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...
Autori principali: | Palin, R, White, R, Green, E, Diener, J, Powell, R, Holland, T |
---|---|
Natura: | Journal article |
Lingua: | English |
Pubblicazione: |
Wiley
2016
|
Documenti analoghi
-
High-grade metamorphism and partial melting in Archean composite grey gneiss complexes
di: White, R, et al.
Pubblicazione: (2016) -
Activity-composition relations for the calculation of partial melting equilibria in metabasic rocks
di: Green, E, et al.
Pubblicazione: (2016) -
Partial melting of metabasic rocks and the generation of tonalitic–trondhjemitic–granodioritic (TTG) crust in the Archaean: Constraints from phase equilibrium modelling
di: Palin, R, et al.
Pubblicazione: (2016) -
New constraints on granulite facies metamorphism and melt production in the Lewisian Complex, northwest Scotland
di: Feisel, Y, et al.
Pubblicazione: (2018) -
The spatial degree of chemical equilibrium in some high grade metamorphic rocks
di: Blackburn, William Howard
Pubblicazione: (2010)