@article{MTMT:2919939, title = {AZ ATR FTIR spektrometria gyakorlati alkalmazása néhány - elsősorban földtani - esettanulmány bemutatásával}, url = {https://m2.mtmt.hu/api/publication/2919939}, author = {Kovács, István János and Udvardi, Beatrix and Falus, György and Földvári, M and Fancsik, Tamás and Kónya, Péter and Bodor, Emese Réka and Mihály, Judith and Németh, Csaba and Czirják, G and Ősi, Attila and Vargáné, Barna Zs and Bhattoa Harjit, Pál and Szekanecz, Zoltán and Turza, S}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {145}, unique-id = {2919939}, issn = {0015-542X}, keywords = {ásványok rezgési spektrometriája; gyengített teljes reflexió; Fourier-transzformációs infravörös spektrometria; földtan}, year = {2015}, eissn = {2559-902X}, pages = {173-192}, orcid-numbers = {Kovács, István János/0000-0002-3488-3716; Bodor, Emese Réka/0000-0003-3894-2506; Ősi, Attila/0000-0003-2967-997X; Bhattoa Harjit, Pál/0000-0002-4909-0065} } @article{MTMT:2814679, title = {Csátalja, the largest H4-5 chondrite from Hungary}, url = {https://m2.mtmt.hu/api/publication/2814679}, author = {Kovács, János and Sajó, István and Márton, Zsuzsanna and Jáger, Viktor and Hegedüs, Tibor and Berecz, Tibor and Tóth, Tamás Ferenc and Gyenizse, Péter and Podobni, András}, doi = {10.1016/j.pss.2014.11.009}, journal-iso = {PLANET SPACE SCI}, journal = {PLANETARY AND SPACE SCIENCE}, volume = {105}, unique-id = {2814679}, issn = {0032-0633}, abstract = {We report here for the first time the composition and mineralogical studies on a new meteorite, which was found in August 2012 near the village of Csátalja, Hungary (46°0'21-N; 18°59'27'E). The Csátalja meteorite is classified as a H4-5 ordinary chondrite with shock stage S2 and a degree of weathering W1 and the total mass is 15 kg. The Csátalja meteorite is characterized by well-defined chondrules composed either of olivine or pyroxene. X-ray diffractogram shows the primary phases olivine, pyroxene, kamacite, and albite. Metal particles were extracted from the bulk powdered samples exhibit only kamacite and small amounts of the intergrowth taenite/kamacite. Raman spectra of forsterite indicate that Csátalja meteorite suffered from relatively low shock pressure regime. The texture of chondrules varies from nonporphyritic (e.g., barred olivine, radial pyroxene) to porphyritic ones (e.g., granular olivine as well as olivine pyroxene). The meteorite name has not yet approved by the Nomenclature Committee of the Meteoritical Society.}, keywords = {Silicate minerals; olivine; Nanocrystalline materials; Cesium; Hungarians; EBSD; LIBS; Micro-Raman; METEORITES; weathering; ORDINARY CHONDRITES; Csátalja; Ordinary chondrite; Hungarian meteorite}, year = {2015}, eissn = {1873-5088}, pages = {94-100}, orcid-numbers = {Kovács, János/0000-0001-7742-5515; Sajó, István/0000-0002-1228-1407; Márton, Zsuzsanna/0000-0001-7625-3571; Jáger, Viktor/0000-0003-1283-5198; Berecz, Tibor/0000-0001-9632-8120; Gyenizse, Péter/0000-0002-8175-9734} } @article{MTMT:2759264, title = {Application of attenuated total reflectance Fourier transform infrared spectroscopy in the mineralogical study of a landslide area, Hungary}, url = {https://m2.mtmt.hu/api/publication/2759264}, author = {Udvardi, Beatrix and Kovács, István János and Kónya, Péter and Földvári, M and Füri, Judit Izabella and Budai, F and Falus, György and Fancsik, Tamás and Szabó, Csaba and Szalai, Zoltán and Mihály, Judith}, doi = {10.1016/j.sedgeo.2014.08.005}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {313}, unique-id = {2759264}, issn = {0037-0738}, abstract = {This study demonstrates that the unpolarized attenuated total reflectance Fourier transform infrared spectroscopy (ATR FTIR) is a practical and quick tool to distinguish different types of sediments in landslide-affected areas, and potentially other types of physical environments too. Identification and quantification of minerals by ATR FTIR is implemented on a set of powdered natural sediments from a loess landslide (Kulcs, Hungary). A protocol including sample preparation, analytical conditions and evaluation of sediment ATR spectra is outlined in order to identify and estimate major minerals in sediments. The comparison of the defined FTIR parameters against qualitative and quantitative results of X-ray diffraction and thermal analysis was used to validate the use of ATR FTIR spectroscopy for the considered sediments. The infrared band areas and their ratios (water/carbonates; silicates/carbonates; kaolinite) appear to be the most sensitive parameters to identify strongly weathered sediments such as paleosols and red clays which most likely facilitate sliding and could form sliding zones. The effect of grain size and orientation of anisotropic minerals on the wave number and intensity of some major absorption bands is also discussed.}, keywords = {Hungary; SEDIMENTS; grain size; landslides; ATR FTIR; landslide; Attenuated total reflectance Fourier transform infrared spectroscopy; Landslide areas; Anisotropy of calcite}, year = {2014}, eissn = {1879-0968}, pages = {1-14}, orcid-numbers = {Kovács, István János/0000-0002-3488-3716; Szabó, Csaba/0000-0002-1580-6344; Szalai, Zoltán/0000-0001-5267-411X} } @article{MTMT:2473699, title = {Short Pressure Pulse Originated Shock Vein in NWA-4383 S4 Stage Ordinary Chondrite}, url = {https://m2.mtmt.hu/api/publication/2473699}, author = {Bencsik, Attila and Fintor, Krisztián and Nagy, Sz and Pál-Molnár, Elemér and Gyollai, Ildikó}, journal-iso = {METEORIT PLANET SCI}, journal = {METEORITICS & PLANETARY SCIENCE}, volume = {48}, unique-id = {2473699}, issn = {1086-9379}, year = {2013}, eissn = {1945-5100}, pages = {A54-A54}, orcid-numbers = {Fintor, Krisztián/0000-0003-4794-9419; Pál-Molnár, Elemér/0000-0002-9606-0133; Gyollai, Ildikó/0000-0001-8576-0196} }