@mastersthesis{MTMT:2709552,
	title = {Egy Tisza-völgyi pleisztocén folyó rekonstrukciója ultranagy felbontású szeizmikus szelvények alapján. Morfometriai elemzések a paleoklíma becsléséhez},
	url = {https://m2.mtmt.hu/api/publication/2709552},
	author = {Cserkész-Nagy, Ágnes},
	unique-id = {2709552},
	year = {2014}
}

@mastersthesis{MTMT:2974032,
	title = {Ártérfejlődési vizsgálatok felső-tiszai mintaterületeken},
	url = {https://m2.mtmt.hu/api/publication/2974032},
	author = {Vass, Róbert},
	unique-id = {2974032},
	year = {2014}
}

@article{MTMT:2141556,
	title = {Tectonically controlled Quaternary intracontinental fluvial sequence development in the Nyírség–Pannonian Basin, Hungary},
	url = {https://m2.mtmt.hu/api/publication/2141556},
	author = {Püspöki, Zoltán and Demeter, Gábor and Tóthné, Makk Ágnes and Kozák, Miklós and Dávid, Árpád and Virág, Margit and Kovács-Pálffy, Péter and Kónya, Péter and Gyuricza, György and Kiss, János and McIntosh, Richard William and Forgács, Zoltán and Buday, Tamás and Kovács, Zoltán and Gombos, T. and Kummer, István},
	doi = {10.1016/j.sedgeo.2012.11.003},
	journal-iso = {SEDIMENT GEOL},
	journal = {SEDIMENTARY GEOLOGY},
	volume = {283},
	unique-id = {2141556},
	issn = {0037-0738},
	abstract = {The Quaternary fluvial succession of the Nyirseg (NE Hungary), a proximal sub-basin of 4000 km(2) in the intracontinental Pannonian Basin, was studied based on log facies analysis. Regional mapping of sequences was established by analysis of fully cored boreholes and high scale local correlations in densely drilled areas. The age of the sequences was determined by correlating the magnetic susceptibility (MS) record of the fully cored boreholes with that of the reference Hungarian boreholes dated paleomagnetically (Devavanya-1 and Veszto-1 in Cooke et al., 1979). To give the Hungarian data global perspective they were correlated to the MS curve of the Chinese Loess (Ding et al., 2005) that are in turn correlated with the Marine Isotope Record (Lisiecki and Raymo, 2005; Gibbard and Cohen, 2008).The ages of the mapped sequence boundaries are 2.62, 226, 2.12, 1.22, 1.04, 0.58 and 0.34 Ma respectively and can be related to the transitions from cool to warm conditions. Regional unconformities at 2.26-2.12, 122 and 0.58 Ma also coincide with activity maxima of the radiometrically dated Quaternary volcanism. This high frequency of climatically controlled erosive sequence boundaries in the structurally active periods indicates that the sedimentary record of climatic erosion is better expressed in times when structural changes generate instability in the drainage network. The occurrence of packages of regional unconformities in relation to volcanic activity enables the geochronological dating of episodes in the Quaternary compression of the Carpathian-Pannonian region.The role of tectonic control on the climatically induced changes in the drainage network has been explained by a structural development model based on seismic, gravity and magnetic data. The changes in the local paleohydrology were triggered by a compression related elevation of the basement and the associated occurrence of a local transtension-related subsidence. (C) 2012 Elsevier B.V. All rights reserved.},
	keywords = {Hungary; Quaternary; Magnetic susceptibility; Sequence stratigraphy; TERRESTRIAL; Tectonic episodes},
	year = {2013},
	eissn = {1879-0968},
	pages = {34-56},
	orcid-numbers = {Kiss, János/0000-0001-8589-1364}
}

@article{MTMT:2051922,
	title = {Reconstruction of a Pleistocene meandering river in East Hungary by VHR seismic images, and its climatic implications},
	url = {https://m2.mtmt.hu/api/publication/2051922},
	author = {Cserkész-Nagy, Ágnes and Thamóné Bozsó, Edit and Toth, T and Sztanó, Orsolya},
	doi = {10.1016/j.geomorph.2012.02.025},
	journal-iso = {GEOMORPHOLOGY},
	journal = {GEOMORPHOLOGY},
	volume = {153},
	unique-id = {2051922},
	issn = {0169-555X},
	abstract = {The upper 20-30 m of the Pleistocene alluvial sequence on the Tisza River, Hungary is investigated by 200 km of VHR single-channel seismic sections. Frequent internal configurations, such as (1) bundles of inclined reflections, (2) trough-shaped converging, and (3) horizontal, parallel reflections are interpreted, respectively, as lateral accretion of point bars, abandoned channel fills and floodplain deposits. The series of 5-8 m-thick inclined strata sets occurring at the same depth throughout the area suggest the presence of a meandering river dated to about 43-47 ka in the Late Pleistocene according to OSL data. Newly recorded quasi-3D seismic profiles reveal that each 1-3 km-long inclined series correlates with an individual point bar continuously migrating in the same direction. Small deviations in the direction of migration are caused by natural wandering of the meander bend. Morphometric parameters of point bars are used to calculate ancient channel parameters (width and depth of 200-500 m and 5-8 m, respectively). Values imply a channel-forming discharge of Q=400-900 m(3)/s. These results imply a greater amount of runoff and supply in the basin during MIS3 compared to the present day. Long-lasting meandering indicates the role of local factors and a different fluvial environment compared to the commonly anastomosing systems in NW Europe. Our data support the thesis of the three-axis drainage system for the basin. New evidence is provided for the antecedent existence of a temporally active third trunk river in addition to the ancestors of Danube and Tisza Rivers, contrary to the present-day two-axis drainage pattern. (C) 2012 Elsevier B.V. All rights reserved.},
	year = {2012},
	eissn = {1872-695X},
	pages = {205-218},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:2124003,
	title = {Holocene aeolian sand mobilization, vegetation history and human impact on the stabilized sand dune area of the southern Nyírség, Hungary},
	url = {https://m2.mtmt.hu/api/publication/2124003},
	author = {Kiss, Tímea and Sipos, György and Mauz, B and Mezősi, Gábor},
	doi = {10.1016/j.yqres.2012.07.002},
	journal-iso = {QUATERNARY RES},
	journal = {QUATERNARY RESEARCH},
	volume = {78},
	unique-id = {2124003},
	issn = {0033-5894},
	year = {2012},
	eissn = {1096-0287},
	pages = {492-501},
	orcid-numbers = {Kiss, Tímea/0000-0002-2597-5176; Sipos, György/0000-0001-6224-2361}
}

@article{MTMT:1384390,
	title = {Geomorphometric floodplain classification in a hill region of Hungary},
	url = {https://m2.mtmt.hu/api/publication/1384390},
	author = {Lóczy, Dénes and Pirkhoffer, Ervin and Gyenizse, Péter},
	doi = {10.1016/j.geomorph.2011.06.040},
	journal-iso = {GEOMORPHOLOGY},
	journal = {GEOMORPHOLOGY},
	volume = {147-148},
	unique-id = {1384390},
	issn = {0169-555X},
	year = {2012},
	eissn = {1872-695X},
	pages = {61-72},
	orcid-numbers = {Lóczy, Dénes/0000-0002-2542-6775; Pirkhoffer, Ervin/0000-0003-2917-3290; Gyenizse, Péter/0000-0002-8175-9734}
}

@article{MTMT:1846857,
	title = {Rapid vegetation response to lateglacial and early Holocene climatic fluctuation in the South Carpathian Mountains (Romania).},
	url = {https://m2.mtmt.hu/api/publication/1846857},
	author = {Magyari, Enikő Katalin and Jakab, Gusztáv and Bálint, M and Kern, Zoltán and Buczkó, Krisztina and Braun, Mihály},
	doi = {10.1016/j.quascirev.2012.01.006},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {35},
	unique-id = {1846857},
	issn = {0277-3791},
	year = {2012},
	eissn = {1873-457X},
	pages = {116-130},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Jakab, Gusztáv/0000-0002-2569-5967; Kern, Zoltán/0000-0003-4900-2587}
}

@article{MTMT:1368443,
	title = {Quantification of Quaternary vertical movements in the central Pannonian Basin: A review of chronologic data along the Danube River, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1368443},
	author = {Ruszkiczay-Rüdiger, Zsófia and Fodor, László and Bada, G and Leél-Őssy, Szabolcs and Horváth, Erzsébet and Dunai, TJ},
	doi = {10.1016/j.tecto.2005.05.048},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {410},
	unique-id = {1368443},
	issn = {0040-1951},
	year = {2005},
	eissn = {1879-3266},
	pages = {157-172},
	orcid-numbers = {Horváth, Erzsébet/0000-0002-0197-4152}
}

@article{MTMT:1184717,
	title = {A magyaroszági würm korú löszök képződésének paleoökológiai rekonstrukciója Mollusca-fauna alapján},
	url = {https://m2.mtmt.hu/api/publication/1184717},
	author = {Sümegi, Pál and Krolopp, E},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {125},
	unique-id = {1184717},
	issn = {0015-542X},
	year = {1995},
	eissn = {2559-902X},
	pages = {125-148},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1043576,
	title = {Szeged geomorfológiai vázlata},
	url = {https://m2.mtmt.hu/api/publication/1043576},
	author = {Mezősi, Gábor},
	journal-iso = {ALFÖLDI TANULMÁNYOK},
	journal = {ALFÖLDI TANULMÁNYOK},
	volume = {7},
	unique-id = {1043576},
	issn = {0139-3545},
	year = {1983},
	pages = {59-74}
}