https://m2.mtmt.hu/ hun 2026-03-07 06:23 JournalArticle 1506102 ADMIN_APPROVED true 0 2018-10-02T08:54:25.000+0000 false 1506102 2026-03-05T08:31:14.047+0000 2025-11-12T16:13:23.176+0000 2011-04-22T21:40:11.000+0000 true 10015050 Németh Károly /api/author/10015050 Author true 10015050 2025-11-12T16:13:23.656+0000 2025-11-12T16:13:23.656+0000 2011-11-11T12:29:10.000+0000 true 10014568 Vándor Andrea /api/admin/10014568 Admin true 10014568 Admin 10065569 /api/admin/10065569 Pécsi Éva true true 2025-11-17T10:33:32.020+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 Kereszturi, G The role of external environmental factors in changing eruption styles of monogenetic volcanoes in a Mio/Pleistocene continental volcanic field in western Hungary true true /api/journal/2944 REVIEWED true false 2944 false 2944 true 0377-0273 1872-6097 Journal FOREIGN 201 1-4 227 240 227 14 2011 true 222334 /api/conference/222334 true 12484 true 10049 /api/country/10049 Country true 2151477 /api/city/12484 City true 10002135 Conference true The occurrence, shape, structure and eruption style of monogenetic volcanoes, such as maars, tuff rings, tuff cones and scoria cones, are generally governed by several internal (composition of the magma, magmatic flux, ascent rate, viscosity, volatile contents) and external conditions (regional and local tectonics, topography, and the presence of surfacial, ground and meteoric water). These controlling factors are together responsible for the eruption style, distribution pattern, volcanic facies architecture and morphology of the monogenetic volcanic landforms. The Late Miocene to Pleistocene Bakony-Balaton Highland Volcanic Field (BBHVF) in western Hungary is a typical small sized (< 50 eruption centres), basaltic, intraplate "monogenetic" volcanic field. Generally, initial eruptions of the BBHVF were phreatomagmatic (n = ~. 28); however, a lesser number (n = ~. 14) of predominantly scoria cone forming eruptions are also inferred. The temporal distribution of the Strombolian style scoria cones was concentrated mostly between 3 and 2.5. Ma. A detailed study of the changes in eruption styles recorded in the pyroclastic sequences suggested a change from a conventional phreatomagmatic to a magmatic fragmentation style during the activity of the volcanic field. A clear correlation has been identified between the long-term environmental changes of the region that resulted in a gradual shift from a more phreatomagmatic eruption style to a more magmatic eruption style. Detailed examination of the temporal distribution of K-Ar and Ar-Ar radiometric data, Digital Elevation Model and Dense Rock Equivalent-based volume calculations of eruptive products and origin of pyroclastic rocks (e.g. phreatomagmatic or magmatic) preserved in variously eroded monogenetic volcanoes were utilized to integrate available volcanological and climatological data to identify potential links between external and internal controlling parameters that responsible for long-term eruption style changes. At least 6 volcanic cycles have been identified by cluster analysis. Time gap between the cycles were vary from 1.66 up to 0.06Ma, while the average eruption recurrence rate was ~0.1078Ma/event. The time-volume diagram of the volcanism of BBHVF have shown time-predictive behavior combined with low magma-flux (total preserved volume ~2.867km3) and output rates (0.53km3/Ma for the entire volcanic field and 0.90km3/Ma for the last 5cycles), suggesting that volcanism was largely tectonically-controlled and not magmatically-controlled.Furthermore, the topographic differences between the northern ("elevated") and southern ("basin-like") parts of the volcanic field, are also important in local differences in dominant fragmentation style, because the elevated part of the field was prone to host large, more magmatically-evolved volcanoes, than on the lower, water-saturated, unconsolidated sediments, which favored to the magma/water interaction driven phreatomagmatic fragmentation. The third controlling parameter, which seems to play an important role in controlling the eruptive style of monogenetic volcanism at BBHVF, was the paleoclimate fluctuation, especially during the time interval of 3.0 to 2.5. Ma. Thus, mainly the long-term environmental changes (e.g. aridification) have been response the shifting fragmentation style from phreatomagmatic to more magmatic ones. © 2010 Elsevier B.V. 2011 true true true true true false PAY 2026-03-05 false true 10045349 Fekete Rita /api/admin/10045349 Admin true 10045349 89 0 86 53 24 85 83 76 78 81 81 50 50 56 33 0 89 56 86 53 0 29 29 Folyóiratcikk Journal Article 24 80 Könyvrészlet Chapter in Book 25 6 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 3 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 2010 0 2 0 2 0 2011 0 2 1 2 1 2012 0 11 6 11 6 2013 0 3 1 3 1 2014 0 2 1 2 1 2015 0 7 4 7 4 2016 0 8 6 8 6 2017 0 6 4 6 4 2018 0 2 2 2 2 2019 0 6 4 6 4 2020 0 10 7 10 7 2021 0 7 6 7 6 2022 0 6 5 6 5 2023 0 7 3 7 3 2024 0 4 2 4 2 2025 0 4 4 4 4 2026 0 2 0 2 0 Q1 A false false false false 2011-11-11T12:29:10.000+0000 2013-02-23T19:18:00.000+0000 Földtani és Meteorológiai Tanszék (PTE / TTK / FI); MTA Atommagkutató Intézet 4 31 2 5 0 true 10065569 Language 10002 /api/language/10002 Angol English true 2 true PersonAuthorship 1561799 /api/authorship/1561799 1 0.2 true false true Kereszturi G true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false 12230682 true PersonAuthorship 1561800 /api/authorship/1561800 2 0.2 false false Author 10015050 /api/author/10015050 Németh Károly true 10015050 true Németh K true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false 12230681 true PersonAuthorship 1561801 /api/authorship/1561801 3 0.2 false false Author 10012053 /api/author/10012053 Csillag Gábor true 10012053 true Csillag G true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false 12230680 true PersonAuthorship 1561802 /api/authorship/1561802 4 0.2 false false Author 10004890 /api/author/10004890 Balogh Kadosa true 10004890 true Balogh K true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false 12230679 true PersonAuthorship 1561803 /api/authorship/1561803 5 0.2 false true Author 10001005 /api/author/10001005 Kovács János true 10001005 true Kovács J true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false 12230678 true PublicationIdentifier 367780 /api/publicationidentifier/367780 PlainSource 6 /api/publicationsource/6 PublicationSourceType 10001 /api/publicationsourcetype/10001 true true true DOI DOI https://doi.org/@@@ true true 6 true PAY false IDENTICAL 10.1016/j.jvolgeores.2010.08.018 https://doi.org/10.1016/j.jvolgeores.2010.08.018 false 211726 true PublicationIdentifier 367778 /api/publicationidentifier/367778 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 false IDENTICAL 000289963900017 https://www.webofscience.com/wos/woscc/full-record/000289963900017 false 211727 true PublicationIdentifier 367779 /api/publicationidentifier/367779 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 false IDENTICAL 79953048662 http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-79953048662 false 211728 true Classification 10399 /api/classification/10399 true true Classification 10423 /api/classification/10423 true true Keyword 8180 /api/keyword/8180 true 8180 true Keyword 20016 /api/keyword/20016 true 20016 true Keyword 1002843 /api/keyword/1002843 true 1002843 true Keyword 1002977 /api/keyword/1002977 true 1002977 true Keyword 1002978 /api/keyword/1002978 true 1002978 true Keyword 1002979 /api/keyword/1002979 true 1002979 true Keyword 1002980 /api/keyword/1002980 true 1002980 true Keyword 1058174 /api/keyword/1058174 true 1058174 true MtaRating 11435122 /api/mtarating/11435122 RatingType 10031 /api/ratingtype/10031 X. 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;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10012053"><a href="/gui2/?type=authors&mode=browse&sel=10012053" target="_blank">Csillag G (<span class="authorship-author-name">Csillag Gábor</span> <span class="authorAux-mtmt"> Rétegtan, geomorfológia, távérzékelés</span>) </a> </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10004890"><a href="/gui2/?type=authors&mode=browse&sel=10004890" target="_blank">Balogh K (<span class="authorship-author-name">Balogh Kadosa</span> <span class="authorAux-mtmt"> Izotóp geológia</span>) </a> </span> <span class="author-affil">MTA Atommagkutató Intézet</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10001005"><a href="/gui2/?type=authors&mode=browse&sel=10001005" target="_blank">Kovács J (<span class="authorship-author-name">Kovács János</span> <span class="authorAux-mtmt"> Földtan</span>) </a> </span> <span class="author-affil"><span title="Pécsi Tudományegyetem">PTE</span>/<span title="Természettudományi Kar">TTK</span>/<span title="Földrajzi Intézet">FI</span>/Földtani és Meteorológiai Tanszék</span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;1506102" target="_blank">The role of external environmental factors in changing eruption styles of monogenetic volcanoes in a Mio/Pleistocene continental volcanic field in 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">201</span> <span class="journal-issue">1-4</span> <span class="page"> pp 227-240 </span> <span class="year">(2011)</span> <div class="conference"> 3rd International Maar Conference (3IMC). Konferencia helye, ideje: <span class="location">Malargüe, Argentína <span class="conference-date">2009.04.14. - 2009.04.17.</span> </div> </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_PAY" title=" Fizetős "> <a style="color:blue" title="10.1016/j.jvolgeores.2010.08.018" target="_blank" href="https://doi.org/10.1016/j.jvolgeores.2010.08.018"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000289963900017" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000289963900017"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="79953048662" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-79953048662"> 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: 89</span> | Független: 56 | Függő: 33 | Nem jelölt: 0 | WoS jelölt: 76 | Scopus jelölt:&nbsp;78 | WoS/Scopus jelölt:&nbsp;81 | DOI jelölt:&nbsp;83 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;1506102&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 29 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 1506102</span> | <span class="status-data status-ADMIN_APPROVED"> Admin láttamozott </span> <span class="oldId">Régi azonosító: 1506102</span> | Forrás Idéző | <span class="type-subtype">Folyóiratcikk ( Szakcikk ) </span> | <span class="pub-category">Tudományos</span> | <span class="publication-sourceOfData">Scopus</span> </div> <div class="lastModified">Utolsó módosítás: 2025.11.12. 17:13 Pécsi Éva (MTMT Közp 2,3, admin) </div> <div class="lockedBy">Központi kezelésű 2025.11.17. 11:33 Pécsi Éva (MTMT Közp 2,3, admin) </div> </div></div>