Peridotite-basalt association at MAR between 19°42′ and 19°59′ N: Evaluation of petrogenetic conditions and material balance during hydrothermal transformation of the oceanic crust

Author:

Silantyev S. A.,Bortnikov N. S.,Shatagin K. N.,Bychkova Ya. V.,Krasnova E. A.,Bel’tenev V. E.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology

Reference49 articles.

1. Abstracts of Chapman Conference on Detachments in Oceanic Lithosphere. Detachments in Oceanic Lithosphere: Deformation, Magmatism, Fluid Flow, and Ecosystems (Agros, 2010).

2. Allen, D.E. and Seyfried, W.E., Jr., Serpentinization and heat generation: constraints from Lost City and Rainbow hydrothermal systems, Geochim. Cosmochim. Acta, 2004, vol. 68, no. 6, pp. 1347–1354.

3. Bach, W., Jöns, N., and Klein, F., Metasomatism within ocean crust, in The Role of Fluids in Terrestrial And Extraterrestrial Processes, Harlov, D. E. and Austrheim, H., Eds., Heidelberg-New York-Dordrecht-London: Springer, 2013.

4. Bogdanov, Yu.A., Bortnikov, N.S., Vikent’ev, I.V., et al., A new type of modern mineral-forming system: black smokers of the hydrothermal field at 14°45′ N latitude, Mid-Atlantic Ridge, Geol. Ore Dep., 1997, vol. 39, no. 1, pp. 58–78.

5. Bogdanov, Yu.A., Bortnikov, N.S., Vikent’ev, I.V., et al., Mineralogical-geochemical peculiarities of hydrothermal sulfide ores and fluids in the Rainbow Field associated with serpentinites, Mid-Atlantic Ridge (36°14′ N), Geol. Ore Dep., 2002, vol. 44, no. 6, pp. 444–473.

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