High‐grade metamorphism and partial melting of basic and intermediate rocks
Rocks of basic and intermediate bulk composition occur in orogenic terranes from all geological time periods and are thought to represent significant petrological components of the middle and lower continental crust. However, the former lack of appropriate thermodynamic models for silicate melt, amp...
Main Authors: | Palin, R, White, R, Green, E, Diener, J, Powell, R, Holland, T |
---|---|
Format: | Journal article |
Language: | English |
Published: |
Wiley
2016
|
Similar Items
-
High-grade metamorphism and partial melting in Archean composite grey gneiss complexes
by: White, R, et al.
Published: (2016) -
Activity-composition relations for the calculation of partial melting equilibria in metabasic rocks
by: Green, E, et al.
Published: (2016) -
Partial melting of metabasic rocks and the generation of tonalitic–trondhjemitic–granodioritic (TTG) crust in the Archaean: Constraints from phase equilibrium modelling
by: Palin, R, et al.
Published: (2016) -
New constraints on granulite facies metamorphism and melt production in the Lewisian Complex, northwest Scotland
by: Feisel, Y, et al.
Published: (2018) -
The spatial degree of chemical equilibrium in some high grade metamorphic rocks
by: Blackburn, William Howard
Published: (2010)