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

Research output: Contribution to journal › Article › peer-review

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.",

author = "Jansen, \{J. Ben H.\} and \{van de Kraats\}, \{Anton H.\} and \{van der Rijst\}, Henk and Schulung, \{Roelof D.\}",

year = "1978",

month = oct,

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T1 - Metamorphism of siliceous dolomites at Naxos, Greece

AU - Jansen, J. Ben H.

AU - van de Kraats, Anton H.

AU - van der Rijst, Henk

AU - Schulung, Roelof D.

PY - 1978/10

Y1 - 1978/10

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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SN - 0010-7999

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SP - 279

EP - 288

JO - Contributions to Mineralogy and Petrology

JF - Contributions to Mineralogy and Petrology

IS - 3

ER -

Metamorphism of siliceous dolomites at Naxos, Greece

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