TY - JOUR AU - Császár, Géza AU - Görög, Ágnes AU - Gyuricza, György AU - SIEGLNÉ-FARKAS, Á AU - Szente, István AU - Szinger, Balázs TI - A Vasasi Márga földtani, őslénytani és üledékföldtani jellegei a Zsibrik és Ófalu közötti területen JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 137 PY - 2007 IS - 2 SP - 193 EP - 226 PG - 34 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1319899 ID - 1319899 LA - Hungarian DB - MTMT ER - TY - GEN AU - Görög, Ágnes TI - Foraminiferavizsgálatok a mecseki Zsibrik és Ófalu környéki liász képződményekből (in Hungarian, translated title: Foraminifera studies from the Liassic rocks in vicinity of Zsibrik and Ófalu)... in: GYALOG L., BALLA Z., CSÁSZÁR G., GULÁCSI Z., KAISER M., KOLOSZÁR L., KOROKNAI B., LANTOS Z., MAGYARI Á., MAROS GY., MARSI I., PEREGI Zs. 2006c: Földtani és geomorfológiai térképezés jelentése [Üveghuta] (in Hungarian, translated title: Report on geological and geomorphological mapping [Üveghuta]). — Kézirat (manuscript), Magyar Állami Földtani Intézet, Tekt. 1339. TS - in: GYALOG L., BALLA Z., CSÁSZÁR G., GULÁCSI Z., KAISER M., KOLOSZÁR L., KOROKNAI B., LANTOS Z., MAGYARI Á., MAROS GY., MARSI I., PEREGI Zs. 2006c: Földtani és geomorfológiai térképezés jelentése [Üveghuta] (in Hungarian, translated title: Report on geological and geomorphological mapping [Üveghuta]). — Kézirat (manuscript), Magyar Állami Földtani Intézet, Tekt. 1339. PY - 2006 SP - 33 EP - 42 PG - 10 UR - https://m2.mtmt.hu/api/publication/3346294 ID - 3346294 LA - Hungarian DB - MTMT ER - TY - GEN AU - Cziczer, István AU - Magyar, I AU - Müller, P TI - A Mórágyi-rög területén gyűjtött pannóniai puhatestű fauna értékelése PY - 2005 UR - https://m2.mtmt.hu/api/publication/1935454 ID - 1935454 N1 - [Kézirat] LA - Hungarian DB - MTMT ER - TY - GEN AU - CSÁSZÁR, G AU - Görög, Ágnes AU - Gyuricza, György AU - SZENTE, I AU - SZINGER, B TI - Jelentés a Zsibrik és Ófalu közötti terület jura képződményeinek földtani térképezéséről és anyagvizsgálatáról (in Hungarian, translated title: Report of the geological mapping and laboratory analysis of the Jurassic rocks of the region between Zsibrik and Ófalu). — Kézirat (manuscript), Magyar Állami Földtani Intézet, Budapest, PY - 2005 UR - https://m2.mtmt.hu/api/publication/3346299 ID - 3346299 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Buda, György AU - Dobosi, Gábor TI - Lamprophyre-derived high-K mafic enclaves in Variscan granitoids from the Mecsek Mts. (South Hungary) JF - NEUES JAHRBUCH FUR MINERALOGIE-ABHANDLUNGEN J2 - NEUES JB MINER ABH VL - 180 PY - 2004 IS - 2 SP - 115 EP - 147 PG - 33 SN - 0077-7757 DO - 10.1127/0077-7757/2004/0180-0115 UR - https://m2.mtmt.hu/api/publication/1124699 ID - 1124699 N1 - Cited By :12 Export Date: 24 January 2023 Correspondence Address: Buda, G.; Eötvös Loránd Univ., Pázmány P. str. 1/C, Budapest H-1117, Hungary; email: buda@ludens.elte.hu AB - Variscan magnesio-potassic microcline megacryst-bearing quartz monzonite and monzogranite contain several chromite-bearing high potassic mafic enclaves of various sizes in Moragy Hills (South Hungary). These enclaves are biotite amphibol melamonzonite, amphibole biotite melasyenite and rarely amphibole meladiorite according to the classification of igneous rocks of the IUGS Subcommission on the Systematics of Igneous Rocks. The mineralogical, petrological and geochemical compositions of these basic enclaves correspond with lamprophyre-derived locally named vaugnerite/durbachite, which are widespread in the Variscan collision belt. The host plutonic rocks enriched in K and Mg due to the interaction of basic and acid magmas. The basic melt originated from the upper mantle revealed by the presence of chromite. The upper mantle was enriched in compatible and incompatible elements probable as a consequence of an older subduction. Acidic melt formed by the partial melting of the continental crust. Both melts crystallized simultaneously and affected each other. Mafic enclaves became more lamprophyric and the acidic one enriched in K and Mg, They formed probably in a postcollisional uplifted tectonic regime due to extension after compression. LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Budai, Tamás AU - Hips, Kinga AU - Konrád, Gyula AU - Török, Ákos TI - Magyarországi triász fáciesterületek szekvencia-rétegtani elemzése JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 132 PY - 2002 IS - 1 SP - 17 EP - 43 PG - 27 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1025644 ID - 1025644 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Lelkes, Felvári GY AU - Árkai, Péter AU - Frank, W AU - Nagy, Géza TI - Late Variscan ultramylonite from the Mórágy Hills, SE Mecsek Mts., Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 43 PY - 2000 IS - 1 SP - 65 EP - 84 PG - 20 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1098542 ID - 1098542 N1 - Megjegyzés-22002031 : 40Ar/ : 39Ar analyses LA - English 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 - JOUR AU - Lennert, J AU - Szónoky, M AU - Gulyás, Sándor AU - Shatilova, I I AU - Geary, D H AU - Magyar, Imre AU - Szuromi-Korecz, A AU - Süto-Szentai, M TI - The Lake Pannon fossils of the Bataszek brickyard JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 42 PY - 1999 IS - 1 SP - 67 EP - 88 PG - 22 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1890286 ID - 1890286 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) AB - The outcrop of the Bataszek brickyard in southeastern Transdanubia of Hungary exposes clayey silt in a 20 to 30 m thickness, containing several thin, sandy, often limonitic, poorly sorted coquina layers. We interpret the silt as sublittoral deposit of the Late Miocene Lake Pannon. The sandy intercalations are probably storm deposits or sediment gravity flows from a nearby littoral environment. The mollusk fauna of the silt is largely autochthonous, and dominated by Congeria rhomboidea and Lymnocardium hungaricum. The partly reworked faunas of the sandy intercalations have a different composition. The entire fauna is very similar to the classic faunas of Okrugljak and Szekszard, and to the fauna of Jazovnik (faciostratotype of the Portaferrian Substage). All of these deposits belong to the Congeria rhomboidea Zone. Other fossils from the outcrop include ostracods, fishes, algae, spores, and pollen. The dinoflagellates indicate that the Bataszek deposits are in a slightly higher stratigraphic position than the top of the Spiniferites validus Zone. LA - English DB - MTMT ER - TY - JOUR AU - Magyar, Imre AU - Geary, D H AU - Süto-Szentai, M AU - Lantos, M AU - Müller, P TI - Integrated biostratigraphic, magnetostratigraphic and chronostratigraphic correlations of the Late Miocene Lake Pannon deposits JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 42 PY - 1999 IS - 1 SP - 5 EP - 31 PG - 27 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1890285 ID - 1890285 N1 - Department of Geology and Geophysics, University of Wisconsin, Madison, WI, United States Geological Institute of Hungary, Budapest, Hungary Natural Historical Collection, Komló, Hungary 1215 W. Dayton Street, Madison, WI 53706, United States Városház tér 1, H-7300 Komló, Hungary Stefánia út 14, H-1143 Budapest, Hungary Cited By :94 Export Date: 24 February 2023 Correspondence Address: Magyar, I.; Department of Geology and Geophysics, 1215 W. Dayton Street, Madison, WI 53706, United States AB - Due to the highly endemic nature of the Late Miocene Lake Pannon's aquatic biota, the stratigraphic correlation of the lake's sediments with the global chronostratigraphic system is dependent upon mammal biostratigraphy, magnetostratigraphy, and radio-isotopic age determinations. However, correlation of mammal localities and isotopically dated volcanic formations with the lacustrine sequence is possible only in a few instances, offering limited independent data for magnetostratigraphic interpretation. In this paper we construct a correlation chart that integrates biostratigraphy (dinoflagellates and mollusks) with the results of physical dating methods. The average time resolution of our biozones (excluding deep-water mollusk zones) is 1 Ma. There is a difference, however, in the amount of available data and consequently in the reliability of our correlations between the lower (older than approximately 9.5 Ma) and upper parts of the sedimentary sequence; the former is well-established, whereas a scarcity of radio-isotopic ages from the upper part of the sequence results in more uncertainty. In addition, a biostratigraphic subdivision of the last ca. 3 Ma interval of the lacustrine sequence is almost entirely lacking. The only opportunity for interbasinal biostratigraphic correlation within the lifetime of Lake Pannon is the Early Pontian migration event, when a great number of the Lake Pannon endemic species entered the Eastern Paratethys. However, due to the scarcity of chronological data from the Late Miocene of the respective basins, correlation of the Eastern Paratethyan Pontian Stage to the Lake Pannon deposits carriers at least a 1.3 Ma uncertainty. 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 - Pouclet, A AU - Horváth, Erzsébet AU - Gábris, Gyula AU - Juvigne, E TI - The Bag Tephra, a widespread tephrochronological marker in Middle Europe: chemical and mineralogical investigations JF - BULLETIN OF VOLCANOLOGY J2 - B VOLCANOL VL - 61 PY - 1999 IS - 4 SP - 265 EP - 272 PG - 8 SN - 0258-8900 DO - 10.1007/s004450050275 UR - https://m2.mtmt.hu/api/publication/1135540 ID - 1135540 AB - The Bag Tephra is a widespread tephra layer interbedded in Quaternary loess deposits along the Danubian valley of Hungary and Slovakia. Its age is poorly defined between 788 and 380 ka B.P. The glass and mineral composition - micropumice clasts of phono-tephrite and blocky shards of tephri-phonolite associated with two kinds of clinopyroxene, fassaitic diopside, and salite - is very distinctive. This tephra could be used as a chronological marker, as soon as its age is refined. The probable origin is the middle Italian volcanic area. LA - English DB - MTMT ER - TY - JOUR AU - Konrád, Gyula TI - Synsedimentary tectonic events in the Middle Triassic evolution of the SE Transdanubian part of the Tisza Unit JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 41 PY - 1998 IS - 3 SP - 327 EP - 341 PG - 15 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1324065 ID - 1324065 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 - THES AU - Görög, Ágnes TI - Magyarországi kréta Orbitolina-félék vizsgálata sztratigráfiai és ökológiai értékelése PY - 1996 UR - https://m2.mtmt.hu/api/publication/1320657 ID - 1320657 N1 - ELTE Őslénytani Tanszék Könyvtár LA - Hungarian DB - MTMT ER - TY - JOUR AU - Buda, György AU - Nagy, Géza TI - Some REE-bearing accessory minerals in two types of Variscan granitoids, Hungary JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 46 PY - 1995 IS - 2 SP - 67 EP - 78 PG - 12 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/1370639 ID - 1370639 LA - English DB - MTMT ER - TY - JOUR AU - Árkai, Péter AU - Nagy, Géza TI - Tectonic and magmatic effects on amphibole chemistry in mylonitized amphibolites and amphibole-bearing enclaves associated with granitoid rocks, Mecsek Mountains, Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 37 PY - 1994 IS - 3-4 SP - 235 EP - 268 PG - 1 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1098518 ID - 1098518 LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Erzsébet AU - Gábris, Gyula AU - Juvigné, E TI - Egy pleisztocén vezérszint a Kárpát medencében: a Bag Tefra JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 122 PY - 1992 IS - 3-4 SP - 233 EP - 249 PG - 17 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1140425 ID - 1140425 N1 - A marker in the Pleistocene of the Carpathian-Basin: the Bag Tephra AB - Several aspects of a tephra layer present in seven loess sections in Hungary and in Czechoslovakia were investigated: grain-size, mafic mineral suites, and chemical composition of bulk samples as well as clinopyroxenes. The tephra is identical in all localities, and the name "Bag Tephra" was given to it. This tephra allows us to propose a new stratigraphical correlation of the investigated loess sections. The tephra-fall occured during or befor the last 5th glaciation. Since the closest pleistocene volcanic fields are situated very far from the investigated localities (more than 500 km), the Bag Tephra can be used as a widespread stratigraphical marker in Central Europe. The currently avaliable data show that the relevant volcano should be located in the East Eifel volcanic field (Germany). 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 - Müller, P AU - Magyar, Imre TI - Continuous record of the evolution of lacustrine cardiid bivalves in the late Miocene Pannonian Lake JF - ACTA PALAEONTOLOGICA POLONICA J2 - ACTA PALAEONTOL POL VL - 36 PY - 1992 SP - 353 EP - 372 PG - 20 SN - 0567-7920 UR - https://m2.mtmt.hu/api/publication/1892935 ID - 1892935 LA - English DB - MTMT ER - TY - JOUR AU - Csontos, László AU - Tari, Gábor AU - Bergerat, F AU - Fodor, László TI - Evolution of the stress fields in the Carpatho-Pannonian area during the Neogene JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 199 PY - 1991 IS - 1 SP - 73 EP - 91 PG - 19 SN - 0040-1951 DO - 10.1016/0040-1951(91)90119-D UR - https://m2.mtmt.hu/api/publication/1368441 ID - 1368441 LA - English DB - MTMT ER -