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We provide detailed\ninsight into the stable isotope distribution of carbonate minerals in a natural CO2 reservoir system from Mihályi-Répcelak area,\nNW-Hungary. Several types of measurements and calculations have been applied for the estimation of CO2 and H2O isotopic\ncomposition in equilibrium with dawsonite. The estimated G13C of CO2 exhibit values around -4.5 to -2.6 ‰ overlapping with\nassumed magmatic values and the presently measured gas data confirming magmatic origin, whereas we may assume that the\nwater present during carbonate formation likely had meteoric origin.\n© 2017 The Authors. 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[12] Baker JC, Bai GP, Hamilton J, Golding SD, Keene JK Continental-scale magmatic carbon dioxid seepage recorded by downso...", "listPosition" : 1, "published" : false, "snippet" : true } ], "hasCitationDuplums" : false, "inSelectedPubs" : "10073729", "userChangeableUntil" : "2017-10-26T09:18:44.000+0000", "publishDate" : "2017-09-04T13:11:23.000+0000", "directInstitutesForSort" : "Földtani és Geokémiai Intézet (HRN CSFK); Kőzettan-Geokémiai Tanszék (ELTE / TTK / Ft_K); Magyar Bányászati és Földtani Szolgálat", "ownerAuthorCount" : 6, "ownerInstituteCount" : 42, "directInstituteCount" : 3, "authorCount" : 6, "contributorCount" : 0, "hasQualityFactor" : false, "link" : "/api/publication/3262057", "label" : "Cseresznyés D et al. Stable Isotope Compositions of Different Mineral Phases Found in a Natural CO2-reservoir (NW-Hungary): Implication for their Origin. (2017) ENERGY PROCEDIA 1876-6102 114 2812-2818", "template" : "