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Tóth Tivadar</span> <span class="authorAux-mtmt"> Kőzettan</span>) </a> </span> <span class="author-affil"><span title="Szegedi Tudományegyetem">SZTE</span>/<span title="Természettudományi és Informatikai Kar">TTIK</span>/<span title="Földrajzi és Földtani Tanszékcsoport">FFTCS</span>/Ásványtani, Geokémiai és Kőzettani Tanszék</span> ; <span class="author-name" >Zachar J </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse¶ms=publication;1129819" target="_blank">Petrology and deformation history of the metamorphic basement in the Mezősas-Furta crystalline high (SE 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>: <span class="journal-volume">49</span> <span class="journal-issue">2</span> <span class="page"> pp 165-188 </span> <span class="year">(2006)</span> </div> <div class="pub-footer"> <span class="language" xmlns="http://www.w3.org/1999/html">Nyelv: Angol | </span> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1556/AGeol.49.2006.2.4" target="_blank" href="https://doi.org/10.1556/AGeol.49.2006.2.4"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="33750436216" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-33750436216"> Scopus </a> </span> </span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 19</span> | Független: 2 | Függő: 17 | Nem jelölt: 0 | WoS jelölt: 8 | Scopus jelölt: 13 | WoS/Scopus jelölt: 13 | DOI jelölt: 10 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;1129819&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 14 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 1129819</span> | <span class="status-data status-CHECKED"> Hitelesített </span> <span class="oldId">Régi azonosító: 1129819</span> | Forrás Idéző | <span class="type-subtype">Folyóiratcikk ( Szakcikk ) </span> | <span class="pub-category">Tudományos</span> | <span class="publication-sourceOfData">kézi felvitel</span> </div> <div class="lastModified">Utolsó módosítás: 2018.10.11. 16:39 WoS import (admin) </div> <div class="lockedBy">Hitelesítő 2015.11.02. 01:28 Bernátskyné Babus Csilla (SZTE admin4)</div> </div></div>
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Lithospheric structure of the Pannonian basin derived from seismic, gravity and geothermal data
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This paper is part of the special publication No.156, The Mediterranean basins: Tertiary extension within the Alpine Orogen. (eds B.Durand, L. Jolivet, F.Horvath and M.Seranne). The structure of the Pannonian basin is the result of distinct modes of Mid-Late Miocene extension exerting a profound effect on the lithospheric configuration, which continues even today. As the first manifestation of extensional collapse, large magnitude, metamorphic core complex style extension took place at the beginning of the Mid-Miocene in certain parts of the basin. Extrapolation of the present-day high heat flow in the basin, corrected for the blanketing effect of the basin fill, indicates a hot and thin lithosphere at the onset of extension. This initial condition, combined with the relatively thick crust inherited from earlier Alpine compressional episodes, appears to be responsible for the core complex type extension at the beginning of the syn-rift period. This type of extension is well documented in the northwestern Pannonian basin. Newly obtained deep reflection seismic and fission-track data integrated with well data from the southeastern part of the basin suggests that it developed in a similar fashion. Shortly after the initial period, the style of syn-rift extension changed to a wide-rift style, covering an area of much larger geographic extent. The associated normal faults revealed by industry reflection seismic data tend to dominate within the upper crust, obscuring pre-existing structures. However, several deep seismic profiles, constrained by gravity and geothermal modeling, image the entire lithosphere beneath the basin. It is the Mid-Miocene synrift extension which is still reflected in the structure of the Pannonian lithosphere, on the scale of the whole basin system. The gradually diminishing extension during the Late Miocene/Pliocene could not advance to the localization of extension into narrow rift zones in the Pannonian region except some deep subbasins such as the Mako/Bekes and Danube basins. These basins are underlain coincidently by anomalously thin crust (22-25 km) and lithosphere (45-60 km). Significant departures (up to 130 mW m -2) from the average present-day surface heat flow for the initiation of two newly defined narrow rift zones (Tisza and Duna) in the Pannonian basin system. However, both of these narrow rifts failed since the final docking of the Eastern Carpathians onto the European foreland excluded any further extension of the back-arc region.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10079398"> <a href="/gui2/?type=authors&mode=browse&sel=10079398" target="_blank">Tari, G</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10011146"> <a href="/gui2/?type=authors&mode=browse&sel=10011146" target="_blank">Dovenyi, P</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10007580"> <a href="/gui2/?type=authors&mode=browse&sel=10007580" target="_blank">Dunkl, I</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" mtid="10012162"> <a href="/gui2/?type=authors&mode=browse&sel=10012162" target="_blank">Lenkey, L</a> </span> <span class="author-type"> </span> ; <span class="author-name" > Szafian, P </span> <span class="author-type"> </span> ; <span class="author-name" > Toth, T </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;1256307" mtid="1256307" target="_blank">Lithospheric structure of the Pannonian basin derived from seismic, gravity and geothermal data</a></div> <div class="pub-info"> <span class="journal-title">GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS</span> <span class="journal-volume">156</span> <span class="page"> pp. 215-250. , 36 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="10.1144/GSL.SP.1999.156.01.12" target="_blank" href="https://doi.org/10.1144/GSL.SP.1999.156.01.12"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="0342948766" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-0342948766"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:1256307 </span> <span class="status-holder"><span class="status-data status-ADMIN_APPROVED"> Admin láttamozott </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: 211</span> | Független: 169 | Függő: 42 | Nem jelölt: 0 | WoS jelölt: 178 | Scopus jelölt: 206 | WoS/Scopus jelölt: 207 | DOI jelölt: 189 </div> </div> </div> </div><div class="JournalArticle Publication long-list"> <div class="authors"> <img title="Forrásközlemény" style="float: left" src="/frontend/resources/grid/publication-core-icon.png"> <img title="Idézőközlemény" style="float: left" src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" mtid="10079398"><a href="/gui2/?type=authors&mode=browse&sel=10079398" target="_blank">Tari G (<span class="authorship-author-name">Tari Gábor</span> <span class="authorAux-mtmt"> Geofizika, geológia</span>) </a> </span> ; <span class="author-name" mtid="10011146"><a href="/gui2/?type=authors&mode=browse&sel=10011146" target="_blank">Dovenyi P (<span class="authorship-author-name">Dövényi Péter</span> <span class="authorAux-mtmt"> Geofizika</span>) </a> </span> <span class="author-affil"><span title="MTA Támogatott Kutatócsoportok">MTA TKI</span>/MTA-ELTE Geofizikai és Környezettudományi Kutatócsoport (2002-2006-ig: MTA-ELTE Geofizikai és Környezetfizikai Kutatócsoport, 2006 végéig működött)</span> ; <span class="author-name" mtid="10007580"><a href="/gui2/?type=authors&mode=browse&sel=10007580" target="_blank">Dunkl I (<span class="authorship-author-name">Dunkl István</span> <span class="authorAux-mtmt"> Geokémia</span>) </a> </span> ; <span class="author-name" mtid="10002672"><a href="/gui2/?type=authors&mode=browse&sel=10002672" target="_blank">Horvath F (<span class="authorship-author-name">Horváth Ferenc</span> <span class="authorAux-mtmt"> Geofizika</span>) </a> </span> <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>/Geofizikai és Űrtudományi Tanszék</span> ; <span class="author-name" mtid="10012162"><a href="/gui2/?type=authors&mode=browse&sel=10012162" target="_blank">Lenkey L (<span class="authorship-author-name">Lenkey László</span> <span class="authorAux-mtmt"> Geotermika, geodinamika</span>) </a> </span> <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> ; <span class="author-name" >Szafian P </span> ; <span class="author-name" >Toth T </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse¶ms=publication;1256307" target="_blank">Lithospheric structure of the Pannonian basin derived from seismic, gravity and geothermal data</a></div> <div> <span class="journal-title">GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0305-8719">0305-8719</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/2041-4927">2041-4927</a>)</span>: <span class="journal-volume">156</span> <span class="page"> pp 215-250 </span> <span class="year">(1999)</span> </div> <div class="pub-footer"> <span class="language" xmlns="http://www.w3.org/1999/html">Nyelv: Angol | </span> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1144/GSL.SP.1999.156.01.12" target="_blank" href="https://doi.org/10.1144/GSL.SP.1999.156.01.12"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="0342948766" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-0342948766"> Scopus </a> </span> </span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 211</span> | Független: 169 | Függő: 42 | Nem jelölt: 0 | WoS jelölt: 178 | Scopus jelölt: 206 | WoS/Scopus jelölt: 207 | DOI jelölt: 189 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;1256307&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 27 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 1256307</span> | <span class="status-data status-ADMIN_APPROVED"> Admin láttamozott </span> <span class="oldId">Régi azonosító: 1256307</span> | Forrás Idéző | <span class="type-subtype">Folyóiratcikk ( Szakcikk ) </span> | <span class="pub-category">Tudományos</span> | <span class="publication-sourceOfData">kézi felvitel</span> </div> <div class="lastModified">Utolsó módosítás: 2021.11.12. 15:37 Mikola Katalin (MTMT 3, admin) </div> </div></div>