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- W2056957689 abstract "Textures and compositional relationships associated with dark-colored, fine-grained enclaves in the Cadillac Mountain and Somesville granites, Mount Desert Island, Maine, preserve abundant evidence for contamination of host granitic magmas by enclave liquids. Fine-grained enclaves, which apparently represent chilled magmatic droplets, have affected the composition and texture of the host granites by three possible mechanisms: (1) crystallization of feldspar-quartz-hornblende pegmatite pods from fluids of enclave origin in the granite surrounding enclaves, and the disaggregation of the pods and dispersion of crystals into the granite; (2) ionic exchange between enclaves and granitic magmas; (3) the generation around enclaves of rinds consisting of an inner alkali feldspar-quartz zone and an outer zone of hornblende-enriched granite. Coarse-grained pegmatite pods that occur outside of enclaves may result from migration of a hydrous residual fluid, evolved during enclave crystallization, out of the enclave, ..." @default.
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- W2056957689 date "1992-07-01" @default.
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- W2056957689 title "Effects of Magma Mingling in the Granites of Mount Desert Island, Maine" @default.
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- W2056957689 doi "https://doi.org/10.1086/629594" @default.
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