Partial melting of metagreywacke: a calculated mineral equilibria study
Greywacke occurs in most regionally metamorphosed orogenic terranes, with depositional ages from Archean to recent. It is commonly the dominant siliciclastic rock type, many times more abundant than pelite. Using calculated pseudosections in the Na2O–CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O–TiO2–O system, the...
| Main Authors: | , , |
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| Format: | Journal Article |
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Wiley - Blackwell
2008
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| Online Access: | http://onlinelibrary.wiley.com/doi/10.1111/j.1525-1314.2008.00790.x/pdf http://hdl.handle.net/20.500.11937/39680 |