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• W2023005834 abstract "Within the subsurface convective system which constitutes the thermomineral waters of which the meteoric origin is proved by the oxygen—deuterium couple, the associated gases, free or dissolved, may represent the only “juvenile” component in this cycle. The “juvenile” origin of the gases can be clearly established through ascertaining the isotopic composition of certain elements: argon, nitrogen, carbon and helium. The study of these gases associated with thermomineral waters has been undertaken systematically since 1976. One of the first objectives of these investigations has been the determination of the carbon isotopic compositions of the carbon dioxide—bicarbonate system for ∼50 thermomineral springs in various geological settings: the Massif Central, Pyrénées, and Vosges mountainous regions, France. On the basis of isotopic compositions, three sources of primordial or initial carbon have been put forward which correspond to characteristic figures for the carbon compositions expressed in δ13C-values. The exogenous carbon domain (δ13CCO2 from −10 to −25‰, δ13CHCO−3 from −18 to −2‰), the endogenous magmatic carbon domain (δ13CCO2 from −10 to −2‰, δ13CHCO−3 from −2 to +6‰) and the endogenous sedimentary carbon domain (δ13CCO2 from −2 to +2‰ and δ13CHCO−3 〉 + 6‰). In the case of springs with exogenous carbon of which a part is atmospheric, nitrogen isotopes confirm that origin. In the cases of springs with magmatic or mantle carbon, argon isotopes indicate also a deep origin." @default.
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• W2023005834 date "1982-03-01" @default.
• W2023005834 modified "2023-09-27" @default.
• W2023005834 title "Isotopic identification of gases of a deep origin in French thermomineral waters" @default.
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• W2023005834 doi "https://doi.org/10.1016/0022-1694(82)90053-1" @default.
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