Titlebook: Copahue Volcano; Franco Tassi,Orlando Vaselli,Alberto Tomas Caselli Book 2016 Springer-Verlag Berlin Heidelberg 2016 Copahue Volcano.Early

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Copahue Volcano and Its Regional Magmatic Settingry mantle environment, with melting of a subducted sediment residue. The back arc basalts show a wide variation in isotopic composition, have similar water contents as the Copahue magmas and show evidence for a subducted sedimentary component in their source regions. The low .Pb/.Pb of some backarc

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Geochemistry of the Magmatic-Hydrothermal Fluid Reservoir of Copahue Volcano (Argentina): Insights ftal source for CO. and N.. Gas discharges of the northern sector of the volcanic edifice are likely produced by mixing of hydrothermal gases with fluids from a shallow source permeating through the local fault systems. Gas geothermometry based on chemical reactions characterized by slow kinetics, su

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Acid Rivers and Lakes at Caviahue-Copahue Volcano as Potential Terrestrial Analogues for Aqueous Palrio) have abundant deposits of ferricrete since 2003: hydrous ferric oxides and schwertmannite occur, their precipitation being mediated by Fe-oxidizing bacteria and photochemical processes. Further downstream, at greater degrees of dilution, hydrous aluminum oxides and sulfates form and create ‘alc

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2195-3589 as health therapies and geothermal energy exploitation. .In a special section, the Copahue volcano is presented as a terrestrial modern analog for early-Earth and Mars environments.978-3-662-51156-5978-3-662-48005-2Series ISSN 2195-3589 Series E-ISSN 2195-7029

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The Economic Crisis in Ethiopia,occurred with emission of a low amount of material mainly constituted by rocks from the volcanic conduit and sediments from the bottom of the crater lake. Seismic activity and degassing continued until December 22nd when the eruption started with an opening phreatic event that rapidly evolved to a phreatomagmatic, and finally a magmatic eruption.

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