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Title :Diversity of fluid geochemistry affected by processes during fluid upwelling in active hydrothermal fields in the Izena Hole, the middle Okinawa Trough back-arc basin
Authors :Ishibashi, Jun-Ichiro
Noguchi, Takuroh
Toki, Tomohiro
Miyabe, Shunsuke
Yamagami, Shosei
Onishi, Yuji
Yamanaka, Toshiro
Yokoyama, Yuka
Omori, Eriko
Takahashi, Yoshio
Hatada, Kenta
Nakaguchi, Yuzuru
Yoshizaki, Motoko
Konno, Uta
Shibuya, Takazo
Takai, Ken
Inagaki, Fumio
Kawagucci, Shinsuke
Issue Date :31-Jul-2014
Abstract :Two active hydrothermal fields, Jade and Hakurei fields have been discovered within the Izena Hole, a rectangular 6 km × 3 km shape depression located in the middle Okinawa Trough back arc basin. In both fields, intense hydrothermal activity is represented by venting of high-temperature fluid (>300°C) and occurrence of sulfide/sulfate ore deposits. We collected hydrothermal fluids during dive expeditions of ROV Hyper Dolphin conducted in 2003, 2010 and 2011, in order to analyze both elemental and gas species. The geochemistry of high temperature hydrothermal fluids collected from the Jade and Hakurei fields is very similar to each other with exceptions in minor gas composition. Little temporal variation was observed in geochemistry of the high-temperature hydrothermal fluid of the Jade field over two decades, since a previous study carried out in 1989. These results suggest that these fluids are derived from a common fluid reservoir where fluid chemistry is basically controlled by fluid-mineral equilibria and gas species are dominantly contributed from the same magma. Venting of low temperature fluid (about 104°C) was discovered in the distal part of the Jade field, which was named as the Biwako vent. Chemical composition of the Biwako vent fluid was distinctive from that of the high temperature fluid in the proximal part of the Jade field, and could not be explained by simple dilution or cooling. This intra-field chemical diversity could be caused by phase separation and segregation during fluid upwelling, based on relationships in concentrations of Cl and major cations. On the other hand, the chemical diversity recognized in minor gas composition between the Jade and Hakurei fields is in accordance with results from previous plume survey. Difference in concentrations of minor gases such as H2 is attributed to contribution from thermal degradation of organic matter in the sediment, during fluid upwelling.
URL :https://doi.org/10.2343/geochemj.2.0311
Type Local :雑誌掲載論文
ISSN :1880-5973
0016-7002
Publisher :GEOCHEMICAL SOCIETY OF JAPAN
URI :http://hdl.handle.net/20.500.12000/37725
Citation :Geochemical Journal Vol.48 no.4 p.357 -369
Appears in Collections:Peer-reviewed Journal Articles (Faculty of Science)

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