Petrogenesis of the ∼500 Ma Fushui mafic intrusion and Early Paleozoic tectonic evolution of the Northern Qinling Belt, Central China
Journal of Asian Earth Sciences(2017)
Abstract
•Geochemical, zircon U-Pb dating and Hf isotopic data were conducted.•The Fushui intrusion was formed at ~500Ma related to subduction of Shangdan oceanic lithosphere.•Rocks were derived from <10% partial melting of phlogopite-garnet lherzolite.
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Key words
Metasomatized mantle source,Early Paleozoic arc setting,Shangdan suture zone,Northern Qinling Belt
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