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H
2
O-rich mantle melting near the slab–wedge interface
Timothy L. Grove,
Christy B. Till
Earth and Space Exploration, School of (SESE)
Research output
:
Contribution to journal
›
Article
›
peer-review
21
Scopus citations
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2
O-rich mantle melting near the slab–wedge interface'. Together they form a unique fingerprint.
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Physics & Astronomy
andesite
100%
Earth mantle
95%
magma
66%
melting
63%
garnets
39%
arcs
37%
wedges
35%
minerals
35%
silicates
34%
peridotite
31%
olivine
23%
solidus
23%
rutile
18%
alkalies
17%
eclogite
16%
liquids
14%
trace elements
11%
supercritical fluids
11%
sediments
10%
fluids
10%
budgets
9%
proportion
8%
field strength
7%
depletion
7%
rare earth elements
7%
silicon dioxide
6%
intervals
6%
temperature
2%
Earth & Environmental Sciences
melting
62%
mantle
59%
melt
59%
andesite
50%
lherzolite
38%
magma
31%
petrol
30%
garnet
29%
clinopyroxene
24%
subduction zone
23%
slab
21%
silicate melt
19%
mineral
17%
rutile
17%
orthopyroxene
17%
olivine
14%
liquid
14%
fluid
14%
rare earth element
13%
silicate
13%
harzburgite
9%
eclogite
8%
budget
6%
subduction
6%
silica
6%
trace element
6%
sediment
3%
experiment
3%
temperature
3%
rate
2%
effect
1%
Chemical Compounds
Melting
70%
Slab Like Crystal
34%
Mineral
32%
Solidus
29%
Rutile
19%
Alkali
16%
Liquid
16%
Supercritical Fluid
11%
Chemical Element
7%
Lanthanoid Atom
7%
Strength
6%
Pressure
5%
Amount
4%