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Metamorphism of siliceous dolomites at Naxos, Greece (1978)

Jansen, J. Ben H. ; Kraats, Anton H. ; Rijst, Henk ; [weitere]

Springer

Contributions to mineralogy and petrology 67 (1978), S. 279-288

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Details

ISSN: 1432-0967

Quelle: Springer Online Journal Archives 1860-2000

Thema: Geologie und Paläontologie

Notizen: Abstract Siliceous dolomitic marbles at Naxos, Greece, are crystallized in a range of metamorphic temperatures, estimated from 350 to 700 °C and a total pressure of about 6 kb. A number of low variant assemblages of this rock-system have been studied. The sequence of these metamorphic assemblages is a function of increasing metamorphism, and this is in agreement with other fielddata and with experimental data for the chemical system CaO-MgO-SiO2-H2O-CO2 (-HF). The composition of the associated fluid inclusions may be considered reasonably correct in the light of experimentally obtained X CO2 values for the mineral equilibria, extrapolated for a total pressure of about 6 kb at the interpolated temperatures at the sample locations.

Materialart: Digitale Medien

URL: http://dx.doi.org/10.1007/BF00381455

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