Effect of Quartz Deposition on the Dynamics of Magma Chamber Degassing


Cite item

Full Text

Open Access Open Access
Restricted Access Access granted
Restricted Access Subscription Access

Abstract

The filtration of a supercritical brine flow during the magma chamber degassing is numerically simulated with consideration of quartz transport and deposition. It is shown that the quartz deposition and the accompanying decrease of permeability reduce the size of the concentrated brine lens formed above the magma chamber. The effect of rock hydraulic fracture on the lens formation is studied. An unsteady degassing regime is revealed; this regime is associated with a periodic increase and decrease in permeability due to the hydraulic fracturing and quartz deposition. The obtained numerical results are in agreement with the geological data on the structure of copper deposits.

About the authors

I. S. Utkin

Moscow State University, Faculty of Mechanics and Mathematics

Author for correspondence.
Email: ivan@utki.ch
Russian Federation, Leninskie Gory, Moscow, 119899

O. E. Mel’nik

Moscow State University, Moscow University Institute of Mechanics

Author for correspondence.
Email: melnik@imec.msu.ru
Russian Federation, Leninskie Gory, Moscow, 119991

A. A. Afanas’ev

Moscow State University, Moscow University Institute of Mechanics

Author for correspondence.
Email: afanasyev@imec.msu.ru
Russian Federation, Leninskie Gory, Moscow, 119991

Yu. D. Tsvetkova

Moscow State University, Moscow University Institute of Mechanics

Author for correspondence.
Email: jultsv@gmail.com
Russian Federation, Leninskie Gory, Moscow, 119991

Supplementary files

Supplementary Files
Action
1. JATS XML

Copyright (c) 2018 Allerton Press, Inc.