Fluid-assisted modification of garnet composition along rims, cracks, and mineral inclusion boundaries in samples of amphibolite facies schists

Compositional zoning patterns in garnet from schists in central Vermont and western Connecticut suggest that prograde garnet growth was followed by an episode of compositional modification during fluid-assisted metasomatism.

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Veröffentlicht in:The American mineralogist 1993-04, Vol.78 (3-4), p.338-344
Hauptverfasser: Hames, Willis E, Menard, Thomas
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container_title The American mineralogist
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Menard, Thomas
description Compositional zoning patterns in garnet from schists in central Vermont and western Connecticut suggest that prograde garnet growth was followed by an episode of compositional modification during fluid-assisted metasomatism.
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subjects amphibolite facies
central Vermont
Connecticut
Devonian
diffusion
facies
fluid inclusions
garnet group
Geology
Gile Mountain Formation
igneous and metamorphic rocks
inclusions
metamorphic rocks
metasomatism
mineral inclusions
mineralization
Mineralogy
Minerals
nesosilicates
orthosilicates
P-T conditions
Paleozoic
Petrology
schists
silicates
United States
Vermont
western Connecticut
title Fluid-assisted modification of garnet composition along rims, cracks, and mineral inclusion boundaries in samples of amphibolite facies schists
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