@{MTMT:31971213,
	title = {A paleogén-medence fejlődése a korai oligocénben mikropaleontológiai és geokémiai adatok tükrében},
	url = {https://m2.mtmt.hu/api/publication/31971213},
	author = {Ozsvárt, Péter and Vető, István and Nagymarosy, András},
	booktitle = {22. Magyar Őslénytani Vándorgyűlés, Döbrönte. Program, előadáskivonatok, kirándulásvezető},
	unique-id = {31971213},
	keywords = {mikropaleontológia; Early Paleogene},
	year = {2019},
	pages = {28-28}
}

@article{MTMT:2209355,
	title = {A kõpatak völgye},
	url = {https://m2.mtmt.hu/api/publication/2209355},
	author = {Albert, Gáspár},
	journal-iso = {TERMÉSZET VILÁGA},
	journal = {TERMÉSZET VILÁGA},
	volume = {144},
	unique-id = {2209355},
	issn = {0040-3717},
	year = {2013},
	pages = {85-86},
	orcid-numbers = {Albert, Gáspár/0000-0002-1723-8328}
}

@article{MTMT:3110525,
	title = {Ipari célú hévíz kútpár tervezése Úri (Pest megyei település) térségében},
	url = {https://m2.mtmt.hu/api/publication/3110525},
	author = {Kerékgyártó, Tamás},
	journal-iso = {HIDROLÓGIAI TÁJÉKOZTATÓ},
	journal = {HIDROLÓGIAI TÁJÉKOZTATÓ},
	volume = {50},
	unique-id = {3110525},
	issn = {0439-0954},
	year = {2011},
	pages = {40-41}
}

@article{MTMT:2076240,
	title = {Platóhelyzetű eolikus üledékek és formák az Agár-tető bazaltfennsíkján (Déli-Bakony). Mountain-top aeolian deposits and ventifacts on the basalt plateau of Agár-tető (Southern Bakony, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2076240},
	author = {Sebe, Krisztina and Csillag, Gábor and Thamóné Bozsó, Edit},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {141},
	unique-id = {2076240},
	issn = {0015-542X},
	abstract = {Mountain-top or cliff-top aeolian deposits are a special type of aeolian sediment, which are transported upwards along steep or even vertical slopes by the wind. Most of the published occurrences are of Holocene age. In Europe, they have been reported from a few sites along the western margin of the continent. Here we describe aeolian deposits covering the extensive basalt plateau of Agár-teto in the Transdanubian Range (Southern Bakony). The deposits have a thickness of around 0.5 m on horizontal surfaces, while in wind shadow they can be several metres thick. They are mainly medium-sorted, with grain sizes ranging from clay to fine gravel but the dominant type is fine sand. The majority of the grains are quartz and probably originated from the north - i.e. from Lake Pannon sediments underlying the basalt. The sediment material itself must have been transported onto the plateau by strong winds during the Pleistocene glacials. Trapping was most probably caused by the coarse surface roughness (i.e. a surface strewn with basalt blocks), by vegetation cover and, in the case of thick accumulations, by the topographical position. Strong aeolian activity is indicated by wind-fluted basalt blocks as well.},
	keywords = {BASALT; PLEISTOCENE; Periglacial; Ventifact; Transdanubian range (Hungary); Mountain-top aeolian sediments},
	year = {2011},
	eissn = {2559-902X},
	pages = {393-399},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:32211767,
	title = {A magyar szakpolitikai területi értékelési rendszer intézményesülése, főbb eredményei, kihívásai.},
	url = {https://m2.mtmt.hu/api/publication/32211767},
	author = {Czira, Tamás and Tipold, F.},
	journal-iso = {FALU VÁROS RÉGIÓ},
	journal = {FALU VÁROS RÉGIÓ},
	unique-id = {32211767},
	issn = {1218-2613},
	year = {2010},
	pages = {4-9}
}

@book{MTMT:3037596,
	title = {A Magyar Állami Földtani Intézet Évi Jelentése (2009)},
	url = {https://m2.mtmt.hu/api/publication/3037596},
	author = {Fancsik, Tamás},
	editor = {Balla, Zoltán and Piros, Olga},
	publisher = {Geological Institute of Hungary},
	unique-id = {3037596},
	keywords = {földtan},
	year = {2010}
}

@article{MTMT:1768076,
	title = {Volumetric modelling of cavities and pores in the Pál-völgy Cave, Budapest. A budapesti Pál-völgyi-barlang üreg- és pórustérfogatának modellezése},
	url = {https://m2.mtmt.hu/api/publication/1768076},
	author = {Albert, Gáspár},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {140},
	unique-id = {1768076},
	issn = {0015-542X},
	abstract = {The aim of this study was the determination of the respective volumes of the cavities in the Pál-völgy Cave (Budapest) and the confirmation of the post-diagenetic origin of the porosity in the incorporating carbonate rock body. This was done by measuring the size and frequency of the fractures and solution marks in the vicinity of the cave. For this a volumetric and a porosity model of the cave and its environs was constructed. This new method for volumetric cave modelling also solved the problem of processing cave maps from archives and data acquired by quick measurement.This involved producing volumetric data with highly accurate mathematical approaches. Furthermore, the value of this new, mostly theoretical, approach for volumetric cave modelling was reinforced by the porosity model, which was based on field measurements. Through the modelling, an estimation of the probable, but still not explored size of the Pál-völgy Cave was also calculated.},
	keywords = {CAVE; Volumetric model; Tectonic porosity; Buda hills},
	year = {2010},
	eissn = {2559-902X},
	pages = {263-280},
	orcid-numbers = {Albert, Gáspár/0000-0002-1723-8328}
}

@article{MTMT:1378829,
	title = {Bentonite deposits of Hungary – a review of their mineralogy and geology.},
	url = {https://m2.mtmt.hu/api/publication/1378829},
	author = {Kovács-Pálffy, P and Földessy, János and Kónya, Péter and Bertalan, Éva},
	journal-iso = {ACTA MINERAL PETROGR ABSTRACT SER},
	journal = {ACTA MINERALOGICA PETROGRAPHICA - ABSTRACT SERIES},
	volume = {6},
	unique-id = {1378829},
	issn = {1589-4835},
	year = {2010},
	pages = {308-308}
}

@CONFERENCE{MTMT:31305409,
	title = {Nehézfém-szennyezések vizsgálata felhagyott bányaterületeken. Erdélyi esettanulmány.},
	url = {https://m2.mtmt.hu/api/publication/31305409},
	author = {HORVáTH, É. and JORDÁN, Gy. and Fügedi, Ubul and BARTHA, A. and BALLÓK, M. and KUTI, L. and HELTAI, GY. and KALMÁR, J. and WALDMANN, I. and NAPRADEAN, I. and DAMIAN, G.},
	booktitle = {VIII. Földtudományi Ankét, Nagykanizsa,},
	unique-id = {31305409},
	year = {2009},
	pages = {2-2}
}

@article{MTMT:1878516,
	title = {Az észlelési földtani térképek digitális feldolgozásának /archiválásának menete},
	url = {https://m2.mtmt.hu/api/publication/1878516},
	author = {Albert, Gáspár},
	journal-iso = {M ÁLL FÖLDT INT JELENT},
	journal = {MAGYAR ÁLLAMI FÖLDTANI INTÉZET ÉVI JELENTÉSE},
	volume = {2007},
	unique-id = {1878516},
	issn = {0368-9751},
	abstract = {During geological surveying the most important objects, besides 
		the hammer and loupe, are the maps and notes. The basic 
		geological data are recorded cartographically on a map with 
		reference key and literally in a booklet. These data are the 
		most genuine information, which can be accessed later, that’s 
		why the preservation of the original notes should be an 
		important aim for an institution, which performs regular 
		scientific observations. In the Geological Institute of Hungary, 
		where geological mapping is one of the primary functions for 
		nearly 140 years, the data of manuscripts are hardly or 
		inaccessible because of the difficulty of cataloging and 
		organizing of them. The needs of recent times make it necessary, 
		the technological frames make it possible to use geological 
		information in the scale of observation, which means the use of 
		authentic data. To achieve this, a method has been worked out, 
		which aimed to transform the information of draw-up maps and 
		field note manuscripts into a unified form, which can be 
		compared with other databases, to insert them into a 
		geographical information system, to create a uniform layout for 
		the digitalized maps, and to operate a functional data storage 
		system. In the study performed, the frames and main connections 
		of this method on demonstrated cases have been revealed.},
	year = {2009},
	pages = {45-53},
	orcid-numbers = {Albert, Gáspár/0000-0002-1723-8328}
}