P_{CO_2 } -T-Evolution and origin of zoning in melilite during the regressive stage of contact metamorphism in carbonate-bearing rocks |
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Authors: | V. V. Reverdatto N. N. Pertsev V. N. Korolyuk |
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Affiliation: | (1) Institute of Geology and Geophysics of Siberian Branch of Academy of Sciences of the USSR, 630090 Novosibirsk 90, USSR;(2) Institute of Ore Geology, Petrography, Mineralogy, and Geochemistry of Academy of Sciences of the USSR, Staromonetniy 35, 109017 Moscow Zh-17, USSR |
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Abstract: | The article describes the thermal metamorphism of siliceous carbonate rocks near the dolerite intrusive body in Eastern Siberia. The mineral associations at the immediate contact with dolerite are the following: wollastonite+rankinite, rankinite+spurrite (+melilite?), spurrite+melilite+merwinite+calcite and merwinite+monticellite+melilite+calcite. The melilite in these associations is usually unzoned; its composition being essentially gehlenitic. During the regressive stage of contact metamorphism new akermanite-rich melilite and calcite were formed by replacement of merwinite and earlier gehlenitic melilite through participation of CO2. The newly forming melilite grains have sharp compositional zoning. The origin of zoning was connected with the fall of temperature and decrease of the mole fraction of CO2 in the fluid equilibrated with the minerals. |
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