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MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/c, Budapest, 1117, Hungary
Geological and Geophysical Institute of Hungary, Stefánia út 14, Budapest, 1143, Hungary
Noble Research Center, Boone Pickens School of Geology, Oklahoma State University, Stillwater, OK 74078, United States
Research Centre for Astronomy and Earth Sciences, Institute for Geological and Geochemical Research, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, 1112, Hungary
ConocoPhillips Company, 600 N Dairy Ashford, Houston, TX 77079, United States
Cited By :13
Export Date: 26 August 2022
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Correspondence Address: Haas, J.; MTA-ELTE Geological, Pázmány P. sétány 1/c, Hungary; email: haas@caesar.elte.hu
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10000315"> <a href="/gui2/?type=authors&mode=browse&sel=10000315" target="_blank">Haas, J ✉</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10009332"> <a href="/gui2/?type=authors&mode=browse&sel=10009332" target="_blank">Hips, K</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10010453"> <a href="/gui2/?type=authors&mode=browse&sel=10010453" target="_blank">Budai, T</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10029206"> <a href="/gui2/?type=authors&mode=browse&sel=10029206" target="_blank">Győri, O</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10021722"> <a href="/gui2/?type=authors&mode=browse&sel=10021722" target="_blank">Lukoczki, G</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10014662"> <a href="/gui2/?type=authors&mode=browse&sel=10014662" target="_blank">Kele, S</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10000314"> <a href="/gui2/?type=authors&mode=browse&sel=10000314" target="_blank">Demény, A</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10027218"> <a href="/gui2/?type=authors&mode=browse&sel=10027218" target="_blank">Poros, Z</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;3091740" mtid="3091740" target="_blank">Processes and controlling factors of polygenetic dolomite formation in the Transdanubian Range, Hungary: a synopsis</a></div> <div class="pub-info"> <span class="journal-title">INTERNATIONAL JOURNAL OF EARTH SCIENCES</span> <span class="journal-volume">106</span> : <span class="journal-issue">3</span> <span class="page"> pp. 991-1021. , 31 p. </span> <span class="year">(2017)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1007/s00531-016-1347-7" target="_blank" href="https://doi.org/10.1007/s00531-016-1347-7"> DOI </a> </span> <span class="id identifier oa_RESTRICTED" title=" Korlátozott "> <a style="color:blue" title="39221" target="_blank" href="http://real.mtak.hu/39221"> REAL </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000398931600011" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000398931600011"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="84975126603" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-84975126603"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:3091740 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 24</span> | Független: 16 | Függő: 8 | Nem jelölt: 0 | WoS jelölt: 16 | Scopus jelölt: 18 | WoS/Scopus jelölt: 20 | DOI jelölt: 18 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;3091740" target="_blank">Processes and controlling factors of polygenetic dolomite formation in the Transdanubian Range, Hungary: a synopsis</a></div> <div> <span class="journal-title">INTERNATIONAL JOURNAL OF EARTH SCIENCES</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/1437-3254">1437-3254</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1437-3262">1437-3262</a>)</span>:
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<div class="lastModified">Utolsó módosítás: 2020.08.25. 12:11 Temesvári Katalin (GKEM admin)
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/c, Budapest, 1117, Hungary
Geological and Geophysical Institute of Hungary, Stefánia út 14, Budapest, 1143, Hungary
Noble Research Center, Boone Pickens School of Geology, Oklahoma State University, Stillwater, OK 74078, United States
Res...</pre>
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Funding text: The study was supported by the Hungarian Scientific Research Found No. 42799 and Austrian-Hungarian Action Foundation No 68ou7. Part of the stratigraphical column was drawn by Z. Lantos (Budapest), and O. Sztano (Budapest) contributed to sedimentological interpretation. Finally, we thank an anonymous reviewer, C. Persano, F. Horvath, and the associate editor Meinert Rahn for detailed and constructive reviews.
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Funding Agency and Grant Number: Hungarian Scientific Research Found [42799]; Austrian-Hungarian Action Foundation [68ou7]
Funding text: The study was supported by the Hungarian Scientific Research Found No. 42799 and Austrian-Hungarian Action Foundation No 68ou7. Part of the stratigraphical column was drawn by Z. Lantos (Budapest), and O. Sztano (Budapest) contributed to sedimentol...</pre>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited By :48
Export Date: 26 August 2022
CODEN: PPPYA
Correspondence Address: Raucsik, B.; Department of Geology, Ifjúság útja 6, H-7624 Pécs, Hungary; email: raucsik.bela@gmail.com</pre>
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;152141" target="_blank">Facies and diagenetic evaluation of the Permian-Triassic boundary interval and basal Triassic carbonates: shallow and deep ramp sections, Hungary.</a></div> <div> <span class="journal-title">FACIES</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited By :17
Export Date: 27 January 2023
Correspondence Address: Hips, K.; Geological, Geophysical and Space Science Research Group, Pázmány s. 1/c, 1117 Budapest, Hungary; email: hips@ludens.elte.hu</pre>
</div></div>
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CODEN: PPPYA
Correspondence Address: Csontos, L.; Geological Department, Pazmany P: setany 1/a, Budapest 1117, Hungary; email: csontos@ludens.elte.hu
Funding details: Hungarian Science Foundation, T 037595, T 043760
Funding text 1: The authors are indebted to many colleagues for the discussions of earlier oral and written versions of the manuscript. We would like to thank especially F. Horváth, A. Galácz, S. Kovács, M. Kázmér, E. Márton (Budapest), D. Plašienka, M. Kováč (Bratislava), F. Neubauer and Č. Tomek (Salzburg), K. Birkenmajer (Kraków), M. Săndulescu (Bucharest) S. Schmid (Basel) and P. Ziegler (Basel). We express our thanks to W. Frisch, F. Horváth, G. Stampfli, Alonso-Gutierrez, J. Von Raumer, B. Murphy, A. Collins and D. Nance who kindly revised and improved earlier versions of the manuscript. This version was helped by critical remarks of K. Birkenmajer, F. Neubauer, B. Sperner, G. Stampfli, and F. Surlyk. IGCP project 453 is gratefully thanked for moral and material support. Hungarian Science Foundation OTKA projects T 043760, T 037595 are also thanked for support.
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Palaeomagnetic, palaeobiogeographic and structural comparisons of
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terranes. These terranes are composed of different Mesozoic continental
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continuation in the Serbo-Macedonian Massif of the Balkans.
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Carpathians and filled the present Carpathian embayment in the Late
Palaeozoic-Early Mesozoic. The Vardar ocean occupied an intermediate
position between the Western Carpathian-Austroalpine-Transdanubian-High
Karst margin and the Bihor-Getic-Serbo-Macedonian microcontinent. The
Vardar and Pindos oceans were opened in the heart of the
Mediterranean-Adriatic microcontinent in the Late Permian-Middle
Triassic. Vardar subducted by the end of Jurassic, causing the
Bihor-Getic-Serbo-Macedonian microcontinent to collide with the
internal Dinaric-Western Carpathian margin.
An external Penninic-Vahic ocean tract began opening in the Early
Jurassic, separating the Austroalpine-Western Carpathian microcontinent
(and its fauna) from the European shelf. Further east, the
Severin-Ceahlau-Magura also began opening in the Early Jurassic, but
final separation of the Bihor-Getic ribbon (and its fauna) from the
European shelf did not take place until the late Middle Jurassic.
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Albian-Maastrichtian. The two oroclinal bends were finally opposed and
pushed into the gates of the Carpathian embayment during the Palaeogene
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Csontos, L </span> <span class="author-type"> </span> ; <span class="author-name" mtid="1329006"> <a href="/gui2/?type=authors&mode=browse&sel=1329006" target="_blank">Voros, A</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;1236932" mtid="1236932" target="_blank">Mesozoic plate tectonic reconstruction of the carpathian region</a></div> <div class="pub-info"> <span class="journal-title">PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY</span> <span class="journal-volume">210</span> : <span class="journal-issue">1</span> <span class="page"> pp. 1-56. , 56 p. </span> <span class="year">(2004)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.palaeo.2004.02.033" target="_blank" href="https://doi.org/10.1016/j.palaeo.2004.02.033"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000222857100001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000222857100001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="3042785180" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-3042785180"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:1236932 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Összefoglaló cikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 548</span> | Független: 532 | Függő: 16 | Nem jelölt: 0 | WoS jelölt: 474 | Scopus jelölt: 526 | WoS/Scopus jelölt: 547 | DOI jelölt: 506 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;1236932" target="_blank">Mesozoic plate tectonic reconstruction of the carpathian region</a></div> <div> <span class="journal-title">PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited By :483
Export Date: 11 November 2022
CODEN: PPPYA
Correspondence Address: Csontos, L.; Geological Department, Pazmany P: setany 1/a, Budapest 1117, Hungary; email: csontos@ludens.elte.hu
Funding details: Hungarian Science Foundation, T 037595, T 043760
Funding text 1: T...</pre>
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Triassic sequence stratigraphy of the Transdanubian Range (Hungary)
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On the basis of surface exposures and core sections, a comprehensive sequence analysis of the Triassic series was carried out in the Transdanubian Range. For recognition of the sequences as well as their boundaries, the regional subaerial exposure horizons, the maximum flooding intervals, the transgressive-regressive trends, the platform progradations and backsteppings, as well as signals of the higher order accommodation changes were primarily considered. Detailed analyses were accomplished in six selected sub-regions. On the basis of the results of these analyses, a composite sequence chart was compiled. The Triassic history of the Transdanubian Range can be subdivided into four stages. Within the first stage (Induan to Middle Anisian) which can be characterized by a ramp setting, five sequences have been recognized. The second stage (Middle Anisian-Ladinian) is mainly controlled by the Neotethys rifting and can be subdivided into three sequences. Infilling of the previously formed basins took place during the third stage (Carnian), consisting of three sequences. The fourth stage (latest Carnian to Rhaetian) reflects the passive margin evolution of the Neotethys. However, a new rifting (Ligurian-Penninic) began in the Late Norian and also influenced the evolution of the Transdanubian Range. Four sequences were recognized in this final evolutionary stage. About 50 % of the recognized sequence boundaries could be correlated with those reported from the Southern and Northern Alps, from the German Basin, and from Western Canada.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10000315"> <a href="/gui2/?type=authors&mode=browse&sel=10000315" target="_blank">Haas, J</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10010453"> <a href="/gui2/?type=authors&mode=browse&sel=10010453" target="_blank">Budai, T</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;1019032" mtid="1019032" target="_blank">Triassic sequence stratigraphy of the Transdanubian Range (Hungary)</a></div> <div class="pub-info"> <span class="journal-title">GEOLOGICA CARPATHICA</span> <span class="journal-volume">50</span> : <span class="journal-issue">6</span> <span class="page"> pp. 459-475. , 17 p. </span> <span class="year">(1999)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000084550900004" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000084550900004"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="0033508606" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-0033508606"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:1019032 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 69</span> | Független: 47 | Függő: 22 | Nem jelölt: 0 | WoS jelölt: 35 | Scopus jelölt: 51 | WoS/Scopus jelölt: 52 | DOI jelölt: 47 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<span class="author-affil"><span title="Eötvös Loránd Tudományegyetem">ELTE</span>/<span title="Természettudományi Kar">TTK</span>/<span title="Földrajz- és Földtudományi Intézet">FoldrFoldt_I</span>/<span title="Földtudományi Központ">Ft_K</span>/MTA-ELTE Geológiai, Geofizikai és Űrtudományi Kutatócsoport</span>
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;1019032" target="_blank">Triassic sequence stratigraphy of the Transdanubian Range (Hungary)</a></div> <div> <span class="journal-title">GEOLOGICA CARPATHICA</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited By :50
Export Date: 19 January 2023
Correspondence Address: Haas, J.; Academic Research Group, Muzeum korut 4/a, H-1088 Budapest, Hungary</pre>
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;1025551" target="_blank">Triassic sequence stratigraphy of the Balaton Highland, Hungary</a></div> <div> <span class="journal-title">ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0236-5278">0236-5278</a> )</span>:
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<span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 45</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited By :23
Export Date: 3 December 2018</pre>
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University of Vienna, Department of Palaeontology, Universitätstr. 7, A-1010 Wien, Austria
University of Vienna, Department of Geology, Universitätstr. 7, A-1010 Wien, Austria
Cited By :245
Export Date: 28 August 2023
Correspondence Address: Haas, J.; Geological Research Group, the Hungarian Academy of Sciences, Múzeum krt. 4 / a, 1088 Budapest, Hungary
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The present-day setting of the tectonic units (terranes) making up the pre-Neogene basement of the Pannonian Basin and the West Carpathians is the result of large-scale displacements during the Alpine collisional phases. To explain this setting, based on various concepts, a number of models have been proposed in the last decade. Most of them agree in an eastward escape of the ''North Pannonian terrane'' from the Alpine domain towards the Pannonian during the Palaeogene-Early Miocene period.
In the present paper a reconstruction of the pre-escape setting of the displaced terranes is presented based on facies zones in selected time-slices from the Late Permian to the Late Triassic. According to our reconstruction the Inner West Carpathian units were located east of the Austroalpine units forming the northern shelf of the ''Euhallstatt''-Meliatic basin of the Vardar oceanic branch. The Drauzug should have been located in a position much more external than its present-day setting. The Transdanubian Range was situated in the northern neighbourhood of the Southern Alps, whereas the Bukk may have been located adjacent to the NW Dinarides. The Mid-Transdanubian zone is a major shear-zone containing elements of the Julian Alps and Sava folds nappe system and the Inner Dinaric ophiolitic melange.
Although the nappe-tectonism may have played an important role in the structural evolution of the ''North Pannonian terrane'', this mechanism alone can hardly produce hundreds of kilometres of facies offset on the opposite sides of strike-slip zones.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10000315"> <a href="/gui2/?type=authors&mode=browse&sel=10000315" target="_blank">Haas, J</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10007960"> <a href="/gui2/?type=authors&mode=browse&sel=10007960" target="_blank">Kovács, S</a> </span> <span class="author-type"> </span> ; <span class="author-name" > Krystyn, L </span> <span class="author-type"> </span> ; <span class="author-name" > Lein, R </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;1019016" mtid="1019016" target="_blank">Significance of Late Permian-Triassic facies zones in terrane reconstructions in the Alpine-North Pannonian domain</a></div> <div class="pub-info"> <span class="journal-title">TECTONOPHYSICS</span> <span class="journal-volume">242</span> : <span class="journal-issue">1-2</span> <span class="page"> pp. 19-40. , 22 p. </span> <span class="year">(1995)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/0040-1951(94)00157-5" target="_blank" href="https://doi.org/10.1016/0040-1951%2894%2900157-5"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="A1995QL30400003" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/A1995QL30400003"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="0028883039" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-0028883039"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:1019016 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 262</span> | Független: 211 | Függő: 51 | Nem jelölt: 0 | WoS jelölt: 196 | Scopus jelölt: 233 | WoS/Scopus jelölt: 246 | DOI jelölt: 202 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;1019016" target="_blank">Significance of Late Permian-Triassic facies zones in terrane reconstructions in the Alpine-North Pannonian domain</a></div> <div> <span class="journal-title">TECTONOPHYSICS</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Geological Research Group, the Hungarian Academy of Sciences, Múzeum krt. 4 / a, 1088 Budapest, Hungary
University of Vienna, Department of Palaeontology, Universitätstr. 7, A-1010 Wien, Austria
University of Vienna, Department of Geology, Universitätstr. 7, A-1010 Wien, Austria
Cited By :245
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Eötvös University of Budapest, Department of Geology, 1088 Budapest, Múzeum krt. 4 / a, Hungary
Eötvös University of Budapest, Department of Geophysics, 1082 Budapest, Ludovika tér 2, Hungary
Slovakian Academy of Sciences, Department of Geology, 81473 Bratislava, Dúbravska cesta, Czechoslovakia
Cited By :473
Export Date: 11 November 2022
Correspondence Address: Csontos, L.
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TERTIARY EVOLUTION OF THE INTRA-CARPATHIAN AREA - A MODEL
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1992
The Outer Carpathian flysch nappes encircle an Intra-Carpathian domain
which can be divided into two megatectonic units (North Pannonian and
Tisza) mostly on the basis of contrasting Mesozoic and Palaeogene
facies development. We see two major kinematic problems to be solved:
(1) The present distribution of the Mesozoic and Palaeogene facies is
mosaic-like, and some belts form exotic bodies within realms of
Austroalpine affinity. (2) Late Eocene palinspastic reconstruction of
the Outer Carpathian flysch nappes suggest, that the entire
Intra-Carpathian area must have been located several hundreds of
kilometres to the south and to the west of its present position.
Neogene extension can account for shortening in the external Carpathian
nappes, but is unable to explain Mesozoic facies anomalies and offsets
of Palaeogene formations. We suggest that evolution of the
Intra-Carpathian area involved first Late Palaeogene-Early Miocene
juxtaposition of the North-Pannonian and Tisza megatectonic units,
accompanied by the closure of the external Carpathian flysch troughs;
thereafter extension of this amalgamated unit occurred, which was
compensated by thrusting of flysch nappes onto the European foreland
and formation of molasse foredeeps.
Eastward escape of the North-Pannonian unit from the Alpine collisional
belt involved left lateral shear along the Pieniny Klippen belt and
right lateral shear along the Mid-Hungarian zone. Parts of the Late
Palaeogene basin and an Early Miocene volcanic edifice were dissected,
offset and elongated by several 100 kms. The driving mechanism of the
eastward escape of the Intra-Carpathian area can be related to the
collision of Apulia and Europe and the subduction of the external
Carpathian crust under the Pannonian units. The escape ceased gradually
in the Early Miocene, when oblique collision between the
North-Pannonian unit and European continent occurred.
Neogene extension of the Pannonian region was an areal deformation. The
extension at locally variable rate resulted in the break-up of the
heterogenous floor of the Neogene basin.
The driving mechanism of basin extension and contemporaneous
compressional deformation of the external Carpathians is thought to be
related to ongoing subduction, involving the marginal part of the
attenuated European continental crust. Tectonic activity in the
Carpathians and basin subsidence and volcanism shifted in time and in
unison from the west toward the east-southeast.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > CSONTOS, L </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10005632"> <a href="/gui2/?type=authors&mode=browse&sel=10005632" target="_blank">NAGYMAROSY, A</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10002672"> <a href="/gui2/?type=authors&mode=browse&sel=10002672" target="_blank">HORVATH, F</a> </span> <span class="author-type"> </span> ; <span class="author-name" > KOVAC, M </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;1255443" mtid="1255443" target="_blank">TERTIARY EVOLUTION OF THE INTRA-CARPATHIAN AREA - A MODEL</a></div> <div class="pub-info"> <span class="journal-title">TECTONOPHYSICS</span> <span class="journal-volume">208</span> : <span class="journal-issue">1-3</span> <span class="page"> pp. 221-241. , 21 p. </span> <span class="year">(1992)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/0040-1951(92)90346-8" target="_blank" href="https://doi.org/10.1016/0040-1951%2892%2990346-8"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="A1992JK74400015" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/A1992JK74400015"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="0026463611" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-0026463611"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:1255443 </span> <span class="status-holder"><span class="status-data status-APPROVED"> Nyilvános </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 485</span> | Független: 433 | Függő: 52 | Nem jelölt: 0 | WoS jelölt: 402 | Scopus jelölt: 425 | WoS/Scopus jelölt: 474 | DOI jelölt: 379 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;1255443" target="_blank">TERTIARY EVOLUTION OF THE INTRA-CARPATHIAN AREA - A MODEL</a></div> <div> <span class="journal-title">TECTONOPHYSICS</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0040-1951">0040-1951</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1879-3266">1879-3266</a>)</span>:
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Idézett közlemények száma: 14
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<div class="mtid"><span class="long-pub-mtid">Közlemény: 1255443</span>
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<div class="lastModified">Utolsó módosítás: 2021.09.08. 17:16 Tari Gábor (Geofizika, geológia)
</div>
<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Eötvös University of Budapest, Department of Geology, 1088 Budapest, Múzeum krt. 4 / a, Hungary
Eötvös University of Budapest, Department of Geophysics, 1082 Budapest, Ludovika tér 2, Hungary
Slovakian Academy of Sciences, Department of Geology, 81473 Bratislava, Dúbravska cesta, Czechoslovakia
Cited By :473
...</pre>
</div></div>