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- W2041003261 abstract "Abstract A local area of the Kap Edvard Holm Upper Layered Series gabbro has been converted into a quartz-albite-epidote ilmenite rock by leaching of iron and with a net mass loss. Among the textural changes is the dissolution of the magnetite matrix of magnetite-ilmenite lamellar intergrowths. This is an extreme example of a series of low-temperature changes occurring throughout the intrusion due to the reaction of the gabbro with a volatile-rich phase which separated during the magmatic stage and remained trapped within the walls of the intrusion. The Fe-rich fluid formed by this autometasomatic process is similar to those responsible for the genesis of Cornwall-type magnetite deposits. The probable temperature range for the process is 400–550°C." @default.
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- W2041003261 date "1982-01-01" @default.
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- W2041003261 title "Autometasomatic alteration of gabbro, Kap Edvard Holm intrusive complex, East Greenland" @default.
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- W2041003261 doi "https://doi.org/10.1180/minmag.1982.045.337.25" @default.
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