Partial melting mechanisms of peraluminous felsic magmatism in a collisional orogen: an example from the Khondalite belt, North China craton
Sedimentary-derived (S-type) granites are an important product of orogenic metamorphism, and a range of subtypes can be recognized by differences in field occurrence, mineralogy and geochemistry. These subtypes can reflect variations of initial protolith composition, partial melting reactions, press...
| Autores principales: | , , , , , |
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| Formato: | Journal article |
| Lenguaje: | English |
| Publicado: |
Wiley
2024
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