@article{MTMT:1712195,
	title = {Wind erosion under cold climate: A Pleistocene periglacial mega-yardang system in Central Europe (Western Pannonian Basin, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1712195},
	author = {Sebe, Krisztina and Csillag, Gábor and Ruszkiczay-Rüdiger, Zsófia and Fodor, László and Thamóné Bozsó, Edit and Müller, P and Braucher, R},
	doi = {10.1016/j.geomorph.2011.08.003},
	journal-iso = {GEOMORPHOLOGY},
	journal = {GEOMORPHOLOGY},
	volume = {134},
	unique-id = {1712195},
	issn = {0169-555X},
	keywords = {REGION; DISCRIMINATION; LUMINESCENCE; RECONSTRUCTION; climate; DISTRIBUTIONS; wind erosion; wind erosion; PLEISTOCENE; Pannonian Basin; Quaternary; DESERT; LANDSCAPE; MIDDLE; Periglacial; Yardang; loess; Vardang},
	year = {2011},
	eissn = {1872-695X},
	pages = {470-482},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1447813,
	title = {A szélerózió szerepe a Dunántúl negyedidőszaki felszínfejlődésében.},
	url = {https://m2.mtmt.hu/api/publication/1447813},
	author = {Csillag, Gábor and Fodor, László and Sebe, Krisztina and Müller, P and Ruszkiczay-Rüdiger, Zsófia and Thamóné Bozsó, Edit and Bada, G},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {140},
	unique-id = {1447813},
	issn = {0015-542X},
	year = {2010},
	eissn = {2559-902X},
	pages = {463-482},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1354802,
	title = {Fiatal tektonikai jelenségek új észlelései a Nyugati-Mecsekben és környezetében},
	url = {https://m2.mtmt.hu/api/publication/1354802},
	author = {Konrád, Gyula and Sebe, Krisztina},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {140},
	unique-id = {1354802},
	issn = {0015-542X},
	abstract = {Exposures of Neogene and Quaternary age were investigated along the main structural zones of the Western Mecsek
		Mts. (SW Hungary) in order to study post-Miocene tectonic activity, with an aim of supplementing studies on the longterm
		stability of the region. Field observations showed that young movements affected only the mountain fronts and the
		foreland. From the 24 studied exposures, those with impacts of tectonic activity were located along the major fault zones
		of the Western Mecsek Mts. and prove tectonic/seismic events occurring as late as the Late Pleistocene along the
		Mecsekalja Dislocation Zone and probably the Hetvehely–Magyarszék Fault. On the contrary, no impact of neotectonic
		activity was found within the Western Mecsek Anticline, indicating that this area behaved as a single solid block during
		post-Miocene movements. Since the Karpatian age, 5 tectonic phases could be distinguished. From these – somewhat
		opposing previous research – transtension seems typical for the Karpatian along the Hetvehely–Magyarszék Fault. The
		Early Pannonian transtensional stress field did not cease to exist at the beginning of the Late Pannonian. Tectonic
		inversion started only within the first half of the Late Pannonian and can be considered active up to present day in the
		major part of the area.
		
		A munka során a Nyugat-Mecsek fő szerkezeti vonalainak környezetében feltárt neogén és kvarter képződményeket
		vizsgáltuk fiatal (posztpannóniai) tektonikai aktivitás nyomai után kutatva, elsősorban a terület hosszú távú
		stabilitásának megítéléséhez. A terepi megfigyelések alapján a fiatal mozgások csak a hegységperemet és az előteret
		érintették. A vizsgált 24 feltárásból a fiatal tektonikával érintettek a Nyugat-Mecsek meghatározó szerkezeti vonalai
		mentén helyezkednek el, és még a késő-pleisztocénben is szerkezeti mozgásokat, illetve szeizmikus aktivitást
		bizonyítanak a Mecsekalja-öv és valószínűleg a Hetvehely–magyarszéki-törés mentén. Ezzel ellentétben a Nyugatmecseki-
		antiklinális területén belül neotektonikára utaló jeleket nem észleltünk, ez alapján a pannóniai–negyedidőszaki
		mozgások során a Nyugat-Mecsek egységes tömbként viselkedhetett.
		A kárpáti korszak óta öt tektonikai fázis volt elkülöníthető a területen. Ezek közül – a korábbi vizsgálati
		eredményekkel szemben – a kárpáti korszakra jellemzőnek tűnik a transztenzió a Hetvehely–magyarszéki-törés
		mentén. A kora-pannóniai transztenziós feszültségtér a Mecsekalja-öv mentén még a késő-pannóniai elején is
		fennállt. Az inverzió a késő-pannóniai első felében kezdődött és a terület legnagyobb részén máig aktívnak
		tekinthető.},
	year = {2010},
	eissn = {2559-902X},
	pages = {135-161},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1110974,
	title = {Grain-size analysis of the Neogene red clay formation in the Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/1110974},
	author = {Kovács, János},
	doi = {10.1007/s00531-006-0150-2},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {97},
	unique-id = {1110974},
	issn = {1437-3254},
	year = {2008},
	eissn = {1437-3262},
	pages = {171-178},
	orcid-numbers = {Kovács, János/0000-0001-7742-5515}
}

@article{MTMT:2972525,
	title = {Late Pleistocene loess-palaeosol sequences in the Vojvodina region, north Serbia},
	url = {https://m2.mtmt.hu/api/publication/2972525},
	author = {Marković, S B and Bokhorst, M P and Vandenberghe, J and McCoy, W D and Oches, E A and Hambach, U and Gaudenyi, Tivadar and Jovanović, M and Zöller, L and Stevens, T and Machallet, B},
	doi = {10.1002/jqs.1124},
	journal-iso = {J QUATERNARY SCI},
	journal = {JOURNAL OF QUATERNARY SCIENCE},
	volume = {23},
	unique-id = {2972525},
	issn = {0267-8179},
	year = {2008},
	eissn = {1099-1417},
	pages = {73-84}
}

@CONFERENCE{MTMT:1422047,
	title = {OSL age data to Quaternary landscape evolution in the forelands of Vértes Hills (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1422047},
	author = {Thamóné Bozsó, Edit and Csillag, Gábor and Fodor, László and Müller, P and Nagy, Attila},
	booktitle = {12th International Conference on Luminescence and Electron Spin Resonance Dating},
	unique-id = {1422047},
	year = {2008},
	pages = {152}
}

@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}
}

@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}
}

@article{MTMT:1177762,
	title = {The full-glacial forests of central and southeastern Europe},
	url = {https://m2.mtmt.hu/api/publication/1177762},
	author = {Willis, KJ and Rudner, Edina and Sümegi, Pál},
	doi = {10.1006/qres.1999.2119},
	journal-iso = {QUATERNARY RES},
	journal = {QUATERNARY RESEARCH},
	volume = {53},
	unique-id = {1177762},
	issn = {0033-5894},
	year = {2000},
	eissn = {1096-0287},
	pages = {203-213},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}