@article{MTMT:34643332,
	title = {Iron-Bearing Minerals in the Boda Claystone Formation: Correspondences with Stages of Evolution Revealed by Mössbauer Spectroscopy},
	url = {https://m2.mtmt.hu/api/publication/34643332},
	author = {Lázár, Károly and Máthé, Z and Németh, Tibor and Kovácsné Kis, Viktória and Stichleutner, Sándor and Kovács, Ivett},
	doi = {10.3390/min14020196},
	journal-iso = {MINERALS-BASEL},
	journal = {MINERALS},
	volume = {14},
	unique-id = {34643332},
	year = {2024},
	eissn = {2075-163X},
	orcid-numbers = {Németh, Tibor/0000-0002-1836-6006; Kovács, Ivett/0000-0001-7015-7909}
}

@article{MTMT:34401167,
	title = {Continuous wavelet transformation to quantify small-scale cycles of petrophysical properties; a new approach applied in a potential disposal repository of nuclear waste, SW Hungary},
	url = {https://m2.mtmt.hu/api/publication/34401167},
	author = {Abutaha, Saja and Geiger, János and Fedor, F and Gulyás, Sándor},
	doi = {10.4154/gc.2023.11},
	journal-iso = {GEOL CROAT},
	journal = {GEOLOGIA CROATICA},
	volume = {76},
	unique-id = {34401167},
	issn = {1330-030X},
	abstract = {Continuous Wavelet Transformation (CWT) was applied to study the small-scale repetitive oscillations of porosity distribution patterns in a 5 m silty-claystone core sample of the Boda Claystone Formation. We handled the fluctuations in voxel porosity averages over unequal depth distributions as signals over uneven time intervals. The strength of wavelet analysis lies in the ability to study the fluctuation of a signal in detail, i.e., the wavelet transforms permit automatic localization of the cyclic attributes' sequences both in time (the depth domain) and according to their frequency (the frequency domain). Thereupon, three main frequency branches (cycles) were discerned: small scale (5, 6.67, and 11 cm), intermediate scale (20, 30 cm), and large scale (66.67 cm). Depending on the CWT coefficients magnitude plot, we were able to detect the developments of porosity oscillation according to the depth variable. Thus, small-scale cycles were seen throughout the core sample., the intermediate-scale cycles were strong in the upper parts of the core sample and dwindled toward greater depths, and the large cycle was predominant in the lower part of the core sample. The cross-correlation of the wavelet coefficients of porosity and rock-forming components allows a detailed study of the inter-dependence of such parameters as their relationship changes over time. The distinct peaks at zero lag indicates that the measured wavelet coefficient series were contemporaneously correlated; their strong positive correlations suggest that both examined series respond similarly and simultaneously to other exogenous factors. The results emphasize that cyclical porosity fluctuations at all scales would concern three main factors; sediment deposition, diagenetic processes, and structural deformation (i.e., convolute laminations).},
	year = {2023},
	eissn = {1333-4875},
	pages = {131-146},
	orcid-numbers = {Abutaha, Saja/0000-0001-8439-5895; Geiger, János/0000-0001-9359-5266; Gulyás, Sándor/0000-0002-3384-2381}
}

@article{MTMT:33832012,
	title = {Adsorption and diffusion of selenite on Boda Claystone Formation},
	url = {https://m2.mtmt.hu/api/publication/33832012},
	author = {Czömpöly, Ottó Sámuel and Fábián, Margit and Korányi, Tamás and Nagy, Gábor and Horváth, Zsolt Endre and Zizak, I. and Pollastri, S. and Aertsens, M. and Osán, János},
	doi = {10.1016/j.clay.2023.106997},
	journal-iso = {APPL CLAY SCI},
	journal = {APPLIED CLAY SCIENCE},
	volume = {241},
	unique-id = {33832012},
	issn = {0169-1317},
	year = {2023},
	eissn = {1872-9053},
	orcid-numbers = {Horváth, Zsolt Endre/0000-0002-4632-0136}
}

@article{MTMT:34151030,
	title = {Geochemical and Sedimentological Signatures of Ariyankuppam and Chunnambar Estuarine Sediments, Pondicherry, India: Implications on Weathering and Provenance},
	url = {https://m2.mtmt.hu/api/publication/34151030},
	author = {Kirubakaran, N. and Sridharan, M. and Senthil Nathan, D. and Rajamanickam, M. and Harikrishnan, S.},
	doi = {10.1007/s12594-023-2461-3},
	journal-iso = {J GEOL SOC INDIA},
	journal = {JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA},
	volume = {99},
	unique-id = {34151030},
	issn = {0016-7622},
	year = {2023},
	eissn = {0974-6889},
	pages = {1275-1284}
}

@article{MTMT:33698292,
	title = {Using geophysical log data to predict the fracture density in a claystone host rock for storing high-level nuclear waste},
	url = {https://m2.mtmt.hu/api/publication/33698292},
	author = {Tóth, Emese and Hrabovszki, Ervin and M. Tóth, Tivadar},
	doi = {10.1007/s40328-023-00407-w},
	journal-iso = {ACTA GEOD GEOPHYS},
	journal = {ACTA GEODAETICA ET GEOPHYSICA},
	volume = {58},
	unique-id = {33698292},
	issn = {2213-5812},
	abstract = {Previously drilled boreholes of a host rock for a potential nuclear waste repository in Hungary revealed a highly fractured claystone rock body. A crucial step for characterizing the hydrodynamic behavior of such a fractured reservoir is fracture identification and accurate calculation of the fracture density. Although acoustic borehole televiewers provide a reliable base for determining the fracture density, older boreholes usually lack such data. However, conventional borehole geophysical measurements are often accessible in such cases. The aim of this study was to identify any correlations between well log data and fracture density. Multiple linear regression analysis was performed on data from two boreholes penetrating the Boda Claystone Formation in southwest Hungary. The upper section of the BAF-4 borehole was used for training, where the fracture density was estimated with a fit of R 2  = 0.767. The computed regression function predicted the fracture density with high accuracy in both boreholes for all intervals with typical lithological features. However, in some sections where anomalous well log data indicated changes in the lithology, the prediction accuracy decreased. For example, the function underestimated the fracture density in sandy intervals.},
	year = {2023},
	eissn = {2213-5820},
	pages = {35-51},
	orcid-numbers = {Hrabovszki, Ervin/0000-0001-7914-6042; M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:32531014,
	title = {Geochemical and microtextural properties of veins in a potential high-level radioactive waste disposal site},
	url = {https://m2.mtmt.hu/api/publication/32531014},
	author = {Hrabovszki, Ervin and Tóth, Emese and M. Tóth, Tivadar and Garaguly, István and Futó, István and Máthé, Zoltán and Schubert, Félix},
	doi = {10.1016/j.jsg.2021.104490},
	journal-iso = {J STRUCT GEOL},
	journal = {JOURNAL OF STRUCTURAL GEOLOGY},
	volume = {154},
	unique-id = {32531014},
	issn = {0191-8141},
	year = {2022},
	eissn = {1873-1201},
	orcid-numbers = {Hrabovszki, Ervin/0000-0001-7914-6042; M. Tóth, Tivadar/0000-0003-1012-1095; Garaguly, István/0000-0002-2802-0738; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:32928316,
	title = {Calculating the representative elementary volume of porosity using X-ray computed tomography: Boda Claystone Formation core sample/Hungary},
	url = {https://m2.mtmt.hu/api/publication/32928316},
	author = {Abutaha, Saja and Geiger, János and Gulyás, Sándor and Fedor, Ferenc},
	journal-iso = {ACTA GEOL SLOV},
	journal = {ACTA GEOLOGICA SLOVACA},
	volume = {14},
	unique-id = {32928316},
	issn = {1338-0044},
	year = {2022},
	eissn = {1338-5674},
	pages = {25-36},
	orcid-numbers = {Abutaha, Saja/0000-0001-8439-5895; Geiger, János/0000-0001-9359-5266; Gulyás, Sándor/0000-0002-3384-2381}
}

@article{MTMT:32775770,
	title = {Influence of the Late Quaternary climate on sedimentology of the Jazmurian Playa, SE Iran},
	url = {https://m2.mtmt.hu/api/publication/32775770},
	author = {Sharifi-Yazdi, Masoud and Tavakoli, Vahid and Salehi-Noparvar, Sara and Vaezi, Alireza and Naderi Beni, Abdolmajid and Nazemi, Maziyar and Duttagupta, Srimanti and Routh, Joyanto},
	doi = {10.1007/s10933-022-00239-8},
	journal-iso = {J PALEOLIMNOL},
	journal = {JOURNAL OF PALEOLIMNOLOGY},
	volume = {2022},
	unique-id = {32775770},
	issn = {0921-2728},
	year = {2022},
	eissn = {1573-0417},
	orcid-numbers = {Vaezi, Alireza/0000-0003-2824-4923}
}

@article{MTMT:32737234,
	title = {Discrete fracture network (DFN) modelling of a high-level radioactive waste repository host rock and the effects on its hydrogeological behaviour},
	url = {https://m2.mtmt.hu/api/publication/32737234},
	author = {Tóth, Emese and Hrabovszki, Ervin and Schubert, Félix and M. Tóth, Tivadar},
	doi = {10.1016/j.jsg.2022.104556},
	journal-iso = {J STRUCT GEOL},
	journal = {JOURNAL OF STRUCTURAL GEOLOGY},
	volume = {156},
	unique-id = {32737234},
	issn = {0191-8141},
	year = {2022},
	eissn = {1873-1201},
	orcid-numbers = {Hrabovszki, Ervin/0000-0001-7914-6042; Schubert, Félix/0000-0001-8647-5354; M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:32716562,
	title = {Lithology-Controlled Hydrodynamic Behaviour of a Fractured Sandstone–Claystone Body in a Radioactive Waste Repository Site, SW Hungary},
	url = {https://m2.mtmt.hu/api/publication/32716562},
	author = {Tóth, Emese and Hrabovszki, Ervin and Schubert, Félix and M. Tóth, Tivadar},
	doi = {10.3390/app12052528},
	journal-iso = {APPL SCI-BASEL},
	journal = {APPLIED SCIENCES-BASEL},
	volume = {12},
	unique-id = {32716562},
	year = {2022},
	eissn = {2076-3417},
	orcid-numbers = {Tóth, Emese/0000-0001-8983-4084; Hrabovszki, Ervin/0000-0001-7914-6042; Schubert, Félix/0000-0001-8647-5354; M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:32589010,
	title = {Evaluation of 3D small-scale lithological heterogeneities and pore distribution of the Boda Claystone Formation using X-Ray Computed Tomography images (CT)},
	url = {https://m2.mtmt.hu/api/publication/32589010},
	author = {Abutaha, Saja and Geiger, János and Gulyás, Sándor and Fedor, Ferenc},
	doi = {10.4154/gc.2021.17},
	journal-iso = {GEOL CROAT},
	journal = {GEOLOGIA CROATICA},
	volume = {74},
	unique-id = {32589010},
	issn = {1330-030X},
	year = {2021},
	eissn = {1333-4875},
	pages = {305-318},
	orcid-numbers = {Abutaha, Saja/0000-0001-8439-5895; Geiger, János/0000-0001-9359-5266; Gulyás, Sándor/0000-0002-3384-2381}
}

@article{MTMT:32826485,
	title = {Vörös homokkő nyersanyagú szerszámkövek Hódmezővásárhely-Gorzsa késő neolit (Tisza kultúra) tell település leletanyagában [Red sandstone as raw material of late neolithic (Tisza culture) groundstones from the tell site of Hódmezővásárhely-Gorzsa.]},
	url = {https://m2.mtmt.hu/api/publication/32826485},
	author = {Miklós, Dóra Georgina and Szakmány, György and Józsa, Sándor and Starnini, Elisabetta and Horváth, Ferenc},
	doi = {10.55023/issn.1786-271X.2021-017},
	journal-iso = {ARCHEOMETRIAI MŰHELY},
	journal = {ARCHEOMETRIAI MŰHELY},
	volume = {18},
	unique-id = {32826485},
	issn = {1786-271X},
	year = {2021},
	pages = {209-236},
	orcid-numbers = {Miklós, Dóra Georgina/0009-0009-1774-8510; Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:31997541,
	title = {Palaeoenvironmental changes in Eocene Tibetan lake systems traced by geochemistry, sedimentology and palynofacies},
	url = {https://m2.mtmt.hu/api/publication/31997541},
	author = {Qin, Yuan and Natasha, Barbolini and Luisa, Ashworth and Catarina, Rydine and Dong-Lin, Gao and Fa-Shou, Shan and Xiao-Yong, Zhong and Vivi, Vajda},
	doi = {10.1016/j.jseaes.2021.104778},
	journal-iso = {J ASIAN EARTH SCI},
	journal = {JOURNAL OF ASIAN EARTH SCIENCES},
	volume = {214},
	unique-id = {31997541},
	issn = {1367-9120},
	keywords = {Quaternary; Cenozoic; Aridification; Grain size analysis; Central Asia; Steppe-desert; Proto-Paratethys Sea},
	year = {2021},
	eissn = {1878-5786},
	pages = {104778-104793}
}

@article{MTMT:32572186,
	title = {Assessing the representative elementary volume of rock types by X-ray computed tomography (CT) – a simple approach to demonstrate the heterogeneity of the Boda Claystone Formation in Hungary},
	url = {https://m2.mtmt.hu/api/publication/32572186},
	author = {Abutaha, Saja and Geiger, János and Gulyás, Sándor and Fedor, Ferenc},
	doi = {10.2478/logos-2021-0018},
	journal-iso = {GEOLOGOS},
	journal = {GEOLOGOS},
	volume = {27},
	unique-id = {32572186},
	issn = {1426-8981},
	year = {2021},
	eissn = {2080-6574},
	pages = {157-172},
	orcid-numbers = {Abutaha, Saja/0000-0001-8439-5895; Geiger, János/0000-0001-9359-5266; Gulyás, Sándor/0000-0002-3384-2381}
}

@article{MTMT:31984216,
	title = {Compositional and diagenetic evolution of a siltstone, with implications for reservoir quality; an example from the Lower Triassic Montney Formation in western Canada},
	url = {https://m2.mtmt.hu/api/publication/31984216},
	author = {Vaisblat, Noga and Harris, Nicholas B. and Ayranci, Korhan and Power, Matthew and DeBhur, Chris and Bish, David L. and Chalaturnyk, Rick and Krause, Federico and Crombez, Vincent and Euzen, Tristan and Rohais, Sebastien},
	doi = {10.1016/j.marpetgeo.2021.105066},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {129},
	unique-id = {31984216},
	issn = {0264-8172},
	year = {2021},
	eissn = {1873-4073},
	orcid-numbers = {Ayranci, Korhan/0000-0002-4808-9898; Bish, David L./0000-0002-2288-6573}
}

@article{MTMT:31253429,
	title = {Paleofluid Fingerprint as an Independent Paleogeographic Correlation Tool: An Example from Pennsylvanian Sandstones and Neighboring Crystalline Rocks (Tisia Composite Terrane, S Hungary)},
	url = {https://m2.mtmt.hu/api/publication/31253429},
	author = {Fintor, Krisztián and Raucsikné Varga, Andrea Beáta},
	doi = {10.1155/2020/3568986},
	journal-iso = {GEOFLUIDS},
	journal = {GEOFLUIDS},
	volume = {2020},
	unique-id = {31253429},
	issn = {1468-8115},
	year = {2020},
	eissn = {1468-8123},
	orcid-numbers = {Fintor, Krisztián/0000-0003-4794-9419; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}

@article{MTMT:31346747,
	title = {Potential formation mechanisms of early diagenetic displacive veins in the Permian Boda Claystone Formation},
	url = {https://m2.mtmt.hu/api/publication/31346747},
	author = {Hrabovszki, Ervin and Tóth, Emese and M. Tóth, Tivadar and Máthé, Zoltán and Schubert, Félix},
	doi = {10.1016/j.jsg.2020.104098},
	journal-iso = {J STRUCT GEOL},
	journal = {JOURNAL OF STRUCTURAL GEOLOGY},
	volume = {138},
	unique-id = {31346747},
	issn = {0191-8141},
	year = {2020},
	eissn = {1873-1201},
	orcid-numbers = {Hrabovszki, Ervin/0000-0001-7914-6042; M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:31124447,
	title = {Pedogenic information from fine-sand. A study in Mediterranean soils},
	url = {https://m2.mtmt.hu/api/publication/31124447},
	author = {Martín-García, J.M. and Molinero-García, A. and Calero, J. and Sánchez-Marañón, M. and Fernández-González, M.V. and Delgado, R.},
	doi = {10.1111/ejss.12935},
	journal-iso = {EUR J SOIL SCI},
	journal = {EUROPEAN JOURNAL OF SOIL SCIENCE},
	volume = {71},
	unique-id = {31124447},
	issn = {1351-0754},
	abstract = {Volume71, Issue4
		
		July 2020
		
		Pages 580-597},
	year = {2020},
	eissn = {1365-2389},
	pages = {580-597},
	orcid-numbers = {Molinero-García, A./0000-0003-0213-4814; Calero, J./0000-0003-2606-307X; Delgado, R./0000-0003-0759-0640}
}

@article{MTMT:31658223,
	title = {Red sandstone as raw material of Baden culture (Late Copper Age) grinding stones (Balatonőszöd - Temetői dűlő site, Hungary), with a review of the red sandstone formations of SW Hungary},
	url = {https://m2.mtmt.hu/api/publication/31658223},
	author = {Péterdi, Bálint},
	doi = {10.2218/jls.3092},
	journal-iso = {J LITHIC STUD},
	journal = {JOURNAL OF LITHIC STUDIES},
	volume = {7},
	unique-id = {31658223},
	year = {2020},
	eissn = {2055-0472},
	pages = {1-29}
}

@article{MTMT:31346919,
	title = {Shear strain and volume change associated with sigmoidal vein arrays in the Boda Claystone},
	url = {https://m2.mtmt.hu/api/publication/31346919},
	author = {Tóth, Emese and Hrabovszki, Ervin and M. Tóth, Tivadar and Schubert, Félix},
	doi = {10.1016/j.jsg.2020.104105},
	journal-iso = {J STRUCT GEOL},
	journal = {JOURNAL OF STRUCTURAL GEOLOGY},
	volume = {138},
	unique-id = {31346919},
	issn = {0191-8141},
	year = {2020},
	eissn = {1873-1201},
	orcid-numbers = {Hrabovszki, Ervin/0000-0001-7914-6042; M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:32589011,
	title = {New results of boda claystone research: Genesis, mineralogy, geochemistry, petrophysics},
	url = {https://m2.mtmt.hu/api/publication/32589011},
	author = {Fedor, Ferenc and Máthé, Zoltán and Ács, Péter and Koroncz, Péter János},
	doi = {10.1144/SP482.13},
	journal-iso = {GEOL SOC SPEC PUBL},
	journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS},
	volume = {482},
	unique-id = {32589011},
	issn = {0305-8719},
	year = {2019},
	eissn = {2041-4927},
	pages = {75-92}
}

@article{MTMT:26793577,
	title = {A multidisciplinary approach to review the vertical and lateral facies relationships of the purported vertebrate-defined terrestrial Permian–Triassic boundary interval at Bethulie, Karoo Basin, South Africa},
	url = {https://m2.mtmt.hu/api/publication/26793577},
	author = {Gastaldo, R A and Neveling, J and Geissman, J W and Li, J},
	doi = {10.1016/j.earscirev.2017.08.002},
	journal-iso = {EARTH-SCI REV},
	journal = {EARTH-SCIENCE REVIEWS},
	volume = {189},
	unique-id = {26793577},
	issn = {0012-8252},
	year = {2017},
	eissn = {1872-6828},
	pages = {220-243}
}

@article{MTMT:3105324,
	title = {Origin of natural Arsenic and Antimony contents in the Permian to Lower Triassic siliciclastic rocks of the Western Mecsek Mountains, SW Hungary},
	url = {https://m2.mtmt.hu/api/publication/3105324},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Szakmány, György},
	journal-iso = {CARPATH J EARTH ENVIRON SCI},
	journal = {CARPATHIAN JOURNAL OF EARTH AND ENVIRONMENTAL SCIENCES},
	volume = {12},
	unique-id = {3105324},
	issn = {1842-4090},
	abstract = {Arsenic and antimony has been determined by neutron 
		activation analysis in a large number (109) of siliciclastic 
		sedimentary rock samples from the western part of the Mecsek 
		Mountains (Tisia Block), Hungary. Additionally, a total of 84 
		samples were selected for XRD mineralogy. The goal of this 
		work is to determine the distribution and origin of the local 
		natural background contents of these toxic elements. 
		Concentrations of As and Sb in different Lower Permian to 
		Lower Triassic lithostratigraphic units are higher than the 
		normal global ranges represented by the Upper Continental 
		Crust composition (1.5 and 0.2 mg/kg, respectively). In the 
		studied mudrock samples, the median values for As and Sb 
		range from 3.5 to 30.5 mg/kg, and from 1.1 to 2.0 mg/kg, 
		respectively. In the sandstone samples, the median As 
		contents range from 2.3 to 20.5 mg/kg, while the values for 
		Sb range from 0.4 to 0.9 mg/kg. The highest metalloid 
		contents were found in the Upper Permian Cserdi and Boda 
		formations, which could be only of local importance as a 
		source of As in the contamination process of soils and 
		natural waters. The relatively enhanced metalloid content of 
		these rocks could be related to hydrothermal activity in the 
		region. Another possibility is that the source for background 
		levels of As and Sb in these siliciclastic rocks could be the 
		metalloid-bearing Fe oxides and oxyhydroxides coating mineral 
		grains.},
	year = {2017},
	eissn = {1844-489X},
	pages = {5-12},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Szakmány, György/0000-0002-9557-2030}
}

@article{MTMT:26651329,
	title = {Clay mineralogical characteristics at the Permian-Triassic Shangsi section and their paleoenvironmental and/or paleoclimatic significance},
	url = {https://m2.mtmt.hu/api/publication/26651329},
	author = {Xu, GZ and Deconinck, JF and Feng, QL and Baudin, F and Pellenard, P and Shen, J and Bruneau, L},
	doi = {10.1016/j.palaeo.2016.07.036},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {474},
	unique-id = {26651329},
	issn = {0031-0182},
	year = {2017},
	eissn = {1872-616X},
	pages = {152-163}
}

@article{MTMT:3000085,
	title = {Analytical performance of a versatile laboratory microscopic X-ray fluorescence system for metal uptake studies on argillaceous rocks},
	url = {https://m2.mtmt.hu/api/publication/3000085},
	author = {Gergely, F and Osán, János and Szabó, Beatrix Katalin and Török, Szabina},
	doi = {10.1016/j.sab.2015.12.007},
	journal-iso = {SPECTROCHIM ACTA B},
	journal = {SPECTROCHIMICA ACTA PART B-ATOMIC SPECTROSCOPY},
	volume = {116},
	unique-id = {3000085},
	issn = {0584-8547},
	year = {2016},
	eissn = {1873-3565},
	pages = {75-84},
	orcid-numbers = {Szabó, Beatrix Katalin/0000-0003-3010-2510}
}

@article{MTMT:3000082,
	title = {Combined X-ray microanalytical study of the Nd uptake capability of argillaceous rocks},
	url = {https://m2.mtmt.hu/api/publication/3000082},
	author = {Kéri, Annamária and Osán, János and Fábián, Margit and Dähn, R and Török, Szabina},
	doi = {10.1002/xrs.2656},
	journal-iso = {X-RAY SPECTROM},
	journal = {X-RAY SPECTROMETRY},
	volume = {45},
	unique-id = {3000082},
	issn = {0049-8246},
	year = {2016},
	eissn = {1097-4539},
	pages = {54-62}
}

@article{MTMT:3071286,
	title = {Clay mineralogy of the Boda Claystone Formation (Mecsek Mts., SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/3071286},
	author = {Németh, Tibor and Máthé, Z and Pekker, Péter and Dódony, István and Kovácsné Kis, Viktória and Sipos, Péter and Cora, Ildikó and Kovács, Ivett},
	doi = {10.1515/geo-2016-0024},
	journal-iso = {OPEN GEOSCI},
	journal = {OPEN GEOSCIENCES},
	volume = {8},
	unique-id = {3071286},
	issn = {2391-5447},
	abstract = {Boda Claystone Formation (BCF) is the host rock of the planned site for high level nuclear waste repository inHungary. Samples representing the dominant rock types of BCF were studied: albitic claystone, claystone with high illite content, and analcime bearing claystone. Clay minerals in these three rock types were characterized by Xray powder diffraction (XRD), transmission electron microscopy (TEM) and thermal analysis (DTA-TG), and the results were discussed from the point of view of the radionuclide sorption properties being studied in the future. Mineral compositions of bulk BCF samples vary in wide ranges. In the albitic sample, besides the dominant illite, few percent of chlorite represents the layer silicates in the clay fraction. Illite is the dominating phase in the illitic sample, with a few percent of chlorite. HRTEM study revealed that the thickness of illite particles rarely reaches 10 layers, usually are of 5-6 TOT layer thick. Illite crystals are generally thicker in the albitic sample than in the illitic one. The significant difference between the clay mineral characterisitics of the analcimous and the other two samples is that the former contains regularly interstratified chlorite/smectite beside the dominant illite. Based on the structural and chemical data two illite type minerals are present in the BCF samples: 1M polytype containing octahedral Fe and Mg besides Al, 2M polytype illite generally is free of Fe andMg. Close association of very thin illite plates and nanosized hematite crystals is typical textural feature for BCF. The goal of this study is to provide solid mineralogical basis for further studies focusing on radionuclide sorption properties. © 2016 T. Németh et al., published by De Gruyter Open.},
	keywords = {HRTEM; analcime; Hematite; Nuclear waste repository; illite polytypes},
	year = {2016},
	eissn = {2391-5447},
	pages = {259-274},
	orcid-numbers = {Németh, Tibor/0000-0002-1836-6006; Pekker, Péter/0000-0002-0463-0742; Sipos, Péter/0000-0002-8746-0573; Kovács, Ivett/0000-0001-7015-7909}
}

@article{MTMT:2717773,
	title = {Characteristics of uranium uptake of Boda Claystone Formation as the candidate host rock of high level radioactive waste repository in Hungary},
	url = {https://m2.mtmt.hu/api/publication/2717773},
	author = {Breitner, Dániel and Osán, János and Fábián, Margit and Zagyvai, Péter and Szabó, Csaba and Dähn, R and Marques, Fernandes M and Sajó, István and Máthé, Zoltán and Török, Szabina},
	doi = {10.1007/s12665-014-3413-4},
	journal-iso = {ENVIRON EARTH SCI},
	journal = {ENVIRONMENTAL EARTH SCIENCES},
	volume = {73},
	unique-id = {2717773},
	issn = {1866-6280},
	year = {2015},
	eissn = {1866-6299},
	pages = {209-219},
	orcid-numbers = {Zagyvai, Péter/0000-0002-8121-8452; Szabó, Csaba/0000-0002-1580-6344; Sajó, István/0000-0002-1228-1407}
}

@article{MTMT:2989417,
	title = {The colour analysis method applied to homogeneous rocks},
	url = {https://m2.mtmt.hu/api/publication/2989417},
	author = {Halász, Amadé and Halmai, Ákos},
	doi = {10.1515/logos-2015-0019},
	journal-iso = {GEOLOGOS},
	journal = {GEOLOGOS},
	volume = {21},
	unique-id = {2989417},
	issn = {1426-8981},
	abstract = {Computer-aided colour analysis can facilitate 
		cyclostratigraphic studies. Here we report on a case study 
		involving the development of a digital colour analysis method 
		for examination of the Boda Claystone Formation which is the 
		most suitable in Hungary for the disposal of high-level 
		radioactive waste. Rock type colours are reddish brown or 
		brownish red, or any shade between brown and red. The method 
		presented here could be used to differentiate similar colours 
		and to identify gradual transitions between these; the latter 
		are of great importance in a cyclostratigraphic analysis of 
		the succession. Geophysical well-logging has demonstrated the 
		existence of characteristic cyclic units, as detected by 
		colour and natural gamma. Based on our research, colour, 
		natural gamma and lithology correlate well. For core Ib-4, 
		these features reveal the presence of orderly cycles with 
		thicknesses of roughly 0.64 to 13 metres. Once the core has 
		been scanned, this is a time- and cost-effective method.},
	keywords = {ImageJ},
	year = {2015},
	eissn = {2080-6574},
	pages = {233-239},
	orcid-numbers = {Halász, Amadé/0000-0003-4582-8883; Halmai, Ákos/0000-0001-5722-8119}
}

@article{MTMT:2475908,
	title = {Microscale analysis of metal uptake by argillaceous rocks using positive matrix factorization of microscopic X-ray fluorescence elemental maps},
	url = {https://m2.mtmt.hu/api/publication/2475908},
	author = {Osán, János and Kéri, Annamária and Breitner, Dániel and Fábián, Margit and Dähn, R and Simon, R and Török, Szabina},
	doi = {10.1016/j.sab.2013.11.002},
	journal-iso = {SPECTROCHIM ACTA B},
	journal = {SPECTROCHIMICA ACTA PART B-ATOMIC SPECTROSCOPY},
	volume = {91},
	unique-id = {2475908},
	issn = {0584-8547},
	year = {2014},
	eissn = {1873-3565},
	pages = {12-23}
}

@misc{MTMT:23337008,
	title = {IV. Kőzettani és Geokémiai Vándorgyűlés. Kirándulásvezető},
	url = {https://m2.mtmt.hu/api/publication/23337008},
	unique-id = {23337008},
	year = {2013}
}

@article{MTMT:2146912,
	title = {Petrology and geochemistry of the Upper Permian – Middle Triassic siliciclastic formations of the Ibafa-4 borehole (NW-Mecsek Mts., Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2146912},
	author = {Bodor, Sarolta and Szakmány, György and Józsa, Sándor and Máthé, Zoltán},
	journal-iso = {CARPATH J EARTH ENVIRON SCI},
	journal = {CARPATHIAN JOURNAL OF EARTH AND ENVIRONMENTAL SCIENCES},
	volume = {7},
	unique-id = {2146912},
	issn = {1842-4090},
	year = {2012},
	eissn = {1844-489X},
	pages = {219-230},
	orcid-numbers = {Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044}
}

@book{MTMT:2127590,
	title = {Balatonőszöd–Temetői dűlő őskori településrészei. a középső rézkori, késő rézkori és kora bronzkori települések},
	url = {https://m2.mtmt.hu/api/publication/2127590},
	isbn = {9786155254000},
	editor = {Horváth, Tünde},
	publisher = {MTA Bölcsészettudományi Kutatóközpont Régészeti Intézete},
	unique-id = {2127590},
	year = {2012},
	orcid-numbers = {Horváth, Tünde/0000-0001-6357-400X}
}

@inbook{MTMT:2038008,
	title = {Claystone as a Potential Host Rock for Nuclear Waste Storage},
	url = {https://m2.mtmt.hu/api/publication/2038008},
	author = {Lázár, Károly and Máthé, Zoltán},
	booktitle = {Clay Minerals in Nature - Their Characterization, Modification and Application},
	doi = {10.5772/48123},
	unique-id = {2038008},
	year = {2012},
	pages = {55-80}
}

@article{MTMT:3072470,
	title = {Balatonőszöd – Temetői dűlő rézkori lelőhely homokkő nyersanyagú kőeszközeinek kőzettani és geokémiai vizsgálata. / Petrographical and Geochemical investigation of stone tools made of sandstone from the site Balatonőszöd – Temetői dűlő (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/3072470},
	author = {Péterdi, Bálint},
	journal-iso = {ARCHEOMETRIAI MŰHELY},
	journal = {ARCHEOMETRIAI MŰHELY},
	volume = {9},
	unique-id = {3072470},
	issn = {1786-271X},
	year = {2012},
	pages = {265-286}
}

@article{MTMT:3026907,
	title = {A Bodai Aleurolit Formációban mért ImaGeo-LIPS elemoxidkoncentráció-értékek eloszlásának statisztikai vizsgálata (Bakonya, Bak-5 fúrás)},
	url = {https://m2.mtmt.hu/api/publication/3026907},
	author = {Andrássy, László and Maros, Gyula},
	journal-iso = {MAGYAR GEOFIZIKA},
	journal = {MAGYAR GEOFIZIKA},
	volume = {52},
	unique-id = {3026907},
	issn = {0025-0120},
	year = {2011},
	eissn = {2677-1497},
	pages = {62-78},
	orcid-numbers = {Maros, Gyula/0000-0002-2973-4513}
}

@mastersthesis{MTMT:1698407,
	title = {A Bodai Aleurolit Formáció ciklussztratigráfiai vizsgálata},
	url = {https://m2.mtmt.hu/api/publication/1698407},
	author = {Halász, Amadé},
	unique-id = {1698407},
	year = {2011},
	orcid-numbers = {Halász, Amadé/0000-0003-4582-8883}
}

@inproceedings{MTMT:1867726,
	title = {Migration of uranyl ions in Boda claystone samples},
	url = {https://m2.mtmt.hu/api/publication/1867726},
	author = {Lázár, Károly and Megyeri, János and Mácsik, Zsuzsa and Kovács-Széles, Éva and Máthé, Zoltán},
	booktitle = {3rd Annual Workshop Proceedings of the Collaborative Project “Redox Phenomena Controlling Systems” (7th EC FP CP RECOSY)},
	unique-id = {1867726},
	year = {2011},
	pages = {91-97}
}

@CONFERENCE{MTMT:2916400,
	title = {A Bodai Aleurolit Formáció ásvány-kőzettani jellemzése},
	url = {https://m2.mtmt.hu/api/publication/2916400},
	author = {Máthé, Zoltán},
	booktitle = {II. Kőzettani és Geokémiai Vándorgyűlés},
	unique-id = {2916400},
	year = {2011},
	pages = {31-32}
}

@mastersthesis{MTMT:1974442,
	title = {Szerszámkövek és csiszolt kőeszközök archeometriai vizsgálatának eredményei. Balatonőszöd-temetői dűlő lelőhely, késő rézkor, bádeni kultúra},
	url = {https://m2.mtmt.hu/api/publication/1974442},
	author = {Péterdi, Bálint},
	unique-id = {1974442},
	year = {2011}
}

@article{MTMT:21723630,
	title = {Magyar eredmények az agyagásványtan és -földtan terén: Az 1960-ban alapított mft agyagásványtani szakosztály 50. évfordulója alkalmából Hungarian contribution to the mineralogy and geology of clays: Commemorating the 50th anniversary of the Hungarian Clay Minerals Group founded in 1960},
	url = {https://m2.mtmt.hu/api/publication/21723630},
	author = {Viczián, I},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {141},
	unique-id = {21723630},
	issn = {0015-542X},
	year = {2011},
	eissn = {2559-902X},
	pages = {313-319}
}

@article{MTMT:1348919,
	title = {Sedimentology of a Permian playa lake: the Boda Claystone Formation, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1348919},
	author = {Konrád, Gyula and Sebe, Krisztina and Halász, Amadé and Babinszki, Edit},
	doi = {10.2478/v10118-010-0002-1},
	journal-iso = {GEOLOGOS},
	journal = {GEOLOGOS},
	volume = {16},
	unique-id = {1348919},
	issn = {1426-8981},
	abstract = {The Upper Permian Boda Claystone Formation (BCF) in SW Hungary has been previously been identified as a saline lake deposit. A country-wide screening found this 800–1000 m thick succession the most suitable for the disposal of high-level radioactive waste in Hungary, and research into this formation has consequently been intensified since. The investigations included a detailed study of the sedimentological characteristics. Data obtained by mapping of the 25 km2 outcrop area of the formation and from more than 40 boreholes were processed. The sedimentary structures were investigated on outcrop to microscopic scales, and cycles in the succession were interpreted.
		The main lithofacies, sedimentary structures and ichnofossils are presented. They indicate that the major part of the succession was deposited in a playa mudflat and is not of lacustrine origin in a strict sense. The lake sediments are represented
		by laminated and ripple-marked/flaser-type cross-laminated claystones and siltstones and by massive dolomites;
		trace fossils include crawling traces and burrows. Partial or complete drying out of the lake commonly occurred after the formation of carbonate mud by evaporation. Periodic fluvial influx is recorded by cross-bedded sandstones and unsorted gravelly sandstones of up to pebble-sized angular grains. Fenestral and stromatolitic structures reflect the repeated appearance of playa mudflat conditions. The silty claystones, which compose the major part of the succession, lost their primary structures due to pedogenic processes and indicate prolonged subaerial intervals with soil formation and only ephemeral inundations. The presence of pedogenic carbonate concretions supports the interpretation of an arid climate and a relatively shallow groundwater table. Drying-out events shown by desiccation cracks and authigenic breccias can be traced all over the succession.
		The various facies form small-scale sedimentary cycles showing a shallowing-upward trend and the growing influence of aridity and subaerial exposure.},
	year = {2010},
	eissn = {2080-6574},
	pages = {27-41},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Halász, Amadé/0000-0003-4582-8883}
}

@mastersthesis{MTMT:26146067,
	title = {Stroncium, cézium, kobalt és jód szorpciójának és migrációjának vizsgálata agyagkőzet mintákon és nagy dózisok detektálására alkalmas termolumineszcens anyag kifejlesztése},
	url = {https://m2.mtmt.hu/api/publication/26146067},
	author = {Mell, P},
	unique-id = {26146067},
	year = {2010}
}

@article{MTMT:1593074,
	title = {Preliminary results on the Co, Sr and Cs sorption properties of the analcime-containing rock type of the Boda Siltstone Formation},
	url = {https://m2.mtmt.hu/api/publication/1593074},
	author = {Sipos, Péter and Németh, Tibor and Máthé, Zoltán},
	doi = {10.1556/CEuGeol.53.2010.1.4},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {53},
	unique-id = {1593074},
	issn = {1788-2281},
	year = {2010},
	eissn = {1789-3348},
	pages = {67-78},
	orcid-numbers = {Sipos, Péter/0000-0002-8746-0573; Németh, Tibor/0000-0002-1836-6006}
}

@article{MTMT:1299028,
	title = {A felső-permi Cserdi Konglomerátum Formáció kavicsanyagának kőzettani és geokémiai vizsgálati eredményei (XV. szerkezetkutató fúrás, Ny-Mecsek)},
	url = {https://m2.mtmt.hu/api/publication/1299028},
	author = {Bodor, Sarolta and Szakmány, György},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {139},
	unique-id = {1299028},
	issn = {0015-542X},
	year = {2009},
	eissn = {2559-902X},
	pages = {325-340},
	orcid-numbers = {Szakmány, György/0000-0002-9557-2030}
}

@article{MTMT:2251164,
	title = {Izotópmigrációs vizsgálatok a Bodai Aleurolit Formáció kőzetmintáin},
	url = {https://m2.mtmt.hu/api/publication/2251164},
	author = {Lázár, Károly and Máthé, Zoltán and Megyeri, János and Mell, P and Szarvas, Tibor},
	journal-iso = {MAGY KÉM FOLY KÉM KÖZL},
	journal = {MAGYAR KÉMIAI FOLYÓIRAT - KÉMIAI KÖZLEMÉNYEK (1997-)},
	volume = {115},
	unique-id = {2251164},
	issn = {1418-9933},
	year = {2009},
	eissn = {1418-8600},
	pages = {129-133}
}

@mastersthesis{MTMT:1337382,
	title = {A dél-dunántúli paleozoos–alsó-triász sziliciklasztos kőzetek kőzettani és geokémiai vizsgálatának eredményei},
	url = {https://m2.mtmt.hu/api/publication/1337382},
	author = {Raucsikné Varga, Andrea Beáta},
	publisher = {Eötvös Loránd University},
	unique-id = {1337382},
	year = {2009},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}

@inbook{MTMT:1325257,
	title = {Metaüledékes képződmények a Tiszai-egység aljzatában: a felső-paleozoikumi Túronyi Formáció (Szlavóniai-Drávai-terrénum)},
	url = {https://m2.mtmt.hu/api/publication/1325257},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla},
	booktitle = {Magmás és metamorf képződmények a Tiszai Egységben},
	unique-id = {1325257},
	abstract = {Tanulmányunkban a Villányi-hegység északi előterében (Szlavóniai-Drávai-terrénum, Villányi zóna) feltárt, bizonytalan rétegtani besorolású Túronyi Formáció metaüledékes rétegsorát mutatjuk be. Az ásványtani, a kőzettani és a geokémiai összetételre épülő lokális és regionális (északi peritethysi régió permokarbon medencéi) korreláció alapján a Túronyi Formáció képződése az asszeli idejére (cisurali, kora-perm) tehető.},
	year = {2009},
	pages = {177-192},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974}
}

@article{MTMT:1679307,
	title = {Laboratory Pressure Pulse Decay Permeability Measurement of Boda Claystone, Mecsek Mts, SW Hungary},
	url = {https://m2.mtmt.hu/api/publication/1679307},
	author = {Fedor, Ferenc and Hámos, Gábor and Jobbik, Anita and Máthé, Zoltán and Somodi, Gábor and Szűcs, István},
	doi = {10.1016/j.pce.2008.10.059},
	journal-iso = {PHYS CHEM EARTH (2002-)},
	journal = {PHYSICS AND CHEMISTRY OF THE EARTH (2002-)},
	volume = {33},
	unique-id = {1679307},
	issn = {1474-7065},
	year = {2008},
	eissn = {1873-5193},
	pages = {S45-S53}
}

@{MTMT:1698520,
	title = {Geological environment of a possible waste repository site in SE Transdanubia (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1698520},
	author = {Halász, Amadé and Konrád, Gyula and Sebe, Krisztina and Szederkényi, Tibor},
	booktitle = {Progress in Geography in the European Capital of Culture 2010},
	unique-id = {1698520},
	year = {2008},
	pages = {271-282},
	orcid-numbers = {Halász, Amadé/0000-0003-4582-8883; Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1337379,
	title = {A felső-paleozoikumi Turonyi Formáció (Szlavóniai–Drávai-terrénum) pelites kőzeteinek ásványtani és kőzettani jellemzői [Mineralogical and petrological characteristics of mudrocks from the Upper Palaeozoic Turony Formation (Slavonia–Drava unit)]},
	url = {https://m2.mtmt.hu/api/publication/1337379},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Kovácsné Kis, Viktória and Szakmány, György},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {138},
	unique-id = {1337379},
	issn = {0015-542X},
	year = {2008},
	eissn = {2559-902X},
	pages = {5-20},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Szakmány, György/0000-0002-9557-2030}
}

@CONFERENCE{MTMT:26146054,
	title = {Dioctahedral vermiculite in the Boda Siltstone Formation (Boda, Mecsek Mts., SW-Hungary)},
	url = {https://m2.mtmt.hu/api/publication/26146054},
	author = {Dódony, I and Lovas, Gy},
	booktitle = {3rd Mineral Sciences in the Carpathians International Conference (MSCC3)},
	unique-id = {26146054},
	year = {2006},
	pages = {26}
}

@article{MTMT:26146072,
	title = {Termoanalízis alkalmazása radioaktív hulladéklerakók földtani kutatása során},
	url = {https://m2.mtmt.hu/api/publication/26146072},
	author = {Földvári, M},
	journal-iso = {ACTA GGM DEBRECINA},
	journal = {ACTA GEOGRAPHICA AC GEOLOGICA ET METEOROLOGICA DEBRECINA: GEOLOGY GEOMORPHOLOGY PHYSICAL GEOGRAPHY SERIES},
	volume = {1},
	unique-id = {26146072},
	issn = {1788-4497},
	year = {2006},
	pages = {25-32}
}

@article{MTMT:1080852,
	title = {Diffusion of Sr, Cs, Co And I in Argillaceous Rock as Studied by Radiotracers},
	url = {https://m2.mtmt.hu/api/publication/1080852},
	author = {Mell, P and Megyeri, J and Riess, L and Máthé, Zoltán and Hámos, G and Lázár, Károly},
	doi = {10.1007/s10967-006-0178-6},
	journal-iso = {J RADIOANAL NUCL CHEM},
	journal = {JOURNAL OF RADIOANALYTICAL AND NUCLEAR CHEMISTRY},
	volume = {268},
	unique-id = {1080852},
	issn = {0236-5731},
	abstract = {Diffusions of Sr-85, Cs-137, Co-60 and I-125 radionuclides have been
		studied in borecore samples from Boda siltstone/claystone formation
		(BCF) under ambient and in situ conditions. In-diffusion (Sr-85,
		Cs-137, Co-60 and I-125) and through-diffusion measurements (I-125)
		were performed at ambient conditions, and for iodine, in-diffusion
		measurements were also carried out at in situ conditions (100 bar, 50
		degrees C). In the case of cationic species carrier-containing
		solutions were also applied. Co-60 was detected only in the first slice
		of borecore at each sample, while Cs-137 was detected also in the
		first-, second- and third slices according to the
		concentration-increase of inactive carrier. Among the investigated
		cations, Sr-85 exhibited the fastest diffusion rate with 2.7 -
		6.0.10(-12) m(2)/s apparent diffusivity values. In the course of
		in-diffusion measurements 4.7.10(-11) m(2)/s, during through-diffusion
		investigations 1.4 - 1.6.10(-12) m(2)/s and at in situ conditions 5.0 -
		8.0.10 - 12 m(2)/s apparent diffusivities were obtained for I-125.
		Modest sorption of I-125 can also be deduced from the results.},
	year = {2006},
	eissn = {1588-2780},
	pages = {411-417}
}

@article{MTMT:1080856,
	title = {Sorption of Co, Cs, Sr And I Onto Argillaceous Rock as Studied by Radiotracers},
	url = {https://m2.mtmt.hu/api/publication/1080856},
	author = {Mell, P and Megyeri, János and Riess, L and Máthé, Zoltán and Csicsák, J and Lázár, Károly},
	doi = {10.1007/s10967-006-0177-7},
	journal-iso = {J RADIOANAL NUCL CHEM},
	journal = {JOURNAL OF RADIOANALYTICAL AND NUCLEAR CHEMISTRY},
	volume = {268},
	unique-id = {1080856},
	issn = {0236-5731},
	year = {2006},
	eissn = {1588-2780},
	pages = {405-410}
}

@article{MTMT:1203520,
	title = {A Bodai Aleurolit Formáció törmelékes kőzettípusainak ásványtani, kőzettani és geokémiai jellemzői [Mineralogical, petrological and geochemical characteristics of the siliciclastic rock types of Boda Siltstone Formation]},
	url = {https://m2.mtmt.hu/api/publication/1203520},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Szakmány, György and Máthé, Zoltán},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {136},
	unique-id = {1203520},
	issn = {0015-542X},
	year = {2006},
	eissn = {2559-902X},
	pages = {201-231},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Szakmány, György/0000-0002-9557-2030}
}

@inproceedings{MTMT:26146053,
	title = {Application of the Fuzzy Set Theory for the Quantitative Phase Analysis of Rocks Using Thermal Analysis Applied to the Boda Siltstone Formation, Hungary},
	url = {https://m2.mtmt.hu/api/publication/26146053},
	author = {Földvári, M},
	booktitle = {6th International Symposium of Hungarian Researchers on Computational Intelligence : proceedings},
	unique-id = {26146053},
	year = {2005},
	pages = {1-7}
}

@article{MTMT:1338185,
	title = {Az őskörnyezeti viszonyok jellemzése a törmelékes üledékes kőzetek kémiai összetétele alapján [Characterization of palaeoenvironment based on chemical composition of siliciclastic sedimentary rocks]},
	url = {https://m2.mtmt.hu/api/publication/1338185},
	author = {Raucsikné Varga, Andrea Beáta},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {135},
	unique-id = {1338185},
	issn = {0015-542X},
	year = {2005},
	eissn = {2559-902X},
	pages = {433-458},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}