@article{MTMT:1370895,
	title = {Uranium-series dating of travertine from Sutto: Implications for reconstruction of environmental change in Hungary},
	url = {https://m2.mtmt.hu/api/publication/1370895},
	author = {Sierralta, M and Kele, Sándor and Melcher, F and Hambach, U and Reinders, J and van Geldern, R and Frechen, M},
	doi = {10.1016/j.quaint.2009.04.004},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {222},
	unique-id = {1370895},
	issn = {1040-6182},
	year = {2010},
	eissn = {1873-4553},
	pages = {178-193},
	orcid-numbers = {Kele, Sándor/0000-0002-8607-7636}
}

@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}
}

@inbook{MTMT:1138114,
	title = {Societal aspects of ongoing deformation in the Pannonian region},
	url = {https://m2.mtmt.hu/api/publication/1138114},
	author = {Bada, G and Horváth, Ferenc and Tóth, László and Fodor, László and Timár, Gábor and Cloetingh, S},
	booktitle = {The Adria Microplate: GPS Geodesy, Tectonics and Hazards},
	doi = {10.1007/1-4020-4235-3_26},
	unique-id = {1138114},
	year = {2006},
	pages = {385-402},
	orcid-numbers = {Timár, Gábor/0000-0001-9675-6192}
}

@article{MTMT:1369376,
	title = {Tertiary tectonic evolution of the Pannonian-Carpathian-Eastern Alpine domain: A personal view from Pannonia in the light of the terminologial question of tectonic units},
	url = {https://m2.mtmt.hu/api/publication/1369376},
	author = {Fodor, László},
	journal-iso = {GEOLINES},
	journal = {GEOLINES},
	volume = {20},
	unique-id = {1369376},
	issn = {1210-9606},
	year = {2006},
	pages = {34-36}
}

@article{MTMT:1138162,
	title = {Comparative volumetric calculations of two segments of the Carpathian Neogene/Quaternary volcanic chain using SRTM elevation data: implications for erosion and magma output rates},
	url = {https://m2.mtmt.hu/api/publication/1138162},
	author = {Karátson, Dávid and Timár, Gábor},
	journal-iso = {Z GEOMORPH SUPPL},
	journal = {ZEITSCHRIFT FUR GEOMORPHOLOGIE SUPPLEMENTBAND},
	volume = {140},
	unique-id = {1138162},
	issn = {0044-2798},
	year = {2005},
	pages = {19-35},
	orcid-numbers = {Karátson, Dávid/0000-0003-0386-1239; Timár, Gábor/0000-0001-9675-6192}
}

@article{MTMT:1329291,
	title = {Application of digital terrain modelling and GIS methods for the morphotectonic investigation of the Kali Basin, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1329291},
	author = {Jordán, Győző and Csillag, Gábor and Szűcs, Andrea and Qvarfort, U},
	journal-iso = {Z GEOMORPHOL},
	journal = {ZEITSCHRIFT FÜR GEOMORPHOLOGIE},
	volume = {47},
	unique-id = {1329291},
	issn = {0372-8854},
	abstract = {The objective of this study was to apply detailed digital terrain modelling to the DEM of the Kali Basin, Hungary, and to study morphological features associated with tectonic structures. Methodology is based on the numerical differential geometry and statistical approach of general geomorphometry. Methods specific to digital terrain modelling, such as shaded relief models, vertical exaggeration, morphological cross-sections and 3D display with image drape are also applied. Resulting terrain models are processed by means of digital image processing techniques to enhance visual interpretation. Characteristic morphological features associated with known faults such as linear valleys, ridgelines and slope-breaks, uniform aspect and steep slopes, morphological depressions and tilt of terrain are subsequently studied. Geological and structural data of various sources and scales, such as geophysical measurements, geological maps and drill core data, existing lineament maps and hydrological data are integrated in a GIS database. Overlay and tectonic interpretation of multi-source information confirmed the findings of morphotectonic analysis. Digital morphotectonic investigation shows that tectonic structures known from previous studies have morphological expressions in the Kali Basin. A simple shear model with principal displacement zone in the NE-SW direction with restraining and releasing bends can explain most of the morphotectonic features associated with structures identified by geological and digital morphotectonic investigations.},
	year = {2003},
	eissn = {1864-1687},
	pages = {145-169}
}

@article{MTMT:1385210,
	title = {Calculation of Erosion Rates Based on Remnants of Mono-genetic Alkaline Basaltic Volcanoes in the Bakony–Balaton Highland Volcanic Field (Western Hungary) of Mio/Pliocene Age},
	url = {https://m2.mtmt.hu/api/publication/1385210},
	author = {Németh, Károly and MARTIN, U and Csillag, Gábor},
	journal-iso = {GEOLINES},
	journal = {GEOLINES},
	volume = {15},
	unique-id = {1385210},
	issn = {1210-9606},
	year = {2003},
	pages = {102-106}
}

@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}
}

@mastersthesis{MTMT:30721230,
	title = {A Pesti-síkság fiatal-harmadidőszaki és negyedidőszaki kavicsképződményeinek összehasonlító vizsgálata},
	url = {https://m2.mtmt.hu/api/publication/30721230},
	author = {Burján, Balázs},
	publisher = {SZTE},
	unique-id = {30721230},
	year = {2002}
}

@article{MTMT:1368976,
	title = {Pliocene-Quaternary landscape evolution and deformation in the eastern Vértes Hills, (Hungary): the heritage and reactivation of Miocene fault pattern},
	url = {https://m2.mtmt.hu/api/publication/1368976},
	author = {Csillag, Gábor and Fodor, László and Peregi, Zs and Roth, L and Selmeczi, Ildikó},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {53},
	unique-id = {1368976},
	issn = {1335-0552},
	year = {2002},
	eissn = {1336-8052},
	pages = {206-208}
}

@article{MTMT:1419807,
	title = {Seismicity in the Pannonian Region - earthquake data},
	url = {https://m2.mtmt.hu/api/publication/1419807},
	author = {Tóth, László and Mónus, Péter and Zsíros, Tibor and Marótiné Kiszely, Márta},
	journal-iso = {EGU STEPHAN MUELLER SPEC PUBL SER},
	journal = {EGU STEPHAN MUELLER SPECIAL PUBLICATION SERIES},
	volume = {3},
	unique-id = {1419807},
	issn = {1868-4556},
	year = {2002},
	eissn = {1868-4564},
	pages = {9-28}
}

@article{MTMT:1353324,
	title = {Baradla-barlangi cseppkőkoradatok a késő-negyedidőszaki klímaingadozások tükrében},
	url = {https://m2.mtmt.hu/api/publication/1353324},
	author = {ZÁMBÓ, L and FORD, D and Telbisz, Tamás Ferenc},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {132},
	unique-id = {1353324},
	issn = {0015-542X},
	year = {2002},
	eissn = {2559-902X},
	pages = {231-238},
	orcid-numbers = {Telbisz, Tamás Ferenc/0000-0003-4471-2889}
}

@mastersthesis{MTMT:1140531,
	title = {A folyóvíz felszínalakító tevékenysége Magyarországon},
	url = {https://m2.mtmt.hu/api/publication/1140531},
	author = {Gábris, Gyula},
	unique-id = {1140531},
	year = {2001}
}

@article{MTMT:2321065,
	title = {Vulkáni törmeléklavinák: általános jellemzők, ismert példák, magyarországi előfordulások},
	url = {https://m2.mtmt.hu/api/publication/2321065},
	author = {Karátson, Dávid},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {131},
	unique-id = {2321065},
	issn = {0015-542X},
	year = {2001},
	eissn = {2559-902X},
	pages = {253-283},
	orcid-numbers = {Karátson, Dávid/0000-0003-0386-1239}
}

@article{MTMT:1353326,
	title = {Új megközelítések a töbör-morfológiában az Aggteleki-karszt példáján},
	url = {https://m2.mtmt.hu/api/publication/1353326},
	author = {Telbisz, Tamás Ferenc},
	journal-iso = {FÖLDRAJZI KÖZLEMÉNYEK},
	journal = {FÖLDRAJZI KÖZLEMÉNYEK},
	volume = {125},
	unique-id = {1353326},
	issn = {0015-5411},
	year = {2001},
	pages = {95-108},
	orcid-numbers = {Telbisz, Tamás Ferenc/0000-0003-4471-2889}
}

@inbook{MTMT:1369059,
	title = {Tertiary tectonic evolution of the Pannonian Basin system and neighbouring orogens: a new synthesis of palaeostress data},
	url = {https://m2.mtmt.hu/api/publication/1369059},
	author = {Fodor, László and Csontos, L and Bada, G and Györfi, I and Benkovics, L},
	booktitle = {The Mediterranean Basins: tertiary extension within the Alpine Orogen},
	doi = {10.1144/GSL.SP.1999.156.01.15},
	unique-id = {1369059},
	year = {1999},
	pages = {295-334}
}

@CONFERENCE{MTMT:1384939,
	title = {AN ANCIENT DEBRIS AVALANCHE INITIATED THE RIVER LOOP? THE MYSTERY OF THE DANUBE BEND, HUNGARY},
	url = {https://m2.mtmt.hu/api/publication/1384939},
	author = {Karátson, Dávid and Németh, Károly and Józsa, Sándor and BORBÉLY, E},
	booktitle = {EUROPEAN UNION OF GEOSCIENCES CONFERENCE},
	unique-id = {1384939},
	year = {1999},
	pages = {320-320},
	orcid-numbers = {Karátson, Dávid/0000-0003-0386-1239; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:1890263,
	title = {Paleogeographic evolution of the Late Miocene Lake Pannon in Central Europe},
	url = {https://m2.mtmt.hu/api/publication/1890263},
	author = {Magyar, Imre and Geary, DH and Muller, P},
	doi = {10.1016/S0031-0182(98)00155-2},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {147},
	unique-id = {1890263},
	issn = {0031-0182},
	abstract = {The paleogeographic evolution of Lake Pannon within the Pannonian basin is reconstructed with eight maps, ranging from the Middle Miocene to the Early Pliocene. The maps are based on the distribution of selected biozones and specific fossils, and on complementary sedimentological and seismic information. Our reconstruction shows that the history of Lake Pannon can be divided into three distinct intervals: an initial stage with low water level, which resulted in isolation from the sea at about 12 Ma and might have led to temporary fragmentation of the lake; an interval of gradual transgression lasting until ca. 9.5 Ma; and a long late interval of shrinkage and infilling of sediments that persisted into the Early Pliocene. The deep subbasins of the lake formed during the transgressive interval, in more basinward locations than the deep basins of the preceding Sarmatian age. The southern shoreline, running parallel with the Sava and Danube rivers along the northern foot of the Dinarides, changed very Little during the Lifetime of the lake, while the northern shoreline underwent profound changes. (C) 1999 Elsevier Science B.V. All rights reserved.},
	keywords = {BASIN; Pannonian Basin; Neogene; Lakes; paleogeography; Paratethys; biogeography},
	year = {1999},
	eissn = {1872-616X},
	pages = {151-167}
}

@article{MTMT:1384635,
	title = {Large hydrovolcanic field in the Pannonian Basin: general characteristics of the Bakony-Balaton Highland Volcanic Field, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1384635},
	author = {Németh, Károly and Martin, U},
	journal-iso = {ACTA VULCANOL},
	journal = {ACTA VULCANOLOGICA},
	volume = {11},
	unique-id = {1384635},
	issn = {1121-9114},
	year = {1999},
	eissn = {1724-0425},
	pages = {271-282}
}

@article{MTMT:1135539,
	title = {Geochronology of Middle and Upper Pleistocene Loess sections in Hungary},
	url = {https://m2.mtmt.hu/api/publication/1135539},
	author = {Frechen, M and Horváth, Erzsébet and Gábris, Gyula},
	doi = {10.1006/qres.1997.1929},
	journal-iso = {QUATERNARY RES},
	journal = {QUATERNARY RESEARCH},
	volume = {48},
	unique-id = {1135539},
	issn = {0033-5894},
	abstract = {The application of both thermoluminescence and infrared stimulated
		luminescence dating to the extensively studied "classical" Hungarian
		loess/paleosol sequences from Basaharc, Mende, and Paks provides a
		reliable chronological framework and climatostratigraphic
		reconstruction for the last interglacial/glacial cycle. Based on this
		combined luminescence dating study a new chronology is proposed for the
		"Young Loess" in Hungary. Luminescence dating suggests that the loess
		below the MF2 horizon formed during the penultimate glaciation. The MF1
		horizon probably formed during an interstade within oxygen isotope
		stage 3. For the youngest loess, overlying MFI, a very high
		accumulation rate was determined. Large time gaps occur above MF2 and
		MF1, indicating that most of the record of the Last glaciation is
		missing in the standard sections at Basaharc, Mende, and Paks. Either
		large discontinuities or a very low accumulation rate occurred in all
		three type sections during the soil-forming periods. High-resolution
		studies of climatic proxies using this combined luminescence dating
		approach provide a reliable chronological framework for loess and loess
		derivatives of the last glacial cycle in Hungary, although a precise
		and complete chronostratigraphic reconstruction cannot be achieved from
		the incomplete records found at these sites. (C) 1997 University of
		Washington.},
	year = {1997},
	eissn = {1096-0287},
	pages = {291-312},
	orcid-numbers = {Horváth, Erzsébet/0000-0002-0197-4152}
}

@article{MTMT:1140415,
	title = {Gondolatok a folyóteraszokról},
	url = {https://m2.mtmt.hu/api/publication/1140415},
	author = {Gábris, Gyula},
	journal-iso = {FÖLDRAJZI KÖZLEMÉNYEK},
	journal = {FÖLDRAJZI KÖZLEMÉNYEK},
	volume = {121 (45)},
	unique-id = {1140415},
	issn = {0015-5411},
	year = {1997},
	pages = {3-16}
}

@article{MTMT:1724097,
	title = {Geomorfológiai megfigyelések a Szentendrei-szigeten},
	url = {https://m2.mtmt.hu/api/publication/1724097},
	author = {Mari, László},
	journal-iso = {FÖLDRAJZI KÖZLEMÉNYEK},
	journal = {FÖLDRAJZI KÖZLEMÉNYEK},
	volume = {CXX.},
	unique-id = {1724097},
	issn = {0015-5411},
	year = {1997},
	pages = {217-233},
	orcid-numbers = {Mari, László/0000-0002-3382-7800}
}

@article{MTMT:1738851,
	title = {Rates and factors of stratovolcano degradation in a continental climate: a complex morphometric analysis of nineteen Neogene/Quaternary crater remnants in the Carpathians},
	url = {https://m2.mtmt.hu/api/publication/1738851},
	author = {Karátson, Dávid},
	doi = {10.1016/0377-0273(96)00016-9},
	journal-iso = {J VOLCANOL GEOTH RES},
	journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH},
	volume = {73},
	unique-id = {1738851},
	issn = {0377-0273},
	year = {1996},
	eissn = {1872-6097},
	pages = {65-78},
	orcid-numbers = {Karátson, Dávid/0000-0003-0386-1239}
}

@article{MTMT:1135538,
	title = {Pleistocene evolution of the Danube in the Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/1135538},
	author = {Gábris, Gyula},
	doi = {10.1111/j.1365-3121.1994.tb00893.x},
	journal-iso = {TERRA NOVA},
	journal = {TERRA NOVA},
	volume = {6},
	unique-id = {1135538},
	issn = {0954-4879},
	abstract = {The present-day drainage system of the Carpathian Basin originates from
		the gradual regression of the last marine transgression (brackish
		Pannonian Sea). The flow directions of the rivers including the Danube,
		are determined by the varying rates and locations of subsidence within
		the region. The Danube, which forms the main axis of the drainage
		network, first filled the depression of the Little Plain Lake and then,
		further southward, the Slavonian Lake. From the end of the Pliocene,
		the crustal movements which caused the uplift of the Transdanubian
		Mountains, forced the Danube to flow in an easterly direction, towards
		the antecedent Visegrad Gorge, and into the subsiding basins of the
		Great Plain. Climatic changes during the Pleistocene had the effect of
		forming up to seven fluvial terraces. The uplift of the mountains is
		demonstrated by the deformation of the terraces, while the subsidence
		of the Plains is proven by an accumulation of several hundred metres of
		sediment. The river only occupied its present position south of
		Budapest in the latest Pleistocene.},
	year = {1994},
	eissn = {1365-3121},
	pages = {495-501}
}

@article{MTMT:1135590,
	title = {A physical geographical sketch of the Hungarian Ipoly Valley},
	url = {https://m2.mtmt.hu/api/publication/1135590},
	author = {Gábris, Gyula and Papp, S and Mari, László and Santa, A},
	journal-iso = {ANN UNIV SCI BP R EÖTVÖS NOM SECT GEOGR},
	journal = {ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLANDO EÖTVÖS NOMINATAE - SECTIO GEOGRAPHICA},
	volume = {22-23},
	unique-id = {1135590},
	issn = {0524-8965},
	abstract = {The Hungarian-Czechoslovak border runs on a long section along the Ipoly river. This may be a reason for the incompleteness of the physical geographical studies concerning this river. The relative proximity to Budapest and the numerous debated issues, however, made the left side of the valley the site of regular field-trips of the Budapest University. With our complex investigations we advanced from the mouth to Ipolytarnoc (where the river, rising in the Vepor Mountains, enters Hungary) over a period of six years, performing geomorphological, plant and soil geographical and hydrogeographical observations and sampling. The results allow a preliminary sketch to be drawn up of the terrace system of the Ipoly river and the plant and soil geography. -after Authors},
	year = {1993},
	pages = {57-66},
	orcid-numbers = {Mari, László/0000-0002-3382-7800}
}

@article{MTMT:1892924,
	title = {A Prosodacnomyák rétegtani jelentősége a Kötcse környéki pannóniai s.l. üledékekben. Stratigraphic significance of the Upper Miocene lacustrine Cardiid Prosodacnomya (Kötcse section, Pannonian basin, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1892924},
	author = {Müller, P and Magyar, Imre},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {122},
	unique-id = {1892924},
	issn = {0015-542X},
	year = {1992},
	eissn = {2559-902X},
	pages = {1-38}
}

@article{MTMT:1855796,
	title = {REVIEW OF NEOGENE AND QUATERNARY VOLCANISM OF THE CARPATHIAN PANNONIAN REGION},
	url = {https://m2.mtmt.hu/api/publication/1855796},
	author = {Szabó, Csaba and Harangi, Szabolcs and Csontos, László},
	doi = {10.1016/0040-1951(92)90347-9},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {208},
	unique-id = {1855796},
	issn = {0040-1951},
	year = {1992},
	eissn = {1879-3266},
	pages = {243-256},
	orcid-numbers = {Szabó, Csaba/0000-0002-1580-6344; Harangi, Szabolcs/0000-0003-2372-4581}
}

@article{MTMT:1782871,
	title = {BIRTH, LIFE AND DEATH OF THE PANNONIAN LAKE},
	url = {https://m2.mtmt.hu/api/publication/1782871},
	author = {Kázmér, Miklós},
	doi = {10.1016/0031-0182(90)90111-J},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {79},
	unique-id = {1782871},
	issn = {0031-0182},
	year = {1990},
	eissn = {1872-616X},
	pages = {171-188},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:1135587,
	title = {Relationships between the orientation of drainage and geological structure in Hungary},
	url = {https://m2.mtmt.hu/api/publication/1135587},
	author = {Gábris, Gyula},
	journal-iso = {ELMÉLET MÓDSZER GYAKORLAT},
	journal = {ELMÉLET MÓDSZER GYAKORLAT},
	volume = {42},
	unique-id = {1135587},
	issn = {0139-2875},
	abstract = {In order to reveal the relationships between major structural elements and the drainage, statistics of directions were analyzed and the results are presented here. The peaks of the statistics of lineament directions are also maxima in the drainage and active to the immediate past; they are interpreted as neotectonic structures (not necessarily recent but possibly rejuvenated old elements) controlling the courses of streams. In contrast, the lineament peaks not manifested in the drainage may indicate ancient inactive structures. -from Author},
	year = {1987},
	pages = {183-194}
}

@article{MTMT:1834167,
	title = {Permian-Paleogene paleogeography along the eastern part of the Insubric-Periadriatic lineament system: Evidence for continental escape of the Bakony-Drauzug unit.},
	url = {https://m2.mtmt.hu/api/publication/1834167},
	author = {Kázmér, Miklós and KOVÁCS, Sándor},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {28},
	unique-id = {1834167},
	issn = {0236-5278},
	year = {1985},
	pages = {71-84},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}