Results 131 to 140 of about 180 (171)
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Journal of Metamorphic Geology, 2005
AbstractMetapelitic residual enclaves in the Neogene Volcanic Province of SE Spain are residues left after melt extraction. Glass (quenched melt) of granitic composition occurs as inclusions in most minerals and as intergranular pockets. The most common enclave types show one stage of garnet growth that is interpreted to have occurred at the same time ...
ALVAREZ VALERO A. M. +2 more
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AbstractMetapelitic residual enclaves in the Neogene Volcanic Province of SE Spain are residues left after melt extraction. Glass (quenched melt) of granitic composition occurs as inclusions in most minerals and as intergranular pockets. The most common enclave types show one stage of garnet growth that is interpreted to have occurred at the same time ...
ALVAREZ VALERO A. M. +2 more
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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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Mechanical behavior of frozen metapelite: Laboratory investigation and constitutive modeling
Cold Regions Science and Technology, 2020Hafssa Tounsi
exaly
The Petrogenetic Grid and Subfacies for Middle-temperature Metapelites
Journal of Petrology, 1977K. B. KEPEZHINSKAS, V. V. KHLESTOV
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THE BEHAVIOR OF GARNET IN METAPELITES DURING POLYMETAMORPHISM
International Geology Review, 1985openaire +1 more source