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- W2068508731 abstract "Abstract The syn-Caledonian Pollen Carbonatite was emplaced into gabbroic cumulates, which were subsequently fenitized to ultrabasic rocks containing ferroan pargasite, augite or salite, biotite, apatite and variable amounts of calcite. The metasomatism took place in two stages. The initial fenitization led to the introduction of Ti, Fe2+, Fe3+, K, Mn, Co, Zn, Zr, Nb, Ba, La, Ce and Nd, and the abstraction of Al, Ni, Cu and Sr. The later carbonatization involved the addition of Ca, C, P, Sr, Y, Ba, La and Nd, removal of Si, Al, Mg, Na, Fe, Ti, Mn, K, V, Cr, Co, Ni and Zn, and the oxidation of Fe2+ to Fe3+. Extreme carbonatization resulted in fenites chemically indistinguishable from silicocarbonatitic facies of the magmatic carbonatite. The course of the infiltration metasomatism is deduced to have been controlled by the changing phase relations in a volatile-saturated carbonatite magma." @default.
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- W2068508731 date "1983-06-01" @default.
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- W2068508731 title "The geology, geochemistry and origin of ultrabasic fenites associated with the Pollen Carbonatite (Finnmark, Norway)" @default.
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- W2068508731 doi "https://doi.org/10.1016/0009-2541(83)90092-x" @default.
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