Isotopic-geochemical characteristics of the lost city hydrothermal field

Author:

Dubinina E. O.,Chernyshev I. V.,Bortnikov N. S.,Lein A. Yu.,Sagalevich A. M.,Gol’tsman Yu. V.,Bairova E. D.,Mokhov A. V.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology,Geophysics

Reference27 articles.

1. C. R. German and K. L. Von Damm, “Hydrothermal Processes,” in Treatise in Geology. The Oceans and Marine Geochemistry, Ed. by H. Elderfield (Elsevier. Amsterdam, 2003), Vol. 6, pp. 182–222.

2. W. S. Shanks III, “Stable Isotopes in Seafloor Hydrothermal Systems: Vent Fluids, Hydrothermal Deposits, Hydrothermal Alteration, and Microprobe Processes,” in Stable Isotope Geochemistry, Ed. by J. W. Valley and D. R. Cole, Rev. Mineral. Geochem. 43, 469–525 (2001).

3. N. S. Bortnikov and I. V. Vikent’ev, “Modern Base Metal Sulfide Mineral Formation in the World Ocean,” Geol. Rudn. Mestorozhd. 47, 16–50 (2005) [Geol. Ore Dep. 47, 13–45 (2005)].

4. D. S. Kelley, J. A. Karson, D. K. Blackman, et al., “An Off-Axis Hydrothermal Vent Field near the Mid-Atlantic Ridge at 30°N,” Nature 412(12), 145–149 (2001).

5. G. L. Fruh-Green, D. S. Kelley, S. M. Bernasconi, et al., “30 000 Years of Hydrothermal Activity at the Lost City Vent Field,” Science 301, 495–498 (2003).

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