Search results for " Thermal springs"

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Regional variations in the chemical and helium–carbon isotope composition of geothermal fluids across Tunisia

2011

Abstract Tunisia has numerous thermo-mineral springs. Previous studies have shown that their chemical composition and occurrence are strongly influenced by the regional geology. However little work has been done so far to study the isotopic composition of volatiles associated with these geothermal manifestations. Here, we report on the results of an extensive survey of both natural hot springs and production wells across Tunisia, aimed at investigating the spatial distribution of thermal fluids' geochemical characteristics and He–C isotopic composition. The chemistry of the analyzed samples highlights the heterogeneity of the water mineralization processes in Tunisia, as a consequence of th…

Tunisia010504 meteorology & atmospheric sciencesEarth scienceGeochemistryAquiferengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)Geochemistry and PetrologyTunisia; Helium isotopes; Carbon isotopes; Geothermal fluids; Groundwaters; Thermal springs[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentGroundwaterChemical compositionGeothermal gradientComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_categoryRiftCarbon isotopeThermal springsGeologyHelium isotopeSettore GEO/08 - Geochimica E Vulcanologia13. Climate actionIsotopes of carbonMagmatismengineeringHaliteGeothermal fluidGeologyChemical Geology
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CO2 release to the atmosphere from thermal springs of Sperchios Basin and northern Euboea (Greece): The contribution of “hidden” degassing

2020

Abstract Greece is a region characterised by intense geodynamic activity that favours the circulation of hydrothermal fluids in the crust transporting volatiles from either the deep crust or the mantle to the surface. Elevated heat flow values are detectable at Sperchios Basin and North Euboea (central Greece), two areas defined by a system of deeply rooted extensional faults and Quaternary volcanic activity. This setting contributed to the formation of numerous hydrothermal systems, which are mostly expressed as CO2-rich thermal springs with intense bubbling. The CO2 output from six bubbling pools has been determined by flux measurements with the use of the floating chamber method. The hig…

geographygeography.geographical_feature_categoryVolcanic arcWater flowCarbonate mineralsCrust010501 environmental sciencesCarbon dioxide Degassing sources Thermal springs Greece010502 geochemistry & geophysics01 natural sciencesPollutionMantle (geology)Hydrothermal circulationSettore GEO/08 - Geochimica E Vulcanologiachemistry.chemical_compoundchemistryVolcanoGeochemistry and PetrologyEnvironmental ChemistryCarbonatePetrologyGeology0105 earth and related environmental sciences
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