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231
Pa excesses in arc volcanic rocks: Constraint on melting rates at convergent margins
Fang Huang
,
Craig C. Lundstrom
Earth Science and Environmental Change
Center for Latin American and Caribbean Studies
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231
Pa excesses in arc volcanic rocks: Constraint on melting rates at convergent margins'. Together they form a unique fingerprint.
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Keyphrases
235U
100%
Melting Rate
100%
Convergent Margin
100%
Arc Volcanic Rocks
100%
Convergence Rate
50%
Subducting Slab
50%
Subduction Rate
50%
Margin Setting
50%
Kick'em Jenny
50%
Lesser Antilles
50%
Physical Model
25%
Flow Velocity
25%
Self-consistent Model
25%
Linear Function
25%
Disequilibrium
25%
Flow Dynamics
25%
Geophysical Modeling
25%
238U
25%
Mantle Melting
25%
230Th
25%
Lava
25%
Melting Model
25%
Melt Generation
25%
226Ra
25%
U-series Disequilibria
25%
Dynamic Melting
25%
Flow Flux
25%
Reactive Porous Flow
25%
Geochemical Model
25%
Submarine Volcano
25%
Corner Flow
25%
Arc Setting
25%
Flux Melting
25%
Earth and Planetary Sciences
Convergent Margin
100%
Volcanic Rock
100%
Lesser Antilles
50%
Flow Velocity
25%
Submarine Volcano
25%
Corner Flow
25%
Porosity
25%