean to Paleo-Pacific Ocean: constraints from the Jurassic adakitic and I-type granites, and calc-alkaline diorites at the northern margin of the North China Craton
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DOI: 10.1080/00206814.2020.1867913
Abstract: There is a broad consensus that subduction of the Paleo-Pacific oceanic plate has caused extensive magmatism, lithospheric deformation, and metal mineralization in the eastern margin of the Eurasia... read more here.
Keywords: regime paleo; paleo pacific; transition tectonic; paleo asian ... See more keywords