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Chemistry and boron isotope ratios of Izu arc front volcanic rocks
The process of fluid release from the subducting slab beneath the Izu arc volcanic front (Izu VF) was examined by measuring B concentrations and B isotope ratios in the Neogene... -
Boron isotope ratios of samples from ODP Leg 125 sites at a serpentine seamou...
Serpentinite clasts and muds erupted from Conical Seamount, Mariana forearc, show substantial enrichment in boron (B) and 11B (delta11B up to +15 per mil ) relative to mantle... -
Composition of matrix glasses and melt inclusions of fallout tephra from ODP ...
We studied the systematics of Cl, F and H2O in Izu arc front volcanic rocks using basaltic through rhyolitic glass shards and melt inclusions (Izu glasses) from Oligocene to... -
Stable isotope composition of O, H, S, and C from serpentinites of the Marian...
The Mariana and Izu-Bonin arcs in the western Pacific are characterized by serpentinite seamounts in the forearc that provide unique windows into the mantle wedge. We present... -
Major element composition of phenocrysts from the volcanic basement of ODP Ho...
Early arc volcanism during Eocene to Oligocene in the Izu forearc region was investigated during ODP Legs 125 and 126 in 1989, and effusive and intrusive volcanics were... -
(Table 3) Strontium contents and isotope compositions in fossil fish teeth fr...
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(Table 2) Neodymium contents and isotope compositions in fossil fish teeth fr...
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(Table 1) Strontium isotope composition in pore waters at ODP Sites 130-807 a...
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