https://m2.mtmt.hu/ hun 2026-09-22 14:36 JournalArticle 35437340 VALIDATED true 1 false 2026-09-19T19:39:31.977+0000 2025-02-10T13:23:43.796+0000 2024-10-06T11:29:25.478+0000 true 10010631 Pap Norbert /api/author/10010631 Author true 10010631 2026-06-12T09:55:56.544+0000 2026-06-12T09:55:56.544+0000 2025-03-08T00:59:56.318+0000 true 521 Szuper Admin /api/admin/521 Admin true Admin 10097583 /api/admin/10097583 Zolnai Dóra true true Admin 10067876 /api/admin/10067876 Ladányi Gusztáv true true 2024-10-17T17:00:58.826+0000 true false true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle true 10000059 Article true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle /api/subtype/10000059 Szakcikk SubType 101 true 10000059 true 1 /api/category/1 Category true 1 Timkó, M Crustal and upper mantle 3-D Vs structure of the Pannonian region from joint earthquake and ambient noise Rayleigh wave tomography true true /api/journal/1705 REVIEWED true false 1705 false 1705 true 0956-540X 1365-246X Journal FOREIGN 239 2 1313 1334 1313 22 2024 The Pannonian Basin, situated in Central Europe, is surrounded by the Alpine, Carpathian and Dinaric orogens. To understand its tectonic characteristics and evolution, we determine a shear wave velocity model of its crust, mantle lithosphere and asthenosphere consistently by jointly inverting Rayleigh wave phase velocities measured consistently from earthquake (EQ) and ambient noise (AN) data. For the AN data, continuous waveform data were collected from 1254 stations, covering an area within 9° from the centre of the Pannonian Basin during the time period from 2006 to 2018. This data set enabled the extraction of over 164 464 interstation Rayleigh phase-velocity curves, after applying a strict quality control workflow. For the EQ data set more than 2000 seismic events and about 1350 seismic stations were used in the broader Central and Eastern European region between the time-span of 1990 to 2015, allowing us to extract 139 987 quality controlled Rayleigh wave phase-velocity curve. Using the combined data set, a small period- and distance-dependent bias between ambient noise and earthquake measurements, mostly below 1 per cent but becoming larger towards longer periods has been found. After applying a period and distance dependent correction, we generated phase-velocity maps, spanning periods from 5 to 250 s. 33 981 local dispersion curves were extracted and a new approach is introduced to link their period-dependent roughness to the standard deviation. Using a non-linear stochastic particle swarm optimization, a consistent 3-D shear wave velocity model (PanREA2023) encompassing the crust and upper mantle down to 300 km depth was obtained with a lateral resolution reaching about 50 km at the centre of the study area for shorter periods. The crust beneath the Carpathian orogen exhibits a distinct low-velocity anomaly extending down to the Moho. It is referred to as Peri-Carpathian anomaly. Similar anomalies were observed in the Northern Apennines, while the Eastern Alps and Dinarides, as collisional orogens, generally demonstrate higher velocities in the upper crust. High crustal shear wave velocities are also evident in the Bohemian Massif and the East European Craton. The brittle upper crust of the Pannonian Basin is characterized by alternating NE–SW trending high- and low-velocity anomalies: the western and central Pannonian low-velocity anomalies and the Transdanubian and Apuseni high-velocity anomalies related to Miocene sedimentary basins and intervening intervening interbasinal highs exposing Pre-Cenozoic rocks including crystalline basement rocks. Beneath the Southeastern Carpathians, a NE-dipping slab was identified, extending to depths of at least 200 km, while a slab gap is evident beneath the Western Carpathians. A short south-dipping Eurasian slab was imaged beneath the Eastern Alps down to only 150–200 km depth. The Adriatic lithosphere is subducting near-vertically dipping beneath the Northern Apennines, and a slab gap was observed beneath the Central Apennines. In the Northern Dinarides, a short slab was evident, reaching depths of around 150 km. The Southern Dinarides featured a thinned but possibly incompletely detached slab. true true 2024 true true true false false false GOLD 2026-09-19 true https://doi.org/10.1093/gji/ggae314 10 0 10 6 3 10 10 10 6 10 10 6 6 6 4 0 10 6 10 6 0 30 30 Folyóiratcikk Journal Article 24 10 Könyvrészlet Chapter in Book 25 0 Könyv Book 23 0 Egyéb konferenciaközlemény Conference paper 31 0 Egyéb konferenciakötet Conference proceedings 32 0 Oltalmi formák Protection forms 26 0 Disszertáció Thesis 28 0 Egyéb Miscellaneous 29 0 Alkotás Achievement 22 0 Kutatási adat Research data 33 0 Folyóiratcikk Journal Article 24 0 0 0 Könyvrészlet Chapter in Book 25 0 0 0 Könyv Book 23 0 0 0 Egyéb konferenciaközlemény Conference paper 31 0 0 0 Egyéb konferenciakötet Conference proceedings 32 0 0 0 Oltalmi formák Protection forms 26 0 0 0 Disszertáció Thesis 28 0 0 0 Egyéb Miscellaneous 29 0 0 0 Alkotás Achievement 22 0 0 0 Kutatási adat Research data 33 0 0 0 2025 0 6 2 6 2 2026 0 4 4 4 4 Q1 A false false false false 2024-11-03T10:31:22.379+0000 Földrajz- és Földtudományi Intézet (ELTE / TTK); HUN-REN Földfizikai és Űrtudományi Kutatóintézet; Általános és Alkalmazott Földtani Tanszék (ELTE / TTK / Ft_K) 3 19 3 8 0 true 10097583 10067876 Language 10002 /api/language/10002 Angol English true 2 true PersonAuthorship 120782362 /api/authorship/120782362 1 0.143 true false true Author 10066197 /api/author/10066197 Timkó Máté true true Timkó M true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 120782363 /api/authorship/120782363 2 0.14285715 false false false El-Sharkawy A true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 120782364 /api/authorship/120782364 3 0.14285715 false false false Wiesenberg L true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 120782365 /api/authorship/120782365 4 0.14285715 false false false Author 10000210 /api/author/10000210 Fodor László true 10000210 true Fodor L true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 120782366 /api/authorship/120782366 5 0.14285715 false false false Author 10007787 /api/author/10007787 Wéber Zoltán true 10007787 true Wéber Z true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 120782367 /api/authorship/120782367 6 0.14285715 false false false Lebedev S true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 120782368 /api/authorship/120782368 7 0.14285715 false false false Eckel F true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 123191865 /api/authorship/123191865 8 0.0 false true Meier T true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true OrgAuthorship 123191897 /api/authorship/123191897 9 0.0 false false true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PublicationIdentifier 27589154 /api/publicationidentifier/27589154 PlainSource 6 /api/publicationsource/6 PublicationSourceType 10001 /api/publicationsourcetype/10001 true true true DOI DOI https://doi.org/@@@ true true 6 true GOLD true IDENTICAL 10.1093/gji/ggae314 https://doi.org/10.1093/gji/ggae314 false true PublicationIdentifier 27640911 /api/publicationidentifier/27640911 PlainSource 1 /api/publicationsource/1 PublicationSourceType 10003 /api/publicationsourcetype/10003 false true true WoS WoS https://www.webofscience.com/wos/woscc/full-record/@@@ true true 1 true IDENTICAL 001325932700001 https://www.webofscience.com/wos/woscc/full-record/001325932700001 true true PublicationIdentifier 32475044 /api/publicationidentifier/32475044 SwordSource 92 /api/publicationsource/92 PublicationSourceType 10007 /api/publicationsourcetype/10007 true true true EDIT EDIT https://edit.elte.hu/handle/10831/@@@ true true 92 true GREEN true 121037 https://edit.elte.hu/handle/10831/121037 false true PublicationIdentifier 27687292 /api/publicationidentifier/27687292 PlainSource 3 /api/publicationsource/3 PublicationSourceType 10003 /api/publicationsourcetype/10003 false true true Scopus Scopus http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-@@@ true true 3 true IDENTICAL 85206442176 http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85206442176 true true MtaRating 11435073 /api/mtarating/11435073 RatingType 10031 /api/ratingtype/10031 X. 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<span class="author-name" mtid="10066197"><a href="/gui2/?type=authors&mode=browse&sel=10066197" target="_blank">Timkó M ✉ (<span class="authorship-author-name">Timkó Máté</span> <span class="authorAux-mtmt"> Szeizmológia</span>) </a> </span> <span class="author-affil">HUN-REN Földfizikai és Űrtudományi Kutatóintézet</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >El-Sharkawy A </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Wiesenberg L </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10000210"><a href="/gui2/?type=authors&mode=browse&sel=10000210" target="_blank">Fodor L (<span class="authorship-author-name">Fodor László</span> <span class="authorAux-mtmt"> Geológia</span>) </a> </span> <span class="author-affil"><span title="Eötvös Loránd Tudományegyetem">ELTE</span>/<span title="Természettudományi Kar">TTK</span>/Földrajz- és Földtudományi Intézet; HUN-REN Földfizikai és Űrtudományi Kutatóintézet; <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>/Általános és Alkalmazott Földtani Tanszék</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10007787"><a href="/gui2/?type=authors&mode=browse&sel=10007787" target="_blank">Wéber Z (<span class="authorship-author-name">Wéber Zoltán</span> <span class="authorAux-mtmt"> Szeizmológia</span>) </a> </span> <span class="author-affil">HUN-REN Földfizikai és Űrtudományi Kutatóintézet</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Lebedev S </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Eckel F </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Meier T </span> ;&nbsp;&nbsp;&nbsp; <span class="author-affil">AlpArray Working Group</span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;35437340" target="_blank">Crustal and upper mantle 3-D Vs structure of the Pannonian region from joint earthquake and ambient noise Rayleigh wave tomography</a></div> <div> <span class="journal-title">GEOPHYSICAL JOURNAL INTERNATIONAL</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0956-540X">0956-540X</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1365-246X">1365-246X</a>)</span>: <span class="journal-volume">239</span> <span class="journal-issue">2</span> <span class="page"> pp 1313-1334 </span> <span class="year">(2024)</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_GOLD" title=" Gold "> <a style="color:blue" title="10.1093/gji/ggae314" target="_blank" href="https://doi.org/10.1093/gji/ggae314"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="001325932700001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/001325932700001"> WoS </a> </span> <span class="id identifier oa_GREEN" title=" Green "> <a style="color:black" title="121037" target="_blank" href="https://edit.elte.hu/handle/10831/121037"> EDIT </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85206442176" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85206442176"> Scopus </a> </span> </span> <OnlyViewableByAuthor><div class="ratings"> <div class="journal-subject">Folyóirat szakterülete: Scopus - Geochemistry and Petrology&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;Q1</div> <div class="journal-subject">Folyóirat szakterülete: Scopus - Geophysics&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;Q1</div> <div class="journal-subject">X. Földtudományok Osztálya XFO&nbsp;&nbsp;&nbsp;A</div> </div></OnlyViewableByAuthor> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 10</span> | Független: 6 | Függő: 4 | Nem jelölt: 0 | WoS jelölt: 10 | Scopus jelölt:&nbsp;6 | WoS/Scopus jelölt:&nbsp;10 | DOI jelölt:&nbsp;10 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;35437340&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 30 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 35437340</span> | <span class="status-data status-VALIDATED"> Egyeztetett </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: 2025.02.10. 14:23 Brányi Gyöngyi (Földfizikai és Űrtud. Kutint. admin4) </div> <div class="lockedBy">Központi kezelésű 2024.10.17. 19:00 Zolnai Dóra (MTMT ellenőrzés, admin) Ladányi Gusztáv (MTMT API user, admin) </div> </div></div>