Trace element and Sr-Nd isotopic features of ultramafic xenoliths from Kurose, Southwest Japan

作者: Masako YOSHIKAWA , Shoji ARAI , Yoshito ISHIDA , Akihiro TAMURA , Yohei SHIMIZU

DOI: 10.2465/JMPS.100622B

关键词: MetasomatismTrace elementPartial meltingIsland arcBasaltLithosphereGeologyXenolithGeochemistryUltramafic rock

摘要: Ultramafic xenoliths from Kurose, Southwest Japan, are fragments of the lithospheric mantle beneath back arc active Japan volcano-tectonic arc. Trace element and Sr-Nd isotopic compositions clinopyroxenes in ultramafic suggest that several enrichment processes responsible for geochemical variation. These would have witnessed following events: (1) open-system partial melting continental lithosphere with an influx asthenospheric melt MORB-like composition during formation back-arc basin resulted Sea opening, (2) under a fluid/melt derived subducted slab, (3) metasomatism after these events by island tholeiitic basalt Neogene period. Moreover, variations depletion levels Zr Ti source preceded metasomatic events.

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