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Andó J 1995: Complementary environmental classifying and environ-technological basic research on waste of Metallochemia premises and its surroundings (in Hungarian). Manuscript, p. 101

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J.P. Chiles 2003 A hybrid approach for addressing uncertainty in risk assessments Journal of Environmental Engineering 129 68

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1998 Stable isotopes and heavy metal distribution in Dreissena polymorpha (zebra mussels) from western basin of Lake Erie, Canada Environmental Geology 33 122 142

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Environmental Medicine. US Department of Health and Human Services, Atlanta Asbestos Toxicity, Case Studies in Environmental Medicine 1997

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Environmental Magnetism George Allen and Unwin London . J Zan X Fang J

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Central European Geology
Authors: Tamás Madarász, Péter Szűcs, Balázs Kovács, László Lénárt, Zoltán Fejes, Andrea Kolencsik-Tóth, István Székely, László Kompár, and Imre Gombkötő

Conference for Environmental Sciences, Cluj, Romania . (in Hungarian)

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Central European Geology
Authors: Ádám Bede, Roderick B. Salisbury, András István Csathó, Péter Czukor, Dávid Gergely Páll, Gábor Szilágyi, and Pál Sümegi

Studies. An Environmental and Archaeological Multiproxy Study of Burial Mounds in the Eurasian Steppe Zone . British Archaeological Reports, International Series 2238, Archaeopress , Oxford , pp. 71 – 131

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: Isotope and water chemistry in sulfide-bearing springs of central Italy . — In: Interpretation of Environmental Isotope and Hydrochemical Data in Groundwater Hydrology . IAEA editor, Vienna, pp. 143 – 158

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Central European Geology
Authors: István Marsi, Ildikó Selmeczi, László Koloszár, József Vatai, Ildikó Szentpétery, Árpád Magyari, and László Róth

Abstract

The authors carried out geologic investigations in the Kolontár area in connection with the red mud catastrophe of 4 October 2010, and have acquired more detailed knowledge using geologic mapping methods. This study is an evaluation on the basis of the immediate analyses that were made after the accident and are published in this paper.

Based on their research results the authors find that the alluvial deposits of the Torna Brook are highly inhomogeneous, which is manifested in the variability of stability and bearing capacity. Based on the morphology in the area of Kolontár a small, rhombus-shaped pull-apart basin can be outlined, which can be interpreted as a neotectonic event characterized by a right-lateral fault. However, further detailed research is needed in order to understand what kind of role the geologic environment played in the development of the situation that led to the dam failure.

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