https://m2.mtmt.hu/ hun 2026-09-22 09:34 JournalArticle 31976833 ADMIN_APPROVED true Összes idézések száma a WoS-ban: 0 cited By 1 Núcleo de Investigación en Riesgo Volcánico-Ckelar Volcanes, Universidad Católica del Norte, Av. Angamos 0610, Antofagasta, 1270709, Chile Programa de Doctorado en Ciencias Mención Geología, Universidad Católica del Norte, Av. Angamos 0610, Antofagasta, 1270709, Chile Centro Nacional de Investigación para la Gestión Integrada del Riesgo de Desastres (CIGIDEN), Av. Vicuña Mackenna 4860, Santiago, 7820436, Chile Volcanic Risk Solutions, School of Agriculture and Environment, Massey University, Palmerston North, 4442, New Zealand Departamento de Ciencias Geológicas, Universidad Católica del Norte, Av. Angamos 0610, Antofagasta, 1270709, Chile Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, Potsdam, 14473, Germany Bruker Nano GmbH, Am Studio 2D, Berlin, 12489, Germany Cited By :1 Export Date: 25 May 2021 Correspondence Address: Ureta, G.; Centro Nacional de Investigación para la Gestión Integrada del Riesgo de Desastres (CIGIDEN), Av. Vicuña Mackenna 4860, Chile; email: gabriel.ureta@ucn.cl Núcleo de Investigación en Riesgo Volcánico-Ckelar Volcanes, Universidad Católica del Norte, Av. Angamos 0610, Antofagasta, 1270709, Chile Programa de Doctorado en Ciencias Mención Geología, Universidad Católica del Norte, Av. Angamos 0610, Antofagasta, 1270709, Chile Centro Nacional de Investigación para la Gestión Integrada del Riesgo de Desastres (CIGIDEN), Av. Vicuña Mackenna 4860, Santiago, 7820436, Chile Volcanic Risk Solutions, School of Agriculture and Environment, Massey University, Palmerston North, 4442, New Zealand Departamento de Ciencias Geológicas, Universidad Católica del Norte, Av. Angamos 0610, Antofagasta, 1270709, Chile Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, Potsdam, 14473, Germany Bruker Nano GmbH, Am Studio 2D, Berlin, 12489, Germany Cited By :1 Export Date: 26 May 2021 Correspondence Address: Ureta, G.; Centro Nacional de Investigación para la Gestión Integrada del Riesgo de Desastres (CIGIDEN), Av. Vicuña Mackenna 4860, Chile; email: gabriel.ureta@ucn.cl Funding Agency and Grant Number: CONICYT-PCHA Doctorado Nacional fellowship [2016-21161286]; Universidad Catolica del Norte; Antofagasta Regional Government, FIC-R project [30488832-0]; CONICYT-PAI MECGerman Research Foundation (DFG)National Health and Medical Research Council of Australia [2017-80170048]; Massey University Funding text: This study is part of G.U. Ph.D. thesis, which is funded by CONICYT-PCHA Doctorado Nacional 2016-21161286 fellowship and supported by the Universidad Catolica del Norte. This research was funded by the Antofagasta Regional Government, FIC-R project, code BIP N degrees 30488832-0 and by CONICYT-PAI MEC 2017-80170048; based on theMemorandum of Understanding of Research Cooperation between Universidad Catolica del Norte and Massey University. 0 false 2026-05-31T08:45:05.788+0000 2022-03-03T17:14:32.389+0000 2021-04-21T03:54:31.585+0000 true 10015050 Németh Károly /api/author/10015050 Author true 10015050 2026-04-17T14:20:26.733+0000 2026-04-17T14:20:26.733+0000 2022-03-03T17:14:32.399+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 Ureta, Gabriel A window on mantle-derived magmas within the Central Andes: eruption style transitions at Cerro Overo maar and La Albondiga lava dome, northern Chile true true /api/journal/645 REVIEWED true false 645 false 645 true 0258-8900 1432-0819 Journal FOREIGN 83 4 19 19 22 2021 Cerro Overo maar and La Albondiga lava dome are two independent monogenetic volcanoes located in the Central Volcanic Zone of the Andes in northern Chile, close to the active Lascar and Chiliques volcanoes. Cerro Overo maar was formed <77 ka ago by explosive-effusive eruptions, including phreatomagmatic activity, while La Albondiga lava dome (Pleistocene) is the result of magmatic explosive-effusive activity alone. Cerro Overo and La Albondiga are characterized by deposits composed of pyroclastic rocks and dense coherent lava blocks. At Cerro Overo, these deposits are located around the crater rim, while at La Albondiga, they form coherent in situ lava dome features. Cerro Overo also displays thin ash- and lapilli-dominated deposit layers presumed to be pyroclastic surge deposits, which include juvenile pyroclasts exhibiting cauliflower textures, numerous exotic accidental lithics, and ballistically transported lapilli, bombs, blocks, and bomb sags. These fragments include recycled, juvenile pyroclasts, as well as material from older volcanic and intrusive rocks from the stratigraphic units immediately below. These small-volume volcanoes represent two of the less silicic volcanoes (similar to 54 wt.% SiO2) in the northern Chilean Pleistocene to Holocene volcanic provinces. They are characterized by a fine grain size (mainly fine lapilli), olivine phenocrysts with skeletal textures, ignimbritic, dioritic, and granitic xenoliths, and quartz xenocrysts, with high concentrations of incompatible trace elements and light rare earth elements. The general magmatic evolution of the Cerro Overo and La Albondiga systems has been controlled by fast ascent (e.g., skeletal olivine phenocrysts) of mantle-derived magma associated with mixing, fractional crystallization, and a low degree of crustal assimilation during turbulent ascent processes. Such eruptions provide evidence that various factors play an essential role in the transition from explosive-effusive magmatic (Cerro Overo and La Albondiga) to phreatomagmatic (Cerro Overo) volcanic eruption styles. 2021 true true true false false NONE 2026-05-31 false 14 1 14 8 3 14 14 12 9 13 13 8 8 8 6 0 14 8 14 8 0 11 11 Folyóiratcikk Journal Article 24 14 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 2021 0 1 0 1 0 2022 0 4 2 4 2 2023 0 3 2 3 2 2024 0 2 1 2 1 2025 0 3 2 3 2 2026 0 1 1 1 1 Q2 A false 10015050 false false false 2021-05-24T09:45:23.016+0000 1 2 0 5 0 true 10003133 Language 10002 /api/language/10002 Angol English true 2 true PersonAuthorship 96038800 /api/authorship/96038800 1 0.2 true false false Ureta Gabriel true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 96038801 /api/authorship/96038801 2 0.2 false false Author 10015050 /api/author/10015050 Németh Károly true 10015050 true Nemeth Karoly true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 96038802 /api/authorship/96038802 3 0.2 false false false Aguilera Felipe true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 96038803 /api/authorship/96038803 4 0.2 false false false Zimmer Martin true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PersonAuthorship 96038804 /api/authorship/96038804 5 0.2 false true false Menzies Andrew true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false true PublicationIdentifier 18686431 /api/publicationidentifier/18686431 PlainSource 6 /api/publicationsource/6 PublicationSourceType 10001 /api/publicationsourcetype/10001 true true true DOI DOI https://doi.org/@@@ true true 6 true IDENTICAL 10.1007/s00445-021-01446-3 https://doi.org/10.1007/s00445-021-01446-3 false true PublicationIdentifier 18686432 /api/publicationidentifier/18686432 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 000625784700001 https://www.webofscience.com/wos/woscc/full-record/000625784700001 false true PublicationIdentifier 18708830 /api/publicationidentifier/18708830 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 85102176297 http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85102176297 false true MtaRating 11435021 /api/mtarating/11435021 RatingType 10031 /api/ratingtype/10031 X. 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Földtudományok Osztálya HAS Section of Earth Sciences (X.) true 70 true true true A true true SjrRating 11208473 /api/sjrrating/11208473 40 0.49 journal RatingType 10002 /api/ratingtype/10002 sjr true true ClassificationExternal 1906 /api/classificationexternal/1906 true 1906 true Q2 DIRECT true true /api/publication/31976833 <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" >Ureta Gabriel </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10015050"><a href="/gui2/?type=authors&mode=browse&sel=10015050" target="_blank">Nemeth Karoly (<span class="authorship-author-name">Németh Károly</span> <span class="authorAux-mtmt"> Vulkanológia, szedimentológia</span>) </a> </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Aguilera Felipe </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Zimmer Martin </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Menzies Andrew </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;31976833" target="_blank">A window on mantle-derived magmas within the Central Andes: eruption style transitions at Cerro Overo maar and La Albondiga lava dome, northern Chile</a></div> <div> <span class="journal-title">BULLETIN OF VOLCANOLOGY</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0258-8900">0258-8900</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1432-0819">1432-0819</a>)</span>: <span class="journal-volume">83</span> <span class="journal-issue">4</span> <span class="page"> Paper 19. 22 p. </span> <span class="year">(2021)</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="10.1007/s00445-021-01446-3" target="_blank" href="https://doi.org/10.1007/s00445-021-01446-3"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000625784700001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000625784700001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85102176297" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85102176297"> Scopus </a> </span> </span> <OnlyViewableByAuthor><div class="ratings"> <div class="journal-subject">Folyóirat szakterülete: Scopus - Geochemistry and Petrology&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;Q2</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: 14</span> | Független: 8 | Függő: 6 | Nem jelölt: 0 | WoS jelölt: 12 | Scopus jelölt:&nbsp;9 | WoS/Scopus jelölt:&nbsp;13 | DOI jelölt:&nbsp;14 (Nem nyilvános:&nbsp;1) </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;31976833&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 11 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 31976833</span> | <span class="status-data status-ADMIN_APPROVED"> Admin láttamozott </span> Forrás Idéző | <span class="type-subtype">Folyóiratcikk ( Szakcikk ) </span> | <span class="pub-category">Tudományos</span> | <span class="publication-sourceOfData">WOS TAGGED</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> <pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Összes idézések száma a WoS-ban: 0 cited By 1 Núcleo de Investigación en Riesgo Volcánico-Ckelar Volcanes, Universidad Católica del Norte, Av. Angamos 0610, Antofagasta, 1270709, Chile Programa de Doctorado en Ciencias Mención Geología, Universidad Católica del Norte, Av. Angamos 0610, Antofagasta, 1270709, Chile Centro Nacional de Investigación p...</pre> </div></div>