Metamorphism of siliceous dolomites at Naxos, Greece

J. Ben H. Jansen; Anton H. van de Kraats; Henk van der Rijst; Roelof D. Schulung

doi:10.1007/BF00381455

Metamorphism of siliceous dolomites at Naxos, Greece

J. Ben H. Jansen, Anton H. van de Kraats, Henk van der Rijst, Roelof D. Schulung

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17 Scopus citations

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.

Original language	English
Pages (from-to)	279-288
Number of pages	10
Journal	Contributions to Mineralogy and Petrology
Volume	67
Issue number	3
DOIs	https://doi.org/10.1007/BF00381455
State	Published - Oct 1978
Externally published	Yes

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title = "Metamorphism of siliceous dolomites at Naxos, Greece",

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 XCO2 values for the mineral equilibria, extrapolated for a total pressure of about 6 kb at the interpolated temperatures at the sample locations.",

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year = "1978",

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AU - Jansen, J. Ben H.

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AU - van der Rijst, Henk

AU - Schulung, Roelof D.

PY - 1978/10

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N2 - 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 XCO2 values for the mineral equilibria, extrapolated for a total pressure of about 6 kb at the interpolated temperatures at the sample locations.

AB - 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 XCO2 values for the mineral equilibria, extrapolated for a total pressure of about 6 kb at the interpolated temperatures at the sample locations.

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JO - Contributions to Mineralogy and Petrology

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ER -

Metamorphism of siliceous dolomites at Naxos, Greece

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