(PDF) Diversity of Fluid Geochemistry Affected by Processes

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

Geochemical Journal - Japan

doi 10.2343/geochemj.2.0311

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January 1, 2014

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Geochemical Society of Japan

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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

Geochemical Journal - Japan

doi 10.2343/geochemj.2.0311

Full Text

Abstract

Categories

Date

Authors

Publisher

Related search

Rare Earth Elements in the Hydrothermal System at Okinawa Trough Back-Arc Basin

Fluid Evolution and Hydrothermal Processes of the Spanish Central System

Comparative Elemental and Oxygen Isotope Geochemistry of Jasperoid in the Northern Great Basin; Evidence for Distinctive Fluid Evolution in Gold-Producing Hydrothermal Systems

Crustal Evolution of a Paleozoic Intra-Oceanic Island-Arc-Back-Arc Basin System Constrained by the Geochemistry and Geochronology of the Yakuno Ophiolite, Southwest Japan

Description of Seba Longimera Sp. Nov. From Hydrothermal Vents in the Okinawa Trough, Northwest Pacific (Amphipoda, Amphilochoidea, Sebidae)

Benthic Eukaryotic Diversity in the Guaymas Basin Hydrothermal Vent Environment

Major and Trace Element Chemistry and D/H, 18o/16o, 87Sr/86Sr and 143Nd/144Nd Ratios of Rocks From the Spreading Center of the Okinawa Trough, a Marginal Back-Arc Basin.

Characterization of the Genome Feature and Toxic Capacity of a Bacillus Wiedmannii Isolate From the Hydrothermal Field in Okinawa Trough

Sulfur Isotopic Ratios of Hydrothermal Vent-Animals at Ogasawara Arc and Mid-Okinawa Trough-Evidence for Microbial Origin of Hydrogen Sulfide at Low-Temperature Submarine Hydrothermal Areas.