https://m2.mtmt.hu/ hun 2026-04-15 19:43 JournalArticle 21749655 ADMIN_APPROVED true 0 2018-10-01T21:27:49.000+0000 false 11749655 2026-03-23T23:09:03.617+0000 2022-03-03T17:14:53.347+0000 2011-12-10T11:42:39.000+0000 true 10001308 Kázmér Miklós /api/author/10001308 Author true 10001308 2022-03-10T17:28:27.021+0000 2022-03-10T17:28:27.021+0000 2022-03-03T17:14:53.355+0000 true 10003133 Boros Annamária /api/admin/10003133 Admin true 10003133 Admin 10003133 /api/admin/10003133 Boros Annamária true 10003133 true 2022-03-22T18:24:48.781+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 Martin, U Blocky versus fluidal peperite textures developed in volcanic conduits, vents and crater lakes of phreatomagmatic volcanoes in Mio/Pliocene volcanic fields of Western Hungary true true /api/journal/2944 REVIEWED true false 2944 false 2944 true 0377-0273 1872-6097 Journal FOREIGN 159 1-3 164 178 164 15 2007 Volcanic fields in the Pannonian Basin, Western Hungary, comprise several Mio/Pliocene volcaniclastic successions that are penetrated by numerous mafic intrusions. Peperite formed where intrusive and extrusive basaltic magma mingled with tuff, lapilli-tuff, and non-volcanic siliciclastic sediments within vent zones. Peperite is more common in the Pannonian Basin than generally realised and may be also important in other settings where sediment sequences accumulate during active volcanism. Hajagos-hegy, an erosional remnant of a maar volcano, was subsequently occupied by a lava lake that interacted with unconsolidated sediments in the maar basin and formed both blocky and globular peperite. Similar peperite developed in Kissomlyo, a small tuff ring remnant, where dykes invaded lake sediments that formed within a tuff ring. Lava foot peperite from both Hajagos-hegy and Kissomlyo were formed when small lava flows travelled over wet sediments in craters of phreatomagmatic volcanoes. At Sag-hegy, a large phreatomagmatic volcanic complex, peperite formed along the margin of a coherent intrusion. All peperite in this study could be described as globular or blocky peperite. Globular and blocky types in the studied fields occur together regardless of the host sediment. (c) 2006 Elsevier B.V. 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<span class="author-name" mtid="10015050"><a href="/gui2/?type=authors&mode=browse&sel=10015050" target="_blank">Nemeth K (<span class="authorship-author-name">Németh Károly</span> <span class="authorAux-mtmt"> Vulkanológia, szedimentológia</span>) </a> </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;21749655" target="_blank">Blocky versus fluidal peperite textures developed in volcanic conduits, vents and crater lakes of phreatomagmatic volcanoes in Mio/Pliocene volcanic fields of Western Hungary</a></div> <div> <span class="journal-title">JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0377-0273">0377-0273</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1872-6097">1872-6097</a>)</span>: <span class="journal-volume">159</span> <span class="journal-issue">1-3</span> <span class="page"> pp 164-178 </span> <span class="year">(2007)</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="10.1016/j.jvolgeores.2006.06.010" target="_blank" href="https://doi.org/10.1016/j.jvolgeores.2006.06.010"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000243607900010" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000243607900010"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="33845548797" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-33845548797"> 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: 81</span> | Független: 59 | Függő: 22 | Nem jelölt: 0 | WoS jelölt: 75 | Scopus jelölt:&nbsp;45 | WoS/Scopus jelölt:&nbsp;75 | DOI jelölt:&nbsp;77 (Nem nyilvános:&nbsp;2) </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;21749655&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 12 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 21749655</span> | <span class="status-data status-ADMIN_APPROVED"> Admin láttamozott </span> <span class="oldId">Régi azonosító: 11749655</span> | Forrás Idéző | <span class="type-subtype">Folyóiratcikk ( Szakcikk ) </span> | <span class="pub-category">Tudományos</span> | <span class="publication-sourceOfData">WOS</span> </div> <div class="lastModified">Utolsó módosítás: 2022.03.03. 18:14 Boros Annamária (MTMT Központi admin) </div> <div class="lockedBy">Központi kezelésű 2022.03.22. 19:24 Boros Annamária (MTMT Központi admin) </div> </div></div>