We analyzed the Sr isotope and trace element compositions of the post-caldera volcanic products of Aso volcano in central Kyushu, with the aim of investigating the genetic relationship between the last caldera-forming (Aso-4) magmas and post-caldera magmas. The 87Sr/86Sr ratio of the magmas drastically changed from the homogeneous (0.7041-0.7042) caldera-forming stage to the heterogeneous (0.7040-0.7044) post-caldera stage. In addition, the obtained geochemical data suggested that the Aso-4 magma did not contribute to the origin and compositional evolution of the post-caldera magmas. These observations indicated that the generation of post-caldera magmas was probably independent of the Aso-4 magma.
Vol.31 (1944) No. 5 and No.6 of the predecessor journal, "The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists" are available at this J-Stage site. (updated Aug. 2, 2018)