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- W2187766602 abstract "AssrRAcr Three hundred and ninety inclusions from the igneous sublayer of the Sudbury Igneous Complex have been examined, and many of them analyzed by microprobe. The 264 samples from the Strathcona mine of the North Range vary from dunite through harzburgite, wehrlite and clinop;roxenite to norite and gabbro, whereas the 126 samples from mines of the South Range include only rock types vdth onhopyroxene dominant, such as harzburgite and melanorite. The texture of the rocks ranges from that of a well-developed adcumulate, mesocumulate or orthocumulate to an extensively granulated and recrystallized fabric. On both the North and South Ranges, olivine varies from 85 to 73 mole Vo Fo, hypersthene from 13.5 to 31 mole 9o Fs, augite from 5 to 15 mole go Fs, plagioclase (including both cumulus and intercumulus phases) from 90 to 30 mole 9o An, and chromite contains up to 50.8 wr. u/o Cr2O3. The textures, presence of plagioclase and evidence of olivine reacting to give orthopyroxene suggest that the inclusions crystallized at crustal pressures. The range of rock types and the observed correlation of increasing MgO/(MgO+FeO) ratio in mafic minerals wittr increasing content of mafic minerals in the host rocks suggest strongly that these rocks are derived from one (or more than one) hidden layered intrusive bodies. Our data do not allow us to state that this intrusive body is cogenetic with the Sudbury norite, but they are consistent with this interpretation." @default.
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- W2187766602 date "1984-02-01" @default.
- W2187766602 modified "2023-09-23" @default.
- W2187766602 title "Mafic and ultramafic inclusions in the sublayer of the Sudbury igneous complex" @default.
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