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Pressure, temperature and C-O-H fluid fugacities across the amphibolite-granulite transition, Northwest adirondack mountains, New York
R. Lawrence Edwards
, E. J. Essene
Earth and Environmental Sciences-Twin Cities
Research output
:
Contribution to journal
›
Article
›
peer-review
44
Scopus citations
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Dive into the research topics of 'Pressure, temperature and C-O-H fluid fugacities across the amphibolite-granulite transition, Northwest adirondack mountains, New York'. Together they form a unique fingerprint.
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Earth & Environmental Sciences
fugacity
49%
granulite
48%
amphibolite
47%
biotite
31%
garnet
30%
mountain
29%
transition
27%
fluid
25%
feldspar
19%
metamorphism
19%
barometry
17%
temperature
16%
grossular
15%
almandine
15%
pyrope
15%
resetting
14%
anorthite
13%
sillimanite
13%
erratic
12%
granulite facies
12%
rutile
12%
muscovite
11%
dehydration
11%
graphite
11%
zoning
10%
partial melting
10%
water temperature
9%
flooding
8%
quartz
7%
Physics & Astronomy
Adirondack Mountains (NY)
100%
biotite
54%
garnets
36%
feldspars
31%
fluids
26%
grade
21%
muscovite
16%
water temperature
15%
dehydration
13%
temperature
13%
rutile
11%
quartz
9%
graphite
9%
melting
8%
Chemical Compounds
Fugacity
61%
Pressure
25%
Rutile
10%
Melting
9%
Dehydration
9%
Graphite
8%