Based on new and previously published Sr and Nd isotope data, we examined the petrogenetic relationship between deep crust- and upper mantle-derived xenoliths contained in Cenozoic volcanic rocks and Cretaceous-Paleogene granitoid rocks in SW Japan. The deep crust- and upper mantle-derived mafic to ultramafic xenoliths contained in Cenozoic volcanic rocks from SW Japan have comparable initial Sr and Nd isotope ratios to the Cretaceous-Paleogene granitoid rocks in their respective districts. This may suggest that these xenoliths were genetically related to the Cretaceous-Paleogene granitoid rocks in SW Japan, and that regional variations in Sr and Nd isotope ratios observed in the granitoid rocks are attributed to differences in the geochemistry of the magma sources.
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Kyoto Univ, Grad Sch Sci, Inst Geothermal Sci, Beppu, Oita 8740903, JapanKyoto Univ, Grad Sch Sci, Inst Geothermal Sci, Beppu, Oita 8740903, Japan
Yoshikawa, Masako
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Arai, Shoji
Ishida, Yoshito
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Kanazawa Univ, Dept Earth Sci, Kanazawa, Ishikawa 9201192, Japan
Tokyo Univ Agr & Technol, Grad Sch Bioapplicat & Syst Engn, Tokyo 1830057, JapanKyoto Univ, Grad Sch Sci, Inst Geothermal Sci, Beppu, Oita 8740903, Japan
Ishida, Yoshito
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Tamura, Akihiro
Shimizu, Yohei
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Kanazawa Univ, Dept Earth Sci, Kanazawa, Ishikawa 9201192, Japan
Dia Consultants Co Ltd, Tokyo 1010032, JapanKyoto Univ, Grad Sch Sci, Inst Geothermal Sci, Beppu, Oita 8740903, Japan