作者: Masako YOSHIKAWA , Shoji ARAI , Yoshito ISHIDA , Akihiro TAMURA , Yohei SHIMIZU
DOI: 10.2465/JMPS.100622B
关键词: Metasomatism 、 Trace element 、 Partial melting 、 Island arc 、 Basalt 、 Lithosphere 、 Geology 、 Xenolith 、 Geochemistry 、 Ultramafic 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.