Composition and evolution of ore fluids in a magmatic-hydrothermal skarn deposit

Volume: 32, Issue: 2, Pages: 117 - 120
Published: Feb 1, 2004
Abstract
The chemistry of brine, vapor, and low-salinity fluid inclusions measured by proton-induced X-ray emission from the Bismark skarn deposit, Mexico, is consistent with an evolving magmatic-hydrothermal system with no evidence for external fluid inputs. The results support a model that invokes early phase separation of magmatic fluids into brine and vapor (two-phase field) at high temperature and lithostatic pressure, followed by the entrapment of...
Paper Details
Title
Composition and evolution of ore fluids in a magmatic-hydrothermal skarn deposit
Published Date
Feb 1, 2004
Journal
Volume
32
Issue
2
Pages
117 - 120
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