Clinopyroxene–Liquid Equilibria and Geothermobarometry in Natural and Experimental Tholeiites: the 2014–2015 Holuhraun Eruption, Iceland [PDF]
Clinopyroxene–liquid geothermobarometry is a widely used tool for estimating the conditions under which mafic magmas are stored before they erupt. However, redox variability, sector zoning and disequilibrium crystallisation present major challenges to ...
Maren Kahl, David A. Neave, Eniko Bali
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GARNET-ORTHOPYROXENE AND GARNET-AMPHIBOLE GEOTHERMOBAROMETRY: EXPERIMENTAL DATA AND THERMODYNAMICS
International Geology Review, 1990L L Perchuk
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Elastic geothermobarometry on multiple inclusions in a single host
2020<p>The characterization of the pressure and temperature (P-T) histories of subducted rocks is of key importance to unravel geological processes at all scales. Conventional element-exchange geothermobarometers are challenged in ultra-high-pressure metamorphic terranes as the subduction temperatures may exceed their closure ...
Mattia Gilio +3 more
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Geothermobarometry of the Central Crystallines from the Garhwal Himalaya
Journal Geological Society of India, 1988Abstract Pelitic schists, gneisses and amphibolites from the Central Crystallines of the Garhwal Himalaya display evidence of multiple deformation (D1, D2 and D3) and polymetamorphism (M1, M2 and M3)' During the M1 episode of regional metamorphism which represents a thermal peak, the pelitic schists and gneisses developed the assemblage:
V. K. Gairola, D. Ackermand
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SCG: A Computer Applicationfor Single Clinopyroxene Geothermobarometry
Italian Journal of Geosciences, 2014SCG stands for Single Clinopyroxene Geothermobarometry, a software application for clinopyroxene geothermobarometry introduced here for the first time to the scientific community along with an explanatory note. SCG is a highly specialised and user-friendly application.
Sayari, Mohammad, Sharifi, Mortaza
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An analysis of uncertainty in non‐equilibrium and equilibrium geothermobarometry
Journal of Metamorphic Geology, 2004AbstractIn statistically optimised P–T estimation, the contributions to overall uncertainty from different sources are represented by ellipses. One source, for a diffusion‐controlled reaction at non‐equilibrium, is diffusion modelling of the reaction texture.
J. R. ASHWORTH +3 more
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Geothermobarometry of high-grade metapelites: simultaneously operating reactions
Geological Society, London, Special Publications, 1989Summary Experimental data on equilibria involving rock-forming minerals in high-grade metapelites (garnet, orthopyroxene, cordierite and plagioclase) have been used to derive an internally consistent system of mineralogical thermometers and barometers based on component reactions and excess mixing properties of solid solutions ...
L. Ya. Aranovich, K. K. Podlesskii
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Metapelitic Garnet-Muscovite-Al2SiO5-Quartz (GMAQ) Geothermobarometry
Journal of Earth Science, 2018The garnet-muscovite geothermometer and garnet-muscovite-Al2SiO5-quartz (GMAQ) geobarometer have been empirically calibrated under P-T conditions of 1–12 kbar and 460–760 oC using natural metapelitic rocks. The chemical compositions of the calibrant muscovite are in the ranges of Fe=0.03–0.21 atoms, Mg=0.02–0.32 atoms and AlVI=1.62–1.96 atoms ...
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Geothermobarometry of Al2SiO5-bearing metapelites in the western Austroalpine �tztal-basement
Mineralogy and Petrology, 1996The dominant amphibolite-facies Variscan event in the Austroalpine Otztal basement can best be studied in the northwestern part of the Otztal block. Further to the southeast it is overprinted by Alpine metamorphism. Metapelites with the assemblage garnet-staurolite-kyanite-sillimanite±andalusite-biotite-muscovite-plagioclase were used to reconstruct ...
P. Tropper, G. Hoinkes
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Geothermometry and geobarometry of orthogneisses and metasediments across the Pikwitonei granulite facies domain of central Manitoba shows an increase of paleopressure from about 6 kbar near the orthopyroxene isograd on the east to 12 kbar near the western boundary against the Thompson Nickel Belt.
A. Dog̃an Paktunc, Alec J. Baer
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