Isotope disequilibrium studies and magmatic processes
Subsurface crystallisation and degassing significantly influence the evolution and eruption of magmas. Both processes are inevitable consequences of the residence of magma in shallow reservoirs, and both obscure the nature of the pristine liquids derived from the melting region. However, the signatu...
Main Author: | Pyle, D |
---|---|
Format: | Journal article |
Language: | English |
Published: |
1994
|
Similar Items
-
Silicon isotopes and magmatic evolution
by: Savage, P, et al.
Published: (2010) -
Silicon isotope fractionation during magmatic differentiation
by: Savage, P, et al.
Published: (2011) -
Rhenium elemental and isotopic variations at magmatic temperatures
by: Wan, W, et al.
Published: (2024) -
Nickel Isotope Fractionation During Magmatic Differentiation
by: Xi‐Ming Yang, et al.
Published: (2023-06-01) -
Oxygen isotope composition of waters recorded in carbonates in strong clumped and oxygen isotopic disequilibrium
by: C. Thaler, et al.
Published: (2020-04-01)