https://m2.mtmt.hu/ eng 2026-10-25 09:48 JournalArticle 34215689 VALIDATED true 0 false 2026-10-23T22:38:07.415+0000 2025-02-26T14:23:24.981+0000 2023-10-25T10:46:45.525+0000 true 10059939 Kalmár Dániel /api/author/10059939 Author true 10059939 2026-06-12T09:55:41.513+0000 2026-06-12T09:55:41.513+0000 2025-03-21T03:07:26.189+0000 true 521 Szuper Admin /api/admin/521 Admin true Admin 10013962 /api/admin/10013962 Vasvari Lilian true 10013962 true 2024-04-08T14:20:54.918+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 Dániel, Kalmár Lithospheric Structure of the Circum-Pannonian Region Imaged by S-To-P Receiver Functions true true /api/journal/10000479 REVIEWED true false 10000479 false 10000479 true 1525-2027 Journal FOREIGN 24 9 e2023GC010937 e2023GC010937 19 2023 The lithosphere‐asthenosphere boundary and mid‐lithospheric discontinuities are primary attributes of the upper mantle. The Pannonian region is an extensional sedimentary basin enclosed by collisional orogens. Here, we estimate the negative phase depth of S‐to‐P receiver functions to image the lithospheric thickness and other discontinuities with high resolution, based on the recent dense seismological broadband networks. The lithosphere‐asthenosphere boundary is relatively shallow (<90 km) in the Pannonian Basin system, and deeper (∼90–140 km) in the surrounding orogens, where average surface heat flow values are higher (120 mW/m<jats:sup>2</jats:sup>) and lower (50–70 mW/m<jats:sup>2</jats:sup>), respectively. The 1D and 2D common conversion point migration with 3D velocity model provide comparable but different resolution images beneath the wider region of the Pannonian Basin. We obtained deeper values in the Western (∼120 km) and Southern‐Carpathians orogens (∼135 km). Furthermore, we provide new information on the lithospheric thickness and its seismic properties in the eastern part of the study region (e.g., Apuseni Mountains (∼95 km), Eastern‐Carpathians (∼120 km), Moesian Platform (∼90 km) and Transylvanian Basin (∼85 km). The shallower negative phase depth can be interpreted as the lithosphere‐asthenosphere boundary beneath the Pannonian Basin system in agreement with its high heat flow values. In contrast, the deeper negative phase depth estimates in the colder surroundings can be interpreted as intra‐ or mid‐lithospheric discontinuities, when compared with local seismic tomography models. 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URL Other URL @@@ true true 40 true IDENTICAL https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023GC010937 https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023GC010937 false true SjrRating 11382334 /api/sjrrating/11382334 13 0.1 journal RatingType 10002 /api/ratingtype/10002 sjr true true ClassificationExternal 1908 /api/classificationexternal/1908 true 1908 true D1 DIRECT true true /api/publication/34215689 <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="10059939"><a href="/gui2/?type=authors&mode=browse&sel=10059939" target="_blank">Dániel Kalmár (<span class="authorship-author-name">Kalmár Dániel</span> <span class="authorAux-mtmt"> geofizika</span>) </a> </span> <span class="author-affil">Institute of Earth Physics and Space Science</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Laura Petrescu </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Josip Stipčević </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10038423"><a href="/gui2/?type=authors&mode=browse&sel=10038423" target="_blank">Attila Balázs (<span class="authorship-author-name">Balázs Attila</span> <span class="authorAux-mtmt"> geofizika</span>) </a> </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10022886"><a href="/gui2/?type=authors&mode=browse&sel=10022886" target="_blank">István János Kovács (<span class="authorship-author-name">Kovács István János</span> <span class="authorAux-mtmt"> Földtudományok</span>) </a> </span> <span class="author-affil">Institute of Earth Physics and Space Science</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >the AlpArray </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >the PACASE Working Groups </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;34215689" target="_blank">Lithospheric Structure of the Circum-Pannonian Region Imaged by S-To-P Receiver Functions</a></div> <div> <span class="journal-title">GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS</span> <span class="journal-issn">( <a target="_blank" href="https://portal.issn.org/resource/ISSN/1525-2027">1525-2027</a>)</span>: <span class="journal-volume">24</span> <span class="journal-issue">9</span> <span class="page"> Paper e2023GC010937. 19 p. </span> <span class="year">(2023)</span> </div> <div class="pub-footer"> <span class="language" xmlns="http://www.w3.org/1999/html">Language: English | </span> <span class="identifiers"> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:blue" title="10.1029/2023GC010937" target="_blank" href="https://doi.org/10.1029/2023GC010937"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="001068442000001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/001068442000001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85171321563" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85171321563"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023GC010937" target="_blank" href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023GC010937"> Other URL </a> </span> </span> <OnlyViewableByAuthor><div class="ratings"> <div class="journal-subject">Journal subject: Scopus - Geophysics&nbsp;&nbsp;&nbsp;Rank:&nbsp;D1</div> <div class="journal-subject">Journal subject: Scopus - Geochemistry and Petrology&nbsp;&nbsp;&nbsp;Rank:&nbsp;Q1</div> </div></OnlyViewableByAuthor> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="" class="citingPub-count">Citing papers: 50</span> | Independent citation: 33 | Self citation: 17 | Unknown citation: 0 | Number of citations in WoS: 48 | Number of citations in Scopus:&nbsp;48 | WoS/Scopus assigned:&nbsp;50 | Number of citations with DOI:&nbsp;50 (Not published:&nbsp;9) </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;34215689&sort=publishedYear,desc&sort=title"> Number of cited publications: 44 </a> </div> <div class="mtid"><span class="long-pub-mtid">Publication: 34215689</span> | <span class="status-data status-VALIDATED"> Validated </span> Core Citing | <span class="type-subtype">Journal Article ( Article ) </span> | <span class="pub-category">Scientific</span> | <span class="publication-sourceOfData">kézi felvitel</span> </div> <div class="lastModified">Last Modified: 2025.02.26. 15:23 Gusztáv Ladányi (MTMT API user, admin) </div> <div class="lockedBy">Centrally managed 2024.04.08. 16:20 Lilian Vasvari (MTMT Központ, admin) </div> </div></div>