Radon in the dry carbon dioxide spa of Mátraderecske, Hungary

1.Szabó, Á. (2005). Radioaktív ásványvizek és mofettagázok. Cluj-Napoca: Stúdium Könyvkiadó.SzabóÁ.2005Radioaktív ásványvizek és mofettagázokCluj-NapocaStúdium KönyvkiadóSearch in Google Scholar

2.Vásárhelyi, A., Hunyadi, I., Csige, I., Hakl, J., Hertelendi, E., Borossay, J., & Torkos, K. (1997). Radon enriched deep earth-gas upflow in a seismically active inhabited area. In H. S. Virk (Ed.), Rare gas geochemistry applications in earth & environmental sciences (pp. 211–233). Amritsar: Guru Nanak Dev University.VásárhelyiA.HunyadiI.CsigeI.HaklJ.HertelendiE.BorossayJ.TorkosK.1997Radon enriched deep earth-gas upflow in a seismically active inhabited areaVirkH. S.Rare gas geochemistry applications in earth & environmental sciences211233AmritsarGuru Nanak Dev UniversitySearch in Google Scholar

3.Pfanz, H., Yüce, G., D’Andria, F., D’Alessandro, W., Pfanz, B., Manetas, Y., & Papatheodorou, G. (2014). The ancient gates to hell and their relevance to geogenic CO₂. In P. Wexler (Ed.), History of toxicology and environmental health (pp. 92–117). Oxford: Elsevier Press.PfanzH.YüceG.D’AndriaF.D’AlessandroW.PfanzB.ManetasY.PapatheodorouG.2014The ancient gates to hell and their relevance to geogenic CO₂WexlerP.History of toxicology and environmental health92117OxfordElsevier Press10.1016/B978-0-12-800045-8.00011-3Search in Google Scholar

4.Ballagi, F. (1995). A szénsavgázfürdő jelentősége a perifériás érbetegek rehabilitációjában. Érbetegségek, 2(3), 21–27.BallagiF.1995A szénsavgázfürdő jelentősége a perifériás érbetegek rehabilitációjábanÉrbetegségek232127Search in Google Scholar

5.Szalainé, Cs. B., & Dózsa, Cs. (2011). A mofetta kezelés – a kiaknázatlan nemzeti kincs. IME, 10(1), 45–49.SzalainéCs. B.DózsaCs.2011A mofetta kezelés – a kiaknázatlan nemzeti kincsIME1014549Search in Google Scholar

6.Czakó, T., & Zelenka, T. (1981). New data about the neotectonics of Mátra Mountains, Northern Hungary. Adv. Space Res., 1(10), 289–298. 10.1016/0273-1177(81)90406-3.CzakóT.ZelenkaT.1981New data about the neotectonics of Mátra Mountains, Northern HungaryAdv. Space Res.11028929810.1016/0273-1177(81)90406-3Apri DOISearch in Google Scholar

7.Tóth, E., Boros, D., Samuelsson, L., Deák, F., Marx, G., & Sükösd, Cs. (1994). High radon activity in Northeast Hungary. Phys. Scr., 50(6), 726–730. 10.1088/0031-8949/50/6/020.TóthE.BorosD.SamuelssonL.DeákF.MarxG.SükösdCs.1994High radon activity in Northeast HungaryPhys. Scr.50672673010.1088/0031-8949/50/6/020Apri DOISearch in Google Scholar

8.Csige, I., & Csegzi, S. (2001). The Radamon radon detector and an example of application. Radiat. Meas., 34(1/6), 437–440. 10.1016/S1350-4487(01)00202-5.CsigeI.CsegziS.2001The Radamon radon detector and an example of applicationRadiat. Meas.341/643744010.1016/S1350-4487(01)00202-5Apri DOISearch in Google Scholar

9.Genrich, V. (1993). AlphaGUARD PQ2000/MC50. Multiparameter Radon Monitor. Characterisation of its physical properties under normal climatic and severe environmental conditions. User manual. Frankfurt, Germany: Genitron Instruments GmbH.GenrichV.1993AlphaGUARD PQ2000/MC50. Multiparameter Radon Monitor. Characterisation of its physical properties under normal climatic and severe environmental conditions. User manualFrankfurt, GermanyGenitron Instruments GmbHSearch in Google Scholar

10.Várhegyi, A., & Hakl, J. (1994). A silicon sensor based radon monitoring device and its use in environmental geophysics. Geophys. Trans., 39(4), 289–302.VárhegyiA.HaklJ.1994A silicon sensor based radon monitoring device and its use in environmental geophysicsGeophys. Trans.394289302Search in Google Scholar