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Experimentally-determined trace element characteristics of aqueous fluid from partially dehydrated mafic oceanic crust at 3.0 GPa, 650-700°C
Trevor H. Green
*
,
John Adam
*
Corresponding author for this work
Research output
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Contribution to journal
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Article
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peer-review
131
Citations (Scopus)
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Dive into the research topics of 'Experimentally-determined trace element characteristics of aqueous fluid from partially dehydrated mafic oceanic crust at 3.0 GPa, 650-700°C'. Together they form a unique fingerprint.
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Earth & Environmental Sciences
lawsonite
100%
oceanic crust
89%
chloritoid
71%
trace element
67%
omphacite
66%
garnet
54%
fluid
51%
phengite
38%
rutile
32%
rare earth element
25%
talc
23%
mid-ocean ridge basalt
21%
dehydration
19%
subduction zone
19%
coesite
13%
staurolite
12%
geothermal gradient
11%
tholeiite
11%
electron probe analysis
10%
clinopyroxene
9%
magmatism
9%
magnetite
9%
partitioning
8%
subduction
8%
magma
7%
fold
7%
mantle
7%
mineral
5%
water
3%
Chemistry
Rutile
87%
Talc
76%
Dehydration
50%
Mineral
23%
Amount
12%