Chemistry of hydrothermal fluids at the TAG active mound, MAR 26

H. Chiba, H. Masuda, S. Y. Lee, K. Fujioka

Research output: Contribution to journalArticle

26 Citations (Scopus)

Abstract

Black smoker and clear fluids were sampled at the TAG active mound (26°08′N, 44°50'W) in August 1998. The major ion chemistry of the black smoker fluid appears to be stable over 12 years, indicating that the physico-chemical condition of the deep reaction zone have not changed significantly within this period. The black smoker fluid chemistry is the same independent of the place of the venting on the mound, suggesting that the black smoker fluid is supplied from the single sourse. Two medium temperature clear fluid samples (256° and 219°C) are depleted in Ca 2+, Fe 2+, and H 2S compared to the black smoker fluid due to the precipitation of anhydrite and iron sulfide caused by mixing with entrained seawater. These clear fluids are formed by the same mechanism as the white smoker and diffuse fluids.

Original languageEnglish
Pages (from-to)2919-2922
Number of pages4
JournalGeophysical Research Letters
Volume28
Issue number15
DOIs
Publication statusPublished - Aug 1 2001

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submarine hydrothermal vents
hydrothermal fluid
black smoker
chemistry
fluid
fluids
venting
iron sulfide
anhydrite
sulfides
seawater
iron
ion

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)

Cite this

Chemistry of hydrothermal fluids at the TAG active mound, MAR 26. / Chiba, H.; Masuda, H.; Lee, S. Y.; Fujioka, K.

In: Geophysical Research Letters, Vol. 28, No. 15, 01.08.2001, p. 2919-2922.

Research output: Contribution to journalArticle

Chiba, H, Masuda, H, Lee, SY & Fujioka, K 2001, 'Chemistry of hydrothermal fluids at the TAG active mound, MAR 26', Geophysical Research Letters, vol. 28, no. 15, pp. 2919-2922. https://doi.org/10.1029/2000GL012645
Chiba, H. ; Masuda, H. ; Lee, S. Y. ; Fujioka, K. / Chemistry of hydrothermal fluids at the TAG active mound, MAR 26. In: Geophysical Research Letters. 2001 ; Vol. 28, No. 15. pp. 2919-2922.
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