@article{MTMT:1768103,
	title = {Dating Pleistocene aeolian landforms in Hungary, Central Europe, using in situ produced cosmogenic 10Be},
	url = {https://m2.mtmt.hu/api/publication/1768103},
	author = {Ruszkiczay-Rüdiger, Zsófia and Braucher, R and Csillag, Gábor and Fodor, László and Dunai, T J and Bada, G and Bourlés, D and Müller, P},
	doi = {10.1016/j.quageo.2011.06.001},
	journal-iso = {QUAT GEOCHRONOL},
	journal = {QUATERNARY GEOCHRONOLOGY},
	volume = {6},
	unique-id = {1768103},
	issn = {1871-1014},
	abstract = {In the Western Pannonian Basin the widespread occurrence of 
		ventifacts and large-scale deflation features indicate strong 
		wind activity during the Quaternary. Pleistocene glaciations are 
		probably the most important periods of wind erosion. However, 
		age of the wind-polished rock surfaces exposed on different 
		geomorphic horizons has remained unknown so far, although they 
		can provide time constraints of landscape evolution. 
		Measurements of 10Be concentrations along depth profiles of 
		exposed wind-facetted rocks allow deriving local denudation 
		rates of 3.46-3.88 m/Ma and exposure ages as old as 1.5 Ma. 
		Regional denudation, which occurred mainly via deflation of the 
		loose sediments, varies between 40 and 80 m/Ma. This study 
		provides evidence that aeolian erosion in continental, 
		periglacial areas of Central Europe played an important role in 
		Quaternary landscape modification. © 2011 Elsevier B.V.},
	keywords = {Quaternary; Depth profile; Wind abrasion; Ventifact; Exposure age; Denudation rate; Deflation; Cosmogenic beryllium-10},
	year = {2011},
	eissn = {1878-0350},
	pages = {515-529}
}

@article{MTMT:1369043,
	title = {OSL-dating the Quaternary landscape evolution in the Vértes Hills forelands (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1369043},
	author = {Thamóné Bozsó, Edit and Csillag, Gábor and Fodor, László and Müller, P M and Nagy, Attila},
	doi = {10.1016/j.quageo.2009.02.020},
	journal-iso = {QUAT GEOCHRONOL},
	journal = {QUATERNARY GEOCHRONOLOGY},
	volume = {5},
	unique-id = {1369043},
	issn = {1871-1014},
	year = {2010},
	eissn = {1878-0350},
	pages = {120-124}
}

@article{MTMT:1406988,
	title = {A Balaton legnagyobb kiterjedésének rekonstrukciója a függőleges kéregmozgások figyelembevételével [Reconstructing the maximum extent of lake Balaton (Transdanubia, Hungary) with respect to vertical crustal movements]},
	url = {https://m2.mtmt.hu/api/publication/1406988},
	author = {Timár, Gábor and Csillag, Gábor and Székely, Balázs and Molnár, Gábor and Galambos, Csilla and Czanik, Csenge},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {140},
	unique-id = {1406988},
	issn = {0015-542X},
	year = {2010},
	eissn = {2559-902X},
	pages = {455-462},
	orcid-numbers = {Timár, Gábor/0000-0001-9675-6192; Székely, Balázs/0000-0002-6552-4329; Molnár, Gábor/0000-0001-9309-3418; Galambos, Csilla/0000-0002-6041-1800}
}

@article{MTMT:1353319,
	title = {Discrimination of fluvial, eolian and neotectonic features in a low hilly landscape: A DEM-based morphotectonic analysis in the Central Pannonian Basin, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1353319},
	author = {Ruszkiczay-Rüdiger, Zsófia and Fodor, László and Horváth, Erzsébet and Telbisz, Tamás Ferenc},
	doi = {10.1016/j.geomorph.2008.08.014},
	journal-iso = {GEOMORPHOLOGY},
	journal = {GEOMORPHOLOGY},
	volume = {104},
	unique-id = {1353319},
	issn = {0169-555X},
	keywords = {EXTRACTION; EVOLUTION; morphometry; DEFORMATION; Pannonian Basin; carpathians; Quaternary; Greece; Digital elevation models; Neotectonics; Godollo Hills; Deflation; EXAMPLE; DRAINAGE NETWORKS; LONGITUDINAL RIVER PROFILES; Drainage pattern analysis},
	year = {2009},
	eissn = {1872-695X},
	pages = {203-217},
	orcid-numbers = {Horváth, Erzsébet/0000-0002-0197-4152; Telbisz, Tamás Ferenc/0000-0003-4471-2889}
}

@article{MTMT:1348917,
	title = {The role of neotectonics in fluvial landscape development in the Western Mecsek Mountains and related foreland basins (SE Transdanubia, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1348917},
	author = {Sebe, Krisztina and Csillag, Gábor and Konrád, Gyula},
	doi = {10.1016/j.geomorph.2007.05.018},
	journal-iso = {GEOMORPHOLOGY},
	journal = {GEOMORPHOLOGY},
	volume = {102},
	unique-id = {1348917},
	issn = {0169-555X},
	year = {2008},
	eissn = {1872-695X},
	pages = {55-67},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1384784,
	title = {The Fekete-hegy (Balaton Highland Hungary) "soft-substrate" and "hard-substrate" maar volcanoes in an aligned volcanic complex - Implications for vent geometry, subsurface stratigraphy and the palaeoenvironmental setting},
	url = {https://m2.mtmt.hu/api/publication/1384784},
	author = {Auer, A and Martin, U and Németh, Károly},
	doi = {10.1016/j.jvolgeores.2006.06.008},
	journal-iso = {J VOLCANOL GEOTH RES},
	journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH},
	volume = {159},
	unique-id = {1384784},
	issn = {0377-0273},
	abstract = {The Fekete-hegy volcanic complex is located in the centre of the Bakony Balaton Highland Volcanic Field, in the Pannonian Basin, which formed from the late Miocene to Pliocene period. The eruption of at least four very closely clustered maar volcanoes into two clearly distinct types of prevolcanic rocks allows the observation and comparison of hard-substrate and soft-substrate maars in one volcanic complex. The analyses of bedding features, determination of the proportion of accidental lithic clasts, granulometry and age determination helped to identify and distinguish the two types of maar volcanoes. Ascending magma interacted with meteoric water in karst aquifers in Mesozoic carbonates, as well as in porous media aquifers in Neogene unconsolidated, wet, siliciclastic sediments. The divided basement setting is reflected by distinct bedding characteristics and morphological features of the individual volcanic edifices as well as a distinct composition of pyroclastic rocks. Country rocks in hard-substrate maars have a steep angle of repose, leading to the formation of steep sided cone-shaped diatremes. Enlargement and filling of these diatreme is mainly a result of shattering material by FCI related shock waves and wall-rock collapse during downward penetration of the explosion locus. Country rocks in soft-substrate maars have much shallower angles of repose, leading to the formation of broad, bowl shaped structures or irregular depressions. Enlargement and filling of these diatremes is mainly the result of substrate collapse, for example due to liquefaction of unconsolidated material by FCI-related shock waves, and its emplacement by gravity flows. The Fekete-hegy is an important example illustrating that the substrate of a volcanic edifice has to be taken into account as an important interface, which can have major control on phreatomagmatic eruptions and the resulting characteristics of the volcanic complex. © 2006 Elsevier B.V. All rights reserved.},
	keywords = {Europe; SUBSTRATE; Hungary; Eurasia; Central Europe; Explosive volcanism; STRATIGRAPHY; MAAR; Pannonian Basin; phreatomagmatism; diatreme; volcanoes; volcanic eruption; Balaton Highland; volcano; Volcanic complex; Subsurface stratigraphy; Maar volcanoes; Diatremes; Substrates; Seismology; phreatomagmatic eruptions; Volcanic rocks; Structural geology},
	year = {2007},
	eissn = {1872-6097},
	pages = {225-245}
}

@article{MTMT:2176400,
	title = {Motion of Adria and ongoing inversion of the Pannonian Basin: Seismicity, GPS velocities, and stress transfer},
	url = {https://m2.mtmt.hu/api/publication/2176400},
	author = {Bada, G and Grenerczy, G and Tóth, László and Horváth, Ferenc and Stein, S and Cloetingh, S and Windhoffer, G and Fodor, László and Pinter, N and Fejes, I},
	doi = {10.1130/2007.2425(16)},
	journal-iso = {SPEC PAP - GEOL SOC AM},
	journal = {SPECIAL PAPERS - GEOLOGICAL SOCIETY OF AMERICA},
	volume = {425},
	unique-id = {2176400},
	issn = {0072-1077},
	abstract = {We present data and models for the present-day stress and strain pattern in the Pannonian Basin and surrounding East Alpine-Dinaric orogens. Formation of the Pannonian Basin within the Alpine mountain belt started in the early Miocene, whereas its compressional reactivation has been taking place since late Pliocene-Quaternary time. Basin inversion is related to changes in the stress field from a state of tension during basin formation in the Miocene to a state of compression resulting from the convergence between the Adria microplate and the European plate. Seismicity indicates that deformation is mainly concentrated along Adria's boundaries where pure contraction (thrusting in Friuli and the southeastern Dinarides), often in combination with transform faulting (dextral transpression in the central Dinarides), is predominant. Tectonic stresses and deformation are transferred into the Pannonian Basin, resulting in a complex pattern of ongoing tectonic activity. From the margin of Adria toward the interior of the Pannonian Basin, the dominant style of deformation gradually changes from pure contraction, through transpression, to strike-slip faulting. Shortening in the basin system, documented by earthquake focal mechanisms, global positioning system (GPS) data, and the neotectonic habitat, has led to considerable seismotectonic activity and folding of the lithosphere. The state of recent stress and deformation in the Pannonian Basin is governed by the interaction of plate-boundary and intraplate forces, which include the counterclockwise rotation and N-NE-directed indentation of the Adria microplate ("Adria-push") as the dominant source of compression, in combination with buoyancy forces associated with differential topography and lithospheric heterogeneities. © 2007 The Geological Society of America.},
	keywords = {GPS; Pannonian Basin; seismicity; STRESS TRANSFER},
	year = {2007},
	pages = {243-262}
}

@{MTMT:1421963,
	title = {Landforms and timing of Quaternary deflation in the western Pannonian Basin, Hungary, using in situ produced cosmogenic 10Be},
	url = {https://m2.mtmt.hu/api/publication/1421963},
	author = {Ruszkiczay-Rüdiger, Zsófia and Bada, G and Csillag, Gábor and Dunai, T and Fodor, László},
	booktitle = {Carpatho-Balkan-Dinaric Conference on Geomorphology, 2007},
	unique-id = {1421963},
	year = {2007},
	pages = {57}
}

@article{MTMT:1353321,
	title = {Folyóvízi, eolikus és neotektonikus hatások szerepe a Gödöllői-dombság felszínfejlődésében: DEM-alapú morfometriai vizsgálat},
	url = {https://m2.mtmt.hu/api/publication/1353321},
	author = {Ruszkiczay-Rüdiger, Zsófia and Fodor, László and Horváth, Erzsébet and Telbisz, Tamás Ferenc},
	journal-iso = {FÖLDRAJZI KÖZLEMÉNYEK},
	journal = {FÖLDRAJZI KÖZLEMÉNYEK},
	volume = {131},
	unique-id = {1353321},
	issn = {0015-5411},
	year = {2007},
	pages = {319-342},
	orcid-numbers = {Horváth, Erzsébet/0000-0002-0197-4152; Telbisz, Tamás Ferenc/0000-0003-4471-2889}
}

@article{MTMT:1369036,
	title = {Neotectonics and Quaternary landscape evolution of the Gödöllő Hills, Central Pannonian Basin, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1369036},
	author = {Ruszkiczay-Rüdiger, Zsófia and Fodor, László and Horváth, Erzsébet},
	doi = {10.1016/j.gloplacha.2007.02.010},
	journal-iso = {GLOBAL PLANET CHANGE},
	journal = {GLOBAL AND PLANETARY CHANGE},
	volume = {58},
	unique-id = {1369036},
	issn = {0921-8181},
	keywords = {Quaternary; compression; landscape evolution; Neotectonics; subsidence; strike-slip fault; morphotectonics; drainage network},
	year = {2007},
	eissn = {1872-6364},
	pages = {181-196},
	orcid-numbers = {Horváth, Erzsébet/0000-0002-0197-4152}
}

@article{MTMT:2899084,
	title = {Neotectonics of the Somogy hills (Part II): Evidence from seismic sections},
	url = {https://m2.mtmt.hu/api/publication/2899084},
	author = {Csontos, László and Magyari, A and Van, Vliet-Lanoe B and Musitz, Balázs},
	doi = {10.1016/j.tecto.2005.05.049},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {410},
	unique-id = {2899084},
	issn = {0040-1951},
	abstract = {The Somogy hills are located in the Pannonian Basin, south of Lake Balaton, Hungary, above several important tectonic zones. Analysis of industrial seismic lines shows that the pre-Late Miocene substratum is deformed by several thrust faults and a transpressive flower structure. Basement is composed of slices of various Palaeo-Mesozoic rocks, overlain by sometimes preserved Paleogene, thick Early Miocene deposits. Middle Miocene, partly overlying a post-thrusting unconformity, partly affected by the thrusts, is also present. Late Miocene thick basin-fill forms onlapping strata above a gentle paleo-topography, and it is also folded into broad anticlines and synclines. These folds are thought to be born of blind fault reactivation of older thrusts. Topography follows the reactivated fold pattern, especially in the central-western part of the study area. The map pattern of basement structures shows an eastern area, where NE-SW striking thrusts, folds and steep normal faults dominate, and a western one, where E-W striking thrusts and folds dominate. Folds in Late Neogene are also parallel to these directions. A NE-SW striking linear normal fault and associated N-S faults cut the highest reflectors. The NE-SW fault is probably a left-lateral master fault acting during-after Late Miocene. Gravity anomaly and Pleistocene surface uplift maps show a very good correlation to the mapped structures. All these observations suggest that the main Early Miocene shortening was renewed during the Middle and Late Miocene, and may still persist. Two types of deformational pattern may explain the structural and topographic features. A NW-SE shortening creates right-lateral slip along E-W faults, and overthrusts on NE-SW striking ones. Another, NNE-SSW shortening creates thrusting and uplift along E-W striking faults and transtensive left-lateral slip along NE-SW striking ones. Traces of both deformation patterns can be found in Quaternary exposures and they seem to be consistent with the present day stress orientations of the Pannonian Basin, too. The alternation of stress fields and multiple reactivation of the older fault sets is thought to be caused by the northwards translation and counter-clockwise rotation of Adria and the continental extrusion generated by this convergence. (c) 2005 Elsevier B.V. All rights reserved.},
	year = {2005},
	eissn = {1879-3266},
	pages = {63-80}
}

@article{MTMT:1138137,
	title = {An outline of neotectonic structures and morphotectonics of the western and central Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/1138137},
	author = {Fodor, László and Bada, G and Csillag, Gábor and Horváth, Erzsébet and Ruszkiczay-Rüdiger, Zsófia and Palotás, Klára and Síkhegyi, F and Timár, Gábor and Cloetingh, S and Horváth, Ferenc},
	doi = {10.1016/j.tecto.2005.06.008},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {410},
	unique-id = {1138137},
	issn = {0040-1951},
	abstract = {Neotectonic deformation in the western and central part of the Pannonian Basin was investigated by means of surface and subsurface structural analyses, and geomorphologic observations. The applied methodology includes the study of outcrops, industrial seismic profiles, digital elevation models, topographic maps, and borehole data. Observations suggest that most of the neotectonic structures in the Pannonian Basin are related to the inverse reactivation of earlier faults formed mainly during the Miocene syn- and post-rift phases. Typical structures are folds, blind reverse faults, and transpressional strike-slip faults, although normal or oblique-normal faults are also present. These structures significantly controlled the evolution of landforms and the drainage pattern by inducing surface upwarping and river deflections. Our analyses do not support the postulated tectonic origin of some landforms, particularly that of the radial valley system in the western Pannonian Basin. The most important neotectonic strike-slip faults are trending to east-northeast and have dextral to sinistral kinematics in the south-western and central-eastern part of the studied area, respectively. The suggested along-strike change of kinematics within the same shear zones is in agreement with the fan-shaped recent stress trajectories and with the present-day motion of crustal blocks derived from GPS data.},
	year = {2005},
	eissn = {1879-3266},
	pages = {15-41},
	orcid-numbers = {Horváth, Erzsébet/0000-0002-0197-4152; Timár, Gábor/0000-0001-9675-6192}
}

@inproceedings{MTMT:1369022,
	title = {New data on neotectonic structures and morphotectonics of the western and central Pannonian basin},
	url = {https://m2.mtmt.hu/api/publication/1369022},
	author = {Fodor, László and Bada, G and Csillag, Gábor and Horváth, Erzsébet and Ruszkiczay-Rüdiger, Zsófia and Síkhegyi, F},
	booktitle = {Proceedings of the workshop on „Application of GPS in plate tectonics, in research on fossil energy resources and in earthquake hazard assessment”},
	unique-id = {1369022},
	year = {2005},
	pages = {35-44},
	orcid-numbers = {Horváth, Erzsébet/0000-0002-0197-4152}
}

@inproceedings{MTMT:1346062,
	title = {Tectonic development, morphotectonics and volcanism of the Transdanubian Range. a field guide},
	url = {https://m2.mtmt.hu/api/publication/1346062},
	author = {Fodor, László and Csillag, Gábor and Németh, Károly and Budai, Tamás and Cserny, Tibor and Martin, U and Brezsnyánszky, Károly and Dewey, J},
	booktitle = {Proceedings of the workshop on „Application of GPS in plate tectonics, in research on fossil energy resources and in earthquake hazard assessment”},
	unique-id = {1346062},
	year = {2005},
	pages = {59-86}
}

@article{MTMT:2899083,
	title = {Quaternary neotectonics of the Somogy Hills, Hungary (part I): Evidence from field observations},
	url = {https://m2.mtmt.hu/api/publication/2899083},
	author = {Magyari, A and Musitz, Balázs and Csontos, László and Van, Vliet-Lanoe B},
	doi = {10.1016/j.tecto.2005.05.044},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {410},
	unique-id = {2899083},
	issn = {0040-1951},
	abstract = {Quaternary and directly underlying Late Miocene (Pannonian) outcrops were analysed by structural, tectono-morphologic and sedimentologic methods to describe the main fault directions, to separate mass movements from faulting and folding and to separate earthquake-induced sediment deformations from other (e.g. periglacial) effects in the Somogy Hills. This is a gentle hilly area elevated at 200-300 m above sea level, located immediately south of Lake Balaton, Hungary. Quaternary outcrops showed several consistent directions of faulting, and co-depositional seismic activity. Three different Mohr-sets of faults/joints could be differentiated in Quaternary sediments. The three sets are considered Late Quaternary since all cut young loess sections and have morphological expressions. On the basis of the microtectonic measurements and morphotectonic investigations, the following sequence of Quaternary events can be proposed: 1. A (W)NW-(E)SE compression and perpendicular extension would create E-W to WNW-ESE oriented right lateral, NNW-SSE to N-S oriented left lateral shear zones, and NW-SE striking normal faults. Some of these can be evidenced in morphology and among the individual fault measurements. Some reactivated faults might suggest that this field is a relatively older one, but fresh topographic elements suggest that this stress field might be operational sub-recently. 2. A second stress field with NNW-SSE extensional and ENE-WSW oriented compressional directions could be separated. This stress field could create NNE-SSW and NW-SE oriented shear fractures and ENE-WSW oriented conjugate normal faults. Flat thrusts giving ENE directed shear may also be active under this field. 3. A third stress field might be proposed with N-S compression and perpendicular extension directions. This would create NE-SW and NW-SE oriented shear fractures, which are observed in the measured fault data. It is remarkable that the NE-SW faults are all steep, subvertical, and give a very well defined fault set. Based on the fresh topographic expression, this stress field is also sub-recent. The different sub-recent stress fields and related fault patterns might succeed each other or might alternate through time. The first and third deformations have fresh topographic expressions and cannot play synchronously. The observed features suggest a compressionally active neotectonics of the study area. (c) 2005 Published by Elsevier B.V.},
	year = {2005},
	eissn = {1879-3266},
	pages = {43-62}
}

@article{MTMT:1964562,
	title = {Késő negyedidőszaki szerkezetfejlődés vizsgálata Külső-Somogyban terepi mikro- és morfotektonikai módszerekkel},
	url = {https://m2.mtmt.hu/api/publication/1964562},
	author = {Magyar, Á and Musitz, Balázs and B., Van Vliet Laone and Csontos, László and Unger, Zoltán},
	journal-iso = {M ÁLL FÖLDT INT JELENT},
	journal = {MAGYAR ÁLLAMI FÖLDTANI INTÉZET ÉVI JELENTÉSE},
	unique-id = {1964562},
	issn = {0368-9751},
	year = {2004},
	pages = {111-128},
	orcid-numbers = {Unger, Zoltán/0000-0002-7986-7146}
}

@article{MTMT:1140404,
	title = {A földtörténet utolsó 30 ezer évének szakaszai és a futóhomok mozgásának főbb periódusai Magyarországon},
	url = {https://m2.mtmt.hu/api/publication/1140404},
	author = {Gábris, Gyula},
	journal-iso = {FÖLDRAJZI KÖZLEMÉNYEK},
	journal = {FÖLDRAJZI KÖZLEMÉNYEK},
	volume = {127 (51)},
	unique-id = {1140404},
	issn = {0015-5411},
	year = {2003},
	pages = {1-14}
}

@article{MTMT:1135541,
	title = {Ages of periods of sand movement in Hungary determined through luminescence measurements},
	url = {https://m2.mtmt.hu/api/publication/1135541},
	author = {Ujhazy, K and Gábris, Gyula and Frechen, M},
	doi = {10.1016/S1040-6182(03)00017-X},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {111},
	unique-id = {1135541},
	issn = {1040-6182},
	abstract = {The Late Glacial and Holocene climatic oscillations in Hungary are
		manifested by changing fluvial and aeolian sand deposition, as well as
		by intercalated soil formations. The sand-blown territories have
		special interest since the buried fossil soils provide detailed
		information about climate and environment changes. During the past two
		decades the time of the sand-moving periods was studied exclusively by
		radiocarbon age determination, but by now, thanks to the latest
		investigations, these results have been controlled and completed by the
		thermoluminescence and infrared optically stimulated luminescence
		dating methods. These techniques have been applied to provide a more
		detailed chronological framework for Late Pleistocene and Holocene sand
		accumulation periods. Five aeolian sand accumulation periods can be
		recognized covering the Late Glacial and Holocene time period at
		14.0+/-2.3, 12.0 +/- 1.9, 9.2 +/- 1.7, 6.0 +/- 0.5 and 0.6 +/- 0.07 ka.
		The sand-blown formations are intercalated by soil horizons. The
		radiocarbon age estimates provide evidence for Late Glacial (Bolling,
		Allerod) and Lower-Atlantic soil-forming periods. (C) 2003 Elsevier
		Science Ltd and INQUA. All rights reserved.},
	year = {2003},
	eissn = {1873-4553},
	pages = {91-100}
}

@inbook{MTMT:1834869,
	title = {A Kárpát-medence domborzatformálódása a késő kainozoikumban és a pliocén időszak},
	url = {https://m2.mtmt.hu/api/publication/1834869},
	author = {Schweitzer, Ferenc},
	booktitle = {Területfejlesztés - regionális kutatások},
	unique-id = {1834869},
	year = {2000},
	pages = {13-29}
}

@inbook{MTMT:25807,
	title = {Geomorphological and stratigraphical significance of Pliocene red clay in Hungary},
	url = {https://m2.mtmt.hu/api/publication/25807},
	author = {Schweitzer, Ferenc and Szöőr, Gy},
	booktitle = {Geomorphology and changing environments in Central Europe},
	unique-id = {25807},
	year = {1997},
	pages = {95-105}
}

@inbook{MTMT:25806,
	title = {On late Miocene - early Pliocene desert climate in the Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/25806},
	author = {Schweitzer, Ferenc},
	booktitle = {Geomorphology and changing environments in Central Europe},
	unique-id = {25806},
	year = {1997},
	pages = {37-43}
}

@mastersthesis{MTMT:25886,
	title = {Domborzatformálódás a Pannóniai-medence belsejében a fiatal újkorban és a negyedidőszak határán},
	url = {https://m2.mtmt.hu/api/publication/25886},
	author = {Schweitzer, Ferenc},
	unique-id = {25886},
	year = {1994}
}

@misc{MTMT:1852021,
	title = {A Balatoni üdülőkörzet környezetföldtani térképsorozat},
	url = {https://m2.mtmt.hu/api/publication/1852021},
	author = {Chikán, G and Cserny, Tibor and Farkas, P and Kuti, L},
	unique-id = {1852021},
	year = {1988}
}

@article{MTMT:1664894,
	title = {PHASES OF BLOWN-SAND MOVEMENTS IN THE NORTH-EAST PART OF THE GREAT HUNGARIAN PLAIN.},
	url = {https://m2.mtmt.hu/api/publication/1664894},
	author = {Borsy, Z and Csongor, Éva and Sárkány, S and Szabó, Ilona},
	journal-iso = {ACTA GEOGR DEBR},
	journal = {ACTA GEOGRAPHICA AC GEOLOGICA ET METEOROLOGICA DEBRECINA},
	volume = {20},
	unique-id = {1664894},
	issn = {0209-9004},
	year = {1982},
	pages = {5}
}

@misc{MTMT:1346352,
	title = {Magyarázó a Balaton környékének M=1:20 000-es építésföldtani térképsorozatához},
	url = {https://m2.mtmt.hu/api/publication/1346352},
	author = {Papp, P and Farkas, P and Csillag, Gábor and Boros, J and Cserny, Tibor and Kurimay, Á and Zaránd, Cs and Varga, Jné},
	unique-id = {1346352},
	year = {1980}
}

@misc{MTMT:1346340,
	title = {Magyarázó a Balaton környékének 1:10 000-es építésföldtani térképsorozatához},
	url = {https://m2.mtmt.hu/api/publication/1346340},
	author = {Cserny, Tibor},
	unique-id = {1346340},
	year = {1975}
}

@mastersthesis{MTMT:1432134,
	title = {Hazánk folyóhálózatának kialakulása},
	url = {https://m2.mtmt.hu/api/publication/1432134},
	author = {Somogyi, Sándor},
	unique-id = {1432134},
	year = {1961}
}