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REVIEWEDtruefalse2944false2944true0377-02731872-6097JournalFOREIGN1772441456441162008Pula maar is a partially eroded Pliocene maar-diatreme volcano, part of the Mio-Pliocene Bakony-Balaton Highland Volcanic Field. The surficial remnant of the maar-diatreme volcano consists of (1) a distinct depression with a thick post-eruptive lacustrine alginite sediment infill interbedded with coarse-grained volcaniclastic sediments, (2) a narrow marginal zone inside the depression consisting of primary pyroclastic rock units that are interpreted to be partly collapsed and subsided blocks of entire sections from the tephra ring formerly surrounding the maar crater depression, and (3) coarse-grained volcaniclastic debris-flow deposits closely associated with the collapsed primary pyroclastic rock units in the marginal zone. The presence of coherent lava rocks below the crater-fill units, their distribution pattern and their association with scoriaceous beds indicate that, after the maar-diatreme-forming phreatomagmatic explosive activity, small (100 m-scale) scoria and/or spatter cones erupted in the maar crater. These cones are the likely source of the lava flows that partially filled the maar crater basin. The widespread dm-to-m thick basaltic sand and/ or silt units at the base of the post-eruptive crater-filling sedimentary succession are interpreted to be reworked volcaniclastic material from the intra-maar scoria/spatter cones as well as from the tephra ring. Based on comparative analyses of 53 core descriptions, this study reveals that the original maar crater basin was larger than previously suggested. The deep level of the maar crater is reconstructed to be a northeast-southwest elongated depression, currently forming a c. 50-m-deep basin. Geomorphological considerations suggest that most of the phreatomagmatic pyroclastic rocks are composed of base surge and tephra fall deposits around the deep maar depression. These allochthonous rock units form a 50-400 m wide zone of proximal tuff-ring sequences. The formation of this zone is inferred to be a result of a combination of syneruptive subsidence due to mass deficit in the rigid Triassic dolomite basement caused by the phreatomagmatic explosions as well as post-eruptive subsidence of the crater- and diatreme-filling successions due to diagenetic compaction. The facies in the centre of the maar lake is a soft laminated "alginite" (mainly Botryococcus colonies, diatom frustles, calcium carbonate crystals, clay minerals). In the section exposed in the Pula open cast mine, a single turbiditic layer is present. This layer originated in a landslide, which possibly could have been caused by either syn-eruptive earthquake and/or a sudden posteruptive subsidence event of the diatreme fill. (c) 2008 Elsevier B.V. All rights reserved.2010truetruetruefalsefalseNONE2024-02-15false390392773635353235352323271203927392702727FolyóiratcikkJournal Article2436KönyvrészletChapter in Book253KönyvBook230Egyéb konferenciaközleményConference paper310Egyéb konferenciakötetConference proceedings320Oltalmi formákProtection forms260DisszertációThesis280EgyébMiscellaneous290AlkotásAchievement220Kutatási adatResearch data330FolyóiratcikkJournal Article24000KönyvrészletChapter in Book25000KönyvBook23000Egyéb konferenciaközleményConference paper31000Egyéb konferenciakötetConference proceedings32000Oltalmi formákProtection forms26000DisszertációThesis28000EgyébMiscellaneous29000AlkotásAchievement22000Kutatási adatResearch data33000200401111200500000200600000200700000200800000200903333201004040201104242201202121201301111201402121201505555201601111201701010201800000201902222202003131202106565202203333202301111Q1Afalsefalsefalsefalse2013-05-24T18:18:00.000+00002013-02-23T19:18:00.000+0000213050true10003133Language10002
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10015050"> <a href="/gui2/?type=authors&mode=browse&sel=10015050" target="_blank">Nemeth, K</a> </span> <span class="author-type"> </span> ; <span class="author-name" > Goth, K </span> <span class="author-type"> </span> ; <span class="author-name" > Martin, U </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10012053"> <a href="/gui2/?type=authors&mode=browse&sel=10012053" target="_blank">Csillag, G</a> </span> <span class="author-type"> </span> ; <span class="author-name" > Suhr, P </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;1384529" mtid="1384529" target="_blank">Reconstructing paleoenvironment, eruption mechanism and paleomorphology of the Pliocene Pula maar, (Hungary)</a></div> <div class="pub-info"> <span class="journal-title">JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH</span> <span class="journal-volume">177</span> : <span class="journal-issue">2</span> <span class="page"> pp. 441-456. , 16 p. </span> <span class="year">(2008)</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="10.1016/j.jvolgeores.2008.06.010" target="_blank" href="https://doi.org/10.1016/j.jvolgeores.2008.06.010"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000261120000011" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000261120000011"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="54049105640" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-54049105640"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="deleted-record">Zárolt</span> <span class="short-pub-mtid"> Közlemény:1384529 </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: 39</span> | Független: 27 | Függő: 12 | Nem jelölt: 0 | WoS jelölt: 35 | Scopus jelölt: 32 | WoS/Scopus jelölt: 35 | DOI jelölt: 35 </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="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> ; <span class="author-name" >Goth K </span> ; <span class="author-name" >Martin U </span> ; <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> ; <span class="author-name" >Suhr P </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse¶ms=publication;1384529" target="_blank">Reconstructing paleoenvironment, eruption mechanism and paleomorphology of the Pliocene Pula maar, (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">177</span> <span class="journal-issue">2</span> <span class="page"> pp 441-456 </span> <span class="year">(2008)</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.2008.06.010" target="_blank" href="https://doi.org/10.1016/j.jvolgeores.2008.06.010"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000261120000011" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000261120000011"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="54049105640" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-54049105640"> 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: 39</span> | Független: 27 | Függő: 12 | Nem jelölt: 0 | WoS jelölt: 35 | Scopus jelölt: 32 | WoS/Scopus jelölt: 35 | DOI jelölt: 35 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;1384529&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 27 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 1384529</span> | <span class="status-data status-ADMIN_APPROVED"> Admin láttamozott </span> <span class="oldId">Régi azonosító: 1384529</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: 2022.03.09. 13:19 Boros Annamária (MTMT Központi admin) </div> <div class="lockedBy">Ideiglenesen zárolva 2022.03.22. 19:24 Boros Annamária (MTMT Központi admin) </div> </div></div>