[S-CG64] 脆性延性境界と超臨界地殻流体：島弧地殻エネルギー

[SCG64-10] 下部地殻マグマプロセス：東北日本第四紀フロント火山の同位体組成からの検討

*伴 雅雄¹、木村 純一²、高橋 俊郎³、鵜沢 由香⁴、大場 司⁵、藤縄 明彦⁶、林 信太郎⁵、吉田 武義⁷、宮崎 隆²、Chan Qing²、仙田 量子⁸、Vaglarov Bogdan²、巽 好幸⁹ (1.山形大学、2.海洋研究開発機構、3.新潟大学、4.千葉工業大学、5.秋田大学、6.茨城大学、7.東北大学、8.九州大学、9.神戸大学)

キーワード：下部地殻、マグマプロセス、Sr-Nd-Pb-Hf同位体組成

We examined the lower crustal magmatic processes beneath Quaternary frontal volcanoes of the NE Japan arc based on Sr–Nd–Hf–Pb isotopic compositions coupled with trace and major element compositions. The frontal arc is characterized by the coexistence of medium-K to low-K calc-alkaline and tholeiitic magma suites. The remarkable findings are quasi-linear isotopic trends in the Pb–Pb and Nd–Pb isotope space, which are distinctive of the magmas from individual volcanoes irrespective of their magma suites. The enriched magmas from volcanoes on the same segment of the basement share the same isotopic composition with their basement granitoids. Further, isotopic compositional variations in basalts cover whole range of the variations in each volcano. Examinations of these geochemical data led us to conclude the observed trends form mixing lines drawn between isotopically depleted metasomatized mantle-derived basalt and enriched mafic lower crustal materials or their melts, which are isotopically heterogeneous along the arc. Assimilation-fractional-crystallization (AFC) and melting-assimilation-storage-hybridization (MASH) are responsible for the intermediate to felsic compositional trends of the tholeiitic and calc-alkaline rock suites, respectively. These processes mostly occurred in an amphibolitic lower crust. The results demonstrate that the mafic lower crust extensively contributes to the diversity of the arc magmas of basalt to rhyolitic compositions. Role of the mafic lower crust to the geochemical variations of arc basalts is usually cryptic but the study of the magmas from NE Japan reveals its fundamental significance in diversity of arc magmas.