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- W2001269366 abstract "Abstract A group of small Ordovician-Silurian plutons was emplaced in the Tafi Megafracture of the Sierras Pampeanas, Argentina. These granites, with some peraluminous features, vary from types with andesine, biotite, magmatic epidote, and sometimes sphene, to other muscovitic types with albite and sometimes garnet (almandine-spessartite), reflecting a fractionated crystallization, with development of cumulates relatively rich in calcic-plagioclases, biotite, and epidote but poor in potast feldspar. The usual classification into I- and S-types is not adequate in these cases, as the final nature of the magma is notably affected by the factors that operate in the crystallization, especially the amount and the kind of volatiles." @default.
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- W2001269366 date "1989-01-01" @default.
- W2001269366 modified "2023-09-27" @default.
- W2001269366 title "Granitoids of the Tafi Megafracture (Sierras Pampeanas, Argentina): Petrogenetic implications" @default.
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- W2001269366 doi "https://doi.org/10.1016/0895-9811(89)90047-3" @default.
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