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handle: 10261/23444
El estudio de rocas andesíticas de la Isla King George (Archipiélago de las Shetland del Sur, Antártida) pone de manifiesto la existencia de procesos de alteración hidrotermal con la formación de minerales zeolíticos secundarios pertenecientes a asociaciones de baja temperatura. Se han identificado dos paragénesis (Esmectitas-Bytownita-Mordenita, Esmectitas-AlbitaLaumontita) que reflejan distintas condiciones durante la alteración hidrotermal de dichas rocas andesíticas.
Atmospheric Science, andesites, andesitas, zeolites, Tectonic and Geochronological Evolution of Orogens, Oceanography, zeolitas, Paleoredox and Paleoproductivity Proxies, Alterations, hydrothermal alteration, Alteración, QE1-996.5, alteración hidrotermal, Paleontology, Geology, FOS: Earth and related environmental sciences, Hydrothermal, Granitic Rocks, Earth and Planetary Sciences, Shetland, Geophysics, Climate Change and Paleoclimatology, Geochemistry, Zeolitas, Andesites, Physical Sciences, Zeolites, Paragenesis, Andesitas, Hidrotermal, Metamorphic rock
Atmospheric Science, andesites, andesitas, zeolites, Tectonic and Geochronological Evolution of Orogens, Oceanography, zeolitas, Paleoredox and Paleoproductivity Proxies, Alterations, hydrothermal alteration, Alteración, QE1-996.5, alteración hidrotermal, Paleontology, Geology, FOS: Earth and related environmental sciences, Hydrothermal, Granitic Rocks, Earth and Planetary Sciences, Shetland, Geophysics, Climate Change and Paleoclimatology, Geochemistry, Zeolitas, Andesites, Physical Sciences, Zeolites, Paragenesis, Andesitas, Hidrotermal, Metamorphic rock
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