Pentlandite and Co-enriched pentlandite as characteristic minerals of modern hydrothermal sulfide mounds hosted by serpentinized ultramafic rocks (Mid-Atlantic Ridge)

Author:

Borodaev Yu. S.,Bryzgalov I. A.,Mozgova N. N.,Uspenskaya T. Yu.

Publisher

Allerton Press

Subject

General Earth and Planetary Sciences

Reference39 articles.

1. Bel’tenev, V.E., Nescheretov, A.V., Ivanov, et al., A New Hydrothermal Ore Field in the Axial Zone of the Mid-Atlantic Ridge, Dokl. RAN. Earth Sci., 2004, vol. 397, no. 5, pp. 690–693.

2. 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 Depos., 2002, vol. 44, no. 6, pp. 444–473.

3. Bogdanov, Yu.A. and Sagalevich, A.M., Geologicheskie issledovaniya s glubokovodnykh obitaemykh apparatov “Mir” (Geological Surveys from Mir Manned Submersibles), Moscow: Nauchnyi Mir, 2002.

4. Borodaev, Yu.S., Mozgova, N.N., Gablina, I.F., et al.,., Zonal Pipes of Black Smokers from the Rainbow Hydrothermal Field (Mid-Atlantic Ridge, 36°14′ N), Vest. Mosk. Univ. Geologiya, 2004, vol. 3, pp. 40–49.

5. Vaughan, D. and Craig, J., Mineral Chemistry of Metal Sulfides, New York: Cambridge Univ., 1978. Translated under the title Khimiya sul’fidnykh mineralov, Moscow: Mir, 1981.

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