Chemical composition of hydrothermal ores from Mid-Okinawa Trough and Suiyo Seamount determined by neutron activation analysis

Author:

NOGUCHI TAKUROH,OOMORI TAMOTSU,TANAHARA AKIRA,TAIRA NAOTO,TAKADA JITSUYA,TAIRA HATSUO

Publisher

Geochemical Society of Japan

Subject

Geochemistry and Petrology,Geophysics

Reference21 articles.

1. Chiba, H., Nakashima, K., Gamo, T., Ishibashi, J., Tsunogai, U. and Sakai, H. (1993) Hydrohtermal activity at the Minami-Ensei Knoll, Okinawa Trough: Chemical characteristics of hydrothermal solutions. Proceedings JAMSTEC Symposium Deep Sea Research, 9, 271-282 (in Japanese with English abstract).

2. Pb-210 fluxes and sedimentation rates on the lower continental slope between Taiwan and the South Okinawa Trough

3. High alkalinity due to sulfate reduction in the CLAM hydrothermal field, Okinawa Trough

4. Glasby, G. P. and Notsu, K. (2003) Submarine hydrothermal mineralization in the Okinawa Trough, SW of Japan: an overview. Ore Geol. Rev. 23, 299-339.

5. Geology and mineralogy of massive sulfide ores from the central Okinawa Trough, Japan

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