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1.Csongor, É, Hertelendi, E. 1986. Low-level counting facility for 14C dating. Nuclear Instruments and Methods in Physics ResearchB 17:493–5.Google Scholar
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19.Figler, A, Bartosiewicz, L, Füleky, Gy, Hertelendi, E. 1997. Copper age settlement and the Danube water System: a case study from North-Western Hungary. In: Chapman, C, Dolukhanov, P, editors. Landscapes in Flux Central and Eastern Europe in Antiquity.Oxford: Oxbow Books. p 209–30.Google Scholar
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21.Sümegi, P, Hertelendi, E. 1998. Reconstruction of microenvironmental changes in Kopasz hill loess area at Tokaj (Hungary) between 15 and 70 ka BP. Radiocarbon40(2):855–65.Google Scholar
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23.Gyulai, J, Hertelendi, E, Szabo, I. 1992. Plant remains from the early medieval lakeshore settlement Fonyód-Bélatelep (Lake Balaton, Hungary) with especial emphasis on the history of fruit cultivation in Pannonia. Vegetation history and archaeobotany1:177–81.CrossRefGoogle Scholar
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24.Hertelendi, E, Vető, I. 1989. Isotopically light aquatic kerogen in the Hungarian Oligocene. In: Wanda, U, Strauch, G, editors. 5th Working Meeting Isotopes in Nature; 1989 Sept; Leipzig. Leipzig: Academy of Sciences of the GDR, Central Institute of Isotope and Radiation Research. p 311–4.Google Scholar
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27.Kertész, R, Sümegi, P, Kozák, M, Braun, M, Félegyházi, E, Hertelendi, E. 1993. Archeological and paleoecological study of an early Holocene settlement in the Jászság area (Jászberény I). Communications from the Deparment of Mineralogy and Geology of Kossuth Lajos University. Acta Geographica Debrecina32:5–16.Google Scholar
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31.Hertelendi, E, Svingor, É, Futó, I, Szántó, Zs, Rank, D. 1997. Isotope Investigation of Lake Vrana and Springs in the Kvarner Area. Rapid Communication in Mass Spectrometry11:651–5.3.0.CO;2-G>CrossRefGoogle Scholar
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32.Lóki, J, Hertelendi, E, Borsy, Z. 1994. New dating of blown sand movement in the Nyírség. Communications from the Geographical Institute of the Kossuth Lajos University of Debrecen188:67–78.Google Scholar
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33.Hertelendi, E, Vető, I. 1991. The marine photosyntetic carbon isotopic fractionation remained constant during the Early Oligocene. Palaeogeography, Palaeoclimatology, Palaeoecology83:333–9.Google Scholar
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34.Vető, I, Demény, A, Hertelendi, E, Hetényi, M. 1997. Estimation of primary productivity in the Toarcian Tethys – a novel approach based on TOC, reduced sulphur and manganese contents. Palaeogeography, Palaeoclimatology, Palaeoecology132:355–71.CrossRefGoogle Scholar
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35.Hertelendi, E, Csongor, É. 1982. Athropogenic 14C excess in the troposphere between 1951 and 1978 measured in tree rings. Radiochemical and Radioanalytical Letters56:103–5.Google Scholar
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36.Vető, I, Hertelendi, E, Sajgó, Cs. 1999. A. Brukner-Wein: Upward increase of kerogen δ13C in the Peru Margin Upper Oligocene: possible implications for the Cenozoic evolution of atmospheric CO2. Palaeogeography, Palaeoclimatology, Palaeoecology145:33–42.Google Scholar
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37.Hertelendi, E. 1998. Radiometric methods for dating groundwater. In: Vértes, A, Nagy, S, Süvegh, K, editors. Nuclear methods in mineralogy and geology: techniques and applications.New York and London: Plenum Press. p 425–52.Google Scholar
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39.Csongor, É, Hertelendi, E. 1982. Fission products and radiocarbon as environmental pollutants due to atmospheric nuclear weapon tests measured in Debrecen since 1952. Atomki Közlemények24: 179–82.Google Scholar
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40.Uchrin, G, Ormai, P, Hertelendi, E. 1989. Local and global impact of tritium and carbon-14 released from Paks Nuclear Power Plant. In: Minkovic, MM, Pavlovic, RS, Raicevic, JJ, editors. Proceedings of the 30th anniversary symposium of radiation protection in the Boris Kidric Institute of Nuclear Science, radiation protection selected topics.Belgrade: Boris Kidric Institute. p 358–67.Google Scholar
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41.Hertelendi, E, Uchrin, G, Ormai, P. 1989. 14C release in various chemical forms with gaseous effluents from Paks Nuclear Power Plant. Radiocarbon31(3):154–60.Google Scholar
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44.Uchrin, G, Hertelendi, E, Volent, G, Slavik, O, Morávek, J, Kobal, I, Vokal, B. 1998. 14C measurements at PWR type nuclear power plants in three Middle European countries. Radiocarbon40(2):439–47.Google Scholar