TY  - JOUR
AU  - Sierralta, M
AU  - Kele, Sándor
AU  - Melcher, F
AU  - Hambach, U
AU  - Reinders, J
AU  - van Geldern, R
AU  - Frechen, M
TI  - Uranium-series dating of travertine from Sutto: Implications for reconstruction of environmental change in Hungary
JF  - QUATERNARY INTERNATIONAL
J2  - QUATERN INT
VL  - 222
PY  - 2010
IS  - 1-2
SP  - 178
EP  - 193
PG  - 16
SN  - 1040-6182
DO  - 10.1016/j.quaint.2009.04.004
UR  - https://m2.mtmt.hu/api/publication/1370895
ID  - 1370895
N1  - Megjegyzés-24852274
Megjegyzés-21064986
FU: Deutsche Forschungsgemeinschaft (DFG) [FR877/6-1, HA2193/7-1]
FX: This study was supported by the Deutsche Forschungsgemeinschaft (DFG,
: grant No. FR877/6-1 and HA2193/7-1). The paper benefited from the
: comments of two anonymous reviewers. Many thanks to Andrea Mindszenty
: for her helpful comments and remarks. We thank Sabine Mogwitz and
: Astrid Jaeckel for help with isotope analysis and Ulrich
: Schwarz-Schampera and Thomas Pletsch for their assistance with the
: cathodolummescence equipment. Particular thanks to Juliane Herrmann for
: her help in preparing the artwork for this article.
Megjegyzés-21064993
FU: Deutsche Forschungsgemeinschaft (DFG) [FR877/6-1, HA2193/7-1]
FX: This study was supported by the Deutsche Forschungsgemeinschaft (DFG,
: grant No. FR877/6-1 and HA2193/7-1). The paper benefited from the
: comments of two anonymous reviewers. Many thanks to Andrea Mindszenty
: for her helpful comments and remarks. We thank Sabine Mogwitz and
: Astrid Jaeckel for help with isotope analysis and Ulrich
: Schwarz-Schampera and Thomas Pletsch for their assistance with the
: cathodolummescence equipment. Particular thanks to Juliane Herrmann for
: her help in preparing the artwork for this article.
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Bada, G
AU  - Grenerczy, G
AU  - Tóth, László
AU  - Horváth, Ferenc
AU  - Stein, S
AU  - Cloetingh, S
AU  - Windhoffer, G
AU  - Fodor, László
AU  - Pinter, N
AU  - Fejes, I
TI  - Motion of Adria and ongoing inversion of the Pannonian Basin: Seismicity, GPS velocities, and stress transfer
JF  - SPECIAL PAPERS - GEOLOGICAL SOCIETY OF AMERICA
J2  - SPEC PAP - GEOL SOC AM
VL  - 425
PY  - 2007
SP  - 243
EP  - 262
PG  - 20
SN  - 0072-1077
DO  - 10.1130/2007.2425(16)
UR  - https://m2.mtmt.hu/api/publication/2176400
ID  - 2176400
N1  - Department of Geophysics, Eötvös L. University, Pdzmdny P. st. 1/C, 1117 Budapest, Hungary            
            Research Centre for Integrated Solid Earth Science (ISES), Vrije Universiteit, De Boelelaan 1085, 1081 HV, Amsterdam, Netherlands            
            FÒMI Satellite Geodetic Observatory, 2614 Pene, Hungary            
            Seismological Observatory, Hungarian Academy of Sciences, Meredek u. 18, 1112 Budapest, Hungary            
            Department of Geophysics, Eötvös L. University, Pázmány P. st. 1/C, 1117 Budapest, Hungary            
            Department of Earth and Planetary Sciences, Northwestern University, 1850 Campus Drive, Evanston, IL 60208, United States            
            Research Centre for Integrated Solid Earth Science (ISES), Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, Netherlands            
            Department of Geophysics, Eötvös L. University, Pázmdny P. st. 1/C, 1117 Budapest, Hungary            
            Geological Institute of Hungary, Stefdnia lit 14, 1143 Budapest, Hungary            
            Department of Geology, Southern IL University, Carbondale, IL 62901, United States            
            FÖMI Satellite Geodetic Observatory, 2614 Penc, Hungary            
            Cited By :30            
            Export Date: 12 December 2022            
            Correspondence Address: Bada, G.; Department of Geophysics, Pdzmdny P. st. 1/C, 1117 Budapest, Hungary; email: bada@ludens.elte.hu
AB  - 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.
LA  - English
DB  - MTMT
ER  - 

TY  - CHAP
AU  - Bada, G
AU  - Horváth, Ferenc
AU  - Tóth, László
AU  - Fodor, László
AU  - Timár, Gábor
AU  - Cloetingh, S
ED  - Pinter, N
ED  - Grenerczy, Gyula
ED  - Wéber, J
ED  - Stein, S
ED  - Medak, D
TI  - Societal aspects of ongoing deformation in the Pannonian region
T2  - The Adria Microplate: GPS Geodesy, Tectonics and Hazards
PB  - Springer Netherlands
CY  - Dordrecht
SN  - 1402042355
T3  - NATO Science Series, Series IV, ISSN 1568-1238 ; 61.
PY  - 2006
SP  - 385
EP  - 402
PG  - 18
DO  - 10.1007/1-4020-4235-3_26
UR  - https://m2.mtmt.hu/api/publication/1138114
ID  - 1138114
N1  - 
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Fodor, László
TI  - 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
JF  - GEOLINES
J2  - GEOLINES
VL  - 20
PY  - 2006
SP  - 34
EP  - 36
PG  - 3
SN  - 1210-9606
UR  - https://m2.mtmt.hu/api/publication/1369376
ID  - 1369376
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Karátson, Dávid
AU  - Timár, Gábor
TI  - Comparative volumetric calculations of two segments of the Carpathian Neogene/Quaternary volcanic chain using SRTM elevation data: implications for erosion and magma output rates
JF  - ZEITSCHRIFT FUR GEOMORPHOLOGIE SUPPLEMENTBAND
J2  - Z GEOMORPH SUPPL
VL  - 140
PY  - 2005
SP  - 19
EP  - 35
PG  - 18
SN  - 0044-2798
UR  - https://m2.mtmt.hu/api/publication/1138162
ID  - 1138162
N1  - WoS:hiba:000233987500002 2020-09-04 06:11 típus nem egyezik
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Jordán, Győző
AU  - Csillag, Gábor
AU  - Szűcs, Andrea
AU  - Qvarfort, U
TI  - Application of digital terrain modelling and GIS methods for the morphotectonic investigation of the Kali Basin, Hungary
JF  - ZEITSCHRIFT FÜR GEOMORPHOLOGIE
J2  - Z GEOMORPHOL
VL  - 47
PY  - 2003
IS  - 2
SP  - 145
EP  - 169
PG  - 25
SN  - 0372-8854
UR  - https://m2.mtmt.hu/api/publication/1329291
ID  - 1329291
AB  - 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.
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Németh, Károly
AU  - MARTIN, U
AU  - Csillag, Gábor
TI  - 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
JF  - GEOLINES
J2  - GEOLINES
VL  - 15
PY  - 2003
SP  - 102
EP  - 106
PG  - 5
SN  - 1210-9606
UR  - https://m2.mtmt.hu/api/publication/1385210
ID  - 1385210
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Ujhazy, K
AU  - Gábris, Gyula
AU  - Frechen, M
TI  - Ages of periods of sand movement in Hungary determined through luminescence measurements
JF  - QUATERNARY INTERNATIONAL
J2  - QUATERN INT
VL  - 111
PY  - 2003
IS  - 1
SP  - 91
EP  - 100
PG  - 10
SN  - 1040-6182
DO  - 10.1016/S1040-6182(03)00017-X
UR  - https://m2.mtmt.hu/api/publication/1135541
ID  - 1135541
AB  - 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.
LA  - English
DB  - MTMT
ER  - 

TY  - THES
AU  - Burján, Balázs
TI  - A Pesti-síkság fiatal-harmadidőszaki és negyedidőszaki kavicsképződményeinek összehasonlító vizsgálata
PB  - Szegedi Tudományegyetem (SZTE)
PY  - 2002
SP  - 133
UR  - https://m2.mtmt.hu/api/publication/30721230
ID  - 30721230
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Csillag, Gábor
AU  - Fodor, László
AU  - Peregi, Zs
AU  - Roth, L
AU  - Selmeczi, Ildikó
TI  - Pliocene-Quaternary landscape evolution and deformation in the eastern Vértes Hills, (Hungary): the heritage and reactivation of Miocene fault pattern
JF  - GEOLOGICA CARPATHICA
J2  - GEOL CARPATH
VL  - 53
PY  - 2002
IS  - Special Issue
SP  - 206
EP  - 208
PG  - 3
SN  - 1335-0552
UR  - https://m2.mtmt.hu/api/publication/1368976
ID  - 1368976
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Tóth, László
AU  - Mónus, Péter
AU  - Zsíros, Tibor
AU  - Marótiné Kiszely, Márta
TI  - Seismicity in the Pannonian Region - earthquake data
JF  - EGU STEPHAN MUELLER SPECIAL PUBLICATION SERIES
J2  - EGU STEPHAN MUELLER SPEC PUBL SER
VL  - 3
PY  - 2002
SP  - 9
EP  - 28
PG  - 20
SN  - 1868-4556
UR  - https://m2.mtmt.hu/api/publication/1419807
ID  - 1419807
N1  - ISSN: 1868-4556
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - ZÁMBÓ, L
AU  - FORD, D
AU  - Telbisz, Tamás Ferenc
TI  - Baradla-barlangi cseppkőkoradatok a késő-negyedidőszaki klímaingadozások tükrében
JF  - FÖLDTANI KÖZLÖNY
J2  - FÖLDTANI KÖZLÖNY
VL  - 132
PY  - 2002
IS  - különszám
SP  - 231
EP  - 238
PG  - 8
SN  - 0015-542X
UR  - https://m2.mtmt.hu/api/publication/1353324
ID  - 1353324
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - THES
AU  - Gábris, Gyula
TI  - A folyóvíz felszínalakító tevékenysége Magyarországon
PY  - 2001
SP  - 131
UR  - https://m2.mtmt.hu/api/publication/1140531
ID  - 1140531
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Karátson, Dávid
TI  - Vulkáni törmeléklavinák: általános jellemzők, ismert példák, magyarországi előfordulások
JF  - FÖLDTANI KÖZLÖNY
J2  - FÖLDTANI KÖZLÖNY
VL  - 131
PY  - 2001
IS  - 1-2
SP  - 253
EP  - 283
PG  - 31
SN  - 0015-542X
UR  - https://m2.mtmt.hu/api/publication/2321065
ID  - 2321065
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Telbisz, Tamás Ferenc
TI  - Új megközelítések a töbör-morfológiában az Aggteleki-karszt példáján
JF  - FÖLDRAJZI KÖZLEMÉNYEK
J2  - FÖLDRAJZI KÖZLEMÉNYEK
VL  - 125
PY  - 2001
IS  - 1-2
SP  - 95
EP  - 108
PG  - 14
SN  - 0015-5411
UR  - https://m2.mtmt.hu/api/publication/1353326
ID  - 1353326
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - CHAP
AU  - Fodor, László
AU  - Csontos, L
AU  - Bada, G
AU  - Györfi, I
AU  - Benkovics, L
ED  - Durand, B
ED  - Jolivet, L
ED  - Horváth, Ferenc
ED  - Seranne, M
TI  - Tertiary tectonic evolution of the Pannonian Basin system and neighbouring orogens: a new synthesis of palaeostress data
T2  - The Mediterranean Basins: tertiary extension within the Alpine Orogen
PB  - Geological Society of London
CY  - London
SN  - 9781862390331
T3  - Geological Society Special Publication, ISSN 0305-8719 ; 156.
PY  - 1999
SP  - 295
EP  - 334
PG  - 40
DO  - 10.1144/GSL.SP.1999.156.01.15
UR  - https://m2.mtmt.hu/api/publication/1369059
ID  - 1369059
N1  - Dept. of Appl. and Environ. Geology, Eötvös University, 1088 Múzeum krt 4/a, Budapest, Hungary            
            Dept. of Gen. and Historical Geology, Eötvös University, 1088 Múzeum krt 4/a, Budapest, Hungary            
            Department of Geophysics, Eötvös University, 1085 Ludovika tér 2, Budapest, Hungary            
            Department of Engineering Geology, Technical University of Budapest, Stoczek u. 2, Budapest, Hungary            
            Cited By :375            
            Export Date: 10 May 2023            
            Correspondence Address: Fodor, L.; Dept. of App. + Envtml. Geol., Muzeum krt 4/a, Budapest 1088, Hungary
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Karátson, Dávid
AU  - Németh, Károly
AU  - Józsa, Sándor
AU  - BORBÉLY, E
TI  - AN ANCIENT DEBRIS AVALANCHE INITIATED THE RIVER LOOP? THE MYSTERY OF THE DANUBE BEND, HUNGARY
T2  - EUROPEAN UNION OF GEOSCIENCES CONFERENCE
C1  - Strasbourg
PY  - 1999
SP  - 320
EP  - 320
PG  - 1
UR  - https://m2.mtmt.hu/api/publication/1384939
ID  - 1384939
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Magyar, Imre
AU  - Geary, DH
AU  - Muller, P
TI  - Paleogeographic evolution of the Late Miocene Lake Pannon in Central Europe
JF  - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
J2  - PALAEOGEOGR PALAEOCL
VL  - 147
PY  - 1999
IS  - 3-4
SP  - 151
EP  - 167
PG  - 17
SN  - 0031-0182
DO  - 10.1016/S0031-0182(98)00155-2
UR  - https://m2.mtmt.hu/api/publication/1890263
ID  - 1890263
N1  - Cited By :351            
            Export Date: 24 February 2023            
            CODEN: PPPYA            
            Correspondence Address: Geary, D.H.; Department of Geology and Geophysics, 1215 West Dayton Street, Madison, WI 53706, United States; email: dana@geology.wisc.edu
AB  - 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.
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Németh, Károly
AU  - Martin, U
TI  - Large hydrovolcanic field in the Pannonian Basin: general characteristics of the Bakony-Balaton Highland Volcanic Field, Hungary
JF  - ACTA VULCANOLOGICA
J2  - ACTA VULCANOL
VL  - 11
PY  - 1999
IS  - 2
SP  - 271
EP  - 282
PG  - 12
SN  - 1121-9114
UR  - https://m2.mtmt.hu/api/publication/1384635
ID  - 1384635
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Frechen, M
AU  - Horváth, Erzsébet
AU  - Gábris, Gyula
TI  - Geochronology of Middle and Upper Pleistocene Loess sections in Hungary
JF  - QUATERNARY RESEARCH
J2  - QUATERNARY RES
VL  - 48
PY  - 1997
IS  - 3
SP  - 291
EP  - 312
PG  - 22
SN  - 0033-5894
DO  - 10.1006/qres.1997.1929
UR  - https://m2.mtmt.hu/api/publication/1135539
ID  - 1135539
AB  - 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.
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Gábris, Gyula
TI  - Gondolatok a folyóteraszokról
JF  - FÖLDRAJZI KÖZLEMÉNYEK
J2  - FÖLDRAJZI KÖZLEMÉNYEK
VL  - 121 (45)
PY  - 1997
IS  - 1
SP  - 3
EP  - 16
PG  - 14
SN  - 0015-5411
UR  - https://m2.mtmt.hu/api/publication/1140415
ID  - 1140415
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Mari, László
TI  - Geomorfológiai megfigyelések a Szentendrei-szigeten
JF  - FÖLDRAJZI KÖZLEMÉNYEK
J2  - FÖLDRAJZI KÖZLEMÉNYEK
VL  - CXX.
PY  - 1997
IS  - 4
SP  - 217
EP  - 233
PG  - 17
SN  - 0015-5411
UR  - https://m2.mtmt.hu/api/publication/1724097
ID  - 1724097
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Karátson, Dávid
TI  - Rates and factors of stratovolcano degradation in a continental climate: a complex morphometric analysis of nineteen Neogene/Quaternary crater remnants in the Carpathians
JF  - JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH
J2  - J VOLCANOL GEOTH RES
VL  - 73
PY  - 1996
IS  - 1-2
SP  - 65
EP  - 78
PG  - 14
SN  - 0377-0273
DO  - 10.1016/0377-0273(96)00016-9
UR  - https://m2.mtmt.hu/api/publication/1738851
ID  - 1738851
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Gábris, Gyula
TI  - Pleistocene evolution of the Danube in the Carpathian Basin
JF  - TERRA NOVA
J2  - TERRA NOVA
VL  - 6
PY  - 1994
IS  - 5
SP  - 495
EP  - 501
PG  - 7
SN  - 0954-4879
DO  - 10.1111/j.1365-3121.1994.tb00893.x
UR  - https://m2.mtmt.hu/api/publication/1135538
ID  - 1135538
AB  - 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.
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Gábris, Gyula
AU  - Papp, S
AU  - Mari, László
AU  - Santa, A
TI  - A physical geographical sketch of the Hungarian Ipoly Valley
JF  - ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLANDO EÖTVÖS NOMINATAE - SECTIO GEOGRAPHICA
J2  - ANN UNIV SCI BP R EÖTVÖS NOM SECT GEOGR
VL  - 22-23
PY  - 1993
SP  - 57
EP  - 66
PG  - 10
SN  - 0524-8965
UR  - https://m2.mtmt.hu/api/publication/1135590
ID  - 1135590
AB  - 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
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Müller, P
AU  - Magyar, Imre
TI  - 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)
TS  - Stratigraphic significance of the Upper Miocene lacustrine Cardiid Prosodacnomya (Kötcse section, Pannonian basin, Hungary)
JF  - FÖLDTANI KÖZLÖNY
J2  - FÖLDTANI KÖZLÖNY
VL  - 122
PY  - 1992
SP  - 1
EP  - 38
PG  - 38
SN  - 0015-542X
UR  - https://m2.mtmt.hu/api/publication/1892924
ID  - 1892924
N1  - Megjegyzés-27443670
31. o
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Szabó, Csaba
AU  - Harangi, Szabolcs
AU  - Csontos, László
TI  - REVIEW OF NEOGENE AND QUATERNARY VOLCANISM OF THE CARPATHIAN PANNONIAN REGION
JF  - TECTONOPHYSICS
J2  - TECTONOPHYSICS
VL  - 208
PY  - 1992
IS  - 1-3
SP  - 243
EP  - 256
PG  - 14
SN  - 0040-1951
DO  - 10.1016/0040-1951(92)90347-9
UR  - https://m2.mtmt.hu/api/publication/1855796
ID  - 1855796
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Kázmér, Miklós
TI  - BIRTH, LIFE AND DEATH OF THE PANNONIAN LAKE
JF  - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
J2  - PALAEOGEOGR PALAEOCL
VL  - 79
PY  - 1990
IS  - 1-2
SP  - 171
EP  - 188
PG  - 18
SN  - 0031-0182
DO  - 10.1016/0031-0182(90)90111-J
UR  - https://m2.mtmt.hu/api/publication/1782871
ID  - 1782871
N1  - Cited By :74            
            Export Date: 24 February 2023            
            CODEN: PPPYA            
            Correspondence Address: Kázmér, M.; Department of Palaeontology, Eötvös University, Kun Béla tér 2, H-1083 Budapest, Hungary
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Gábris, Gyula
TI  - Relationships between the orientation of drainage and geological structure in Hungary
JF  - ELMÉLET MÓDSZER GYAKORLAT
J2  - ELMÉLET MÓDSZER GYAKORLAT
VL  - 42
PY  - 1987
SP  - 183
EP  - 194
PG  - 12
SN  - 0139-2875
UR  - https://m2.mtmt.hu/api/publication/1135587
ID  - 1135587
AB  - 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
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Kázmér, Miklós
AU  - KOVÁCS, Sándor
TI  - Permian-Paleogene paleogeography along the eastern part of the Insubric-Periadriatic lineament system: Evidence for continental escape of the Bakony-Drauzug unit.
JF  - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES
J2  - ACTA GEOL HUNG
VL  - 28
PY  - 1985
IS  - 1-2
SP  - 71
EP  - 84
PG  - 14
SN  - 0236-5278
UR  - https://m2.mtmt.hu/api/publication/1834167
ID  - 1834167
LA  - English
DB  - MTMT
ER  -