Investigation of hydrodynamic conditions Ashadze vent fields (Mid-Atlantic ridge)
About authors
- 1 — Ph.D., Dr.Sci. professor Saint Petersburg State Mining University
- 2 — undergraduate student Saint Petersburg State Mining University
Abstract
The main geological and thermodynamic conditions of hydrothermal vents formation and activity. Calculation of hydrothermal field vents flow have been made after E.S.Romm model. A comparison of model data with data obtained in the Russian-French expedition «SERPENTINE».
Область исследования:
Geology
Funding:
None
References
- Bogdanov Y.A. Hydrothermal ores of the Mid-Atlantic ridge rift zones. Мoscow, 1997. 167 p.
- Hydrothermal sulfide ores and metalliferous sediments of the ocean / E d. by . I.S.Gramberg and A.I.Aynemer. Saint Petersburg, 1992. P.192-204.
- Grichuk D.V. Thermodynamic model of submarine hydrothermal systems. Moscow, 2000. 205 p.
- Krasnov S.G., Sudarikov S.M. Chemical composition and origin of oceanic hydrothermal ore-forming solutions // Volcanology and Seismology . 1990 . N 5. P.37-50.
- Romm E.S. Structural models of the pore space of rocks. Saint Petersburg, 1989. 257 p.
- Sudarikov S.M. Hydrogeological structure of hydro-thermally active regions of the North Atlantic // State Mining Institute. 2008. Vol. 176. P.26-30.
- Sudarikov S.M. Hydrothermal solutions Mid-Atlantic Ridge: initial results of Russian-French expedition of 2007 // Hydrogeochemistry sedimentary basins. Tomsk, 2007. P.59-65.
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