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Mid-Paleozoic arc granitoids in SW Japan with Neoproterozoic xenocrysts from South China: New zircon U–Pb ages by LA-ICP-MS

Shuhei Sakata,Takafumi Hirata,Kazumasa Aoki,Yukio Isozaki,Atsushi Yamamoto

Journal of Asian Earth Sciences（2015）

Cited 55|Views6
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Abstract
•Zircon from the Paleozoic igneous rock in SW Japan was dated by LA-ICP-MS.•Mitaki dioritic rocks formed a part of Paleozoic arc batholith of proto-Japan.•Nabaenohana “tonalite” formed through melting of terrigenous clastic rocks.•Paleozoic Japan developed along the Cathaysia margin of South China.•Disappearance of Paleozoic granitic belt of proto-Japan occurred by tectonic erosion.
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Key words
U–Pb age,Zircon,Paleozoic,Kurosegawa,South China
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