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- W4321379646 abstract "We identified six Kuroko-type deposits in the Izu collision zone, central Japan, which formed as seafloor massive sulfides (SMS) in the Paleo-Izu Arc before its collision with the Honshū Arc during the middle Miocene. These deposits are found in the same stratigraphic horizon (~15 Ma) in the Nishiyatsushiro and Koma groups, between the basaltic volcanic sequence of the Furusekigawa Formation (or its equivalent) and the hanging-wall mudstone of the Tokiwa Formation of the Nishiyatsushiro Group (or the equivalent sedimentary unit in the Koma Group)." @default.
- W4321379646 created "2023-02-21" @default.
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- W4321379646 date "2023-02-22" @default.
- W4321379646 modified "2023-09-30" @default.
- W4321379646 title "Kuroko-type Deposits of the Misaka-Koma Mountains in the Izu collision zone, central Japan: Their Occurrence and Geological Implications" @default.
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- W4321379646 doi "https://doi.org/10.5575/geosoc.2022.0028" @default.
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