Geochemical characteristics of stable isotopes from hydrothermal chimneys in the Mariana Trough, West Pacific Ocean

Wu Shi-ying; Zhang Dao-jian; Wang Kui-yang; Chen Cheng-ye; Bai Li-ming

doi:10.1007/BF02876089

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Geochemical characteristics of stable isotopes from hydrothermal chimneys in the Mariana Trough, West Pacific Ocean

Updated：2023-05-16

- Geochemical characteristics of stable isotopes from hydrothermal chimneys in the Mariana Trough, West Pacific Ocean
- Journal of Oceanology and Limnology Vol. 18, Issue 4, Pages: 378-384(2000)
- Affiliations：
  
  1. SOA First Institute of Oceanography
  2. Department of Geology Beijing University
- Author bio：
- Funds：
- DOI：10.1007/BF02876089
  CLC：
- Published：2000
- Accepted：
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Shi-ying, W., Dao-jian, Z., Kui-yang, W. et al. Geochemical characteristics of stable isotopes from hydrothermal chimneys in the Mariana Trough, West Pacific Ocean., Chin. J. Ocean. Limnol. 18, 378–384 (2000). https://doi.org/10.1007/BF02876089
DOI：

Shi-ying, W., Dao-jian, Z., Kui-yang, W. et al. Geochemical characteristics of stable isotopes from hydrothermal chimneys in the Mariana Trough, West Pacific Ocean., Chin. J. Ocean. Limnol. 18, 378–384 (2000). https://doi.org/10.1007/BF02876089 DOI：

摘要

Abstract

The determination of the stable isotopes

δD

δ18 and δ30

values from hydrothermal chimneys in the Mariana Trough

the West Pacific

indicated that the pure siliceous chimneys with gentle data variation were formed in low temperature environment. It reflects that the sea-floor hydrothermal activity of the Mariana Trough is primarily low-to-medium temperature hydrothermal eruption

and those chimneys with strong data variation and containing pyrite were formed in higher temperature environment.

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references

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