A new model of thermal and physicochemical dynamics for volcanogenic epithermal deposits (Asacha Deposit, Kamchatka)

The key problem in description of the dynamics of the ore-forming process in volcanogenic epithermal deposits is to take into account the appearance and disappearance of phase boundaries in the flows of magmatic or mixed fluids in the system of leading equations and boundary conditions. This require...

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Bibliographic Details
Published in:	Doklady earth sciences Vol. 431; no. 2; pp. 453 - 457
Main Authors:	Bessonova, E. P., Sharapov, V. N., Chudnenko, K. V., Cherepanova, V. K.
Format:	Journal Article
Language:	English
Published:	Dordrecht SP MAIK Nauka/Interperiodica 01-04-2010 Springer Springer Nature B.V
Subjects:	Boundary conditions Earth and Environmental Science Earth Sciences Fluid flow Geochemistry Geophysics Magma Volcanoes Kamchatka Peninsula Wall Rock DOKLADY Earth Science Epithermal Deposit Magmatic Fluid Fluid Conductor
Online Access:	Get full text
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Summary:	The key problem in description of the dynamics of the ore-forming process in volcanogenic epithermal deposits is to take into account the appearance and disappearance of phase boundaries in the flows of magmatic or mixed fluids in the system of leading equations and boundary conditions. This requires a model of nonisothermal physicochemical interaction of fluid flow and rock in the presence of mobile interfaces in the fluid infiltration area.
ISSN:	1028-334X 1531-8354
DOI:	10.1134/S1028334X10040094