https://m2.mtmt.hu/ hun 2026-03-14 00:53 JournalArticle 1506098 ADMIN_APPROVED true Megjegyzés-21630189 : FN Thomson Reuters Web of Knowledge WC: Geosciences, Multidisciplinary Összes idézések száma a WoS-ban: 0 0 2014-10-16T11:08:33.000+0000 false 1506098 2025-12-20T23:46:45.850+0000 2022-03-04T18:45:17.398+0000 2011-04-22T21:40:09.000+0000 true 10015050 Németh Károly /api/author/10015050 Author Németh Károly (Vulkanológia, szedimentológia) true 10015050 2022-03-16T13:05:49.637+0000 2022-03-16T13:05:49.637+0000 2022-03-04T18:45:17.410+0000 true 10003133 Boros Annamária /api/admin/10003133 Admin Boros Annamária (MTMT Központi admin) true 10003133 Admin 10003133 /api/admin/10003133 Boros Annamária (MTMT Központi admin) Boros Annamária true 10003133 true 2022-03-22T18:24:48.781+0000 true false true 24 24 /api/publicationtype/24 PublicationType Folyóiratcikk 1 true 24 JournalArticle true 10000059 Article true 24 24 /api/publicationtype/24 PublicationType Folyóiratcikk 1 true 24 JournalArticle /api/subtype/10000059 Szakcikk SubType Szakcikk (Folyóiratcikk) 101 true 10000059 true 1 /api/category/1 Category Tudományos true 1 Geshi, N true true /api/journal/2944 REVIEWED JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH 0377-0273 1872-6097 true false 2944 false 2944 true 0377-0273 1872-6097 Journal FOREIGN 201 1-4 30 38 30 9 2011 A subvertical cross section of a maar-diatreme volcano is exposed in the wall of the A.D. 2000 caldera on Miyakejima Volcano. The maar, Suoana, is one of the lateral vents of this volcano and it was inferred to be formed in the 7th century. The subvertical wall of the A.D. 2000 caldera truncated the Suoana maar crater at its center revealing the near comlete cross section of this small maar-diatreme volcano. Exposed in the cross section are a 400. m wide maar crater, an associated tuff ring with a maximum thickness of 20. m, a diatreme extending vertically to a depth of about 220. m from the floor of the maar crater, and a feeder dike connected to the base of the diatreme. The depth of the diatreme structure is about 260. m from the original ground surface. The outline of the diatreme resembles an upward-opening funnel with an almost vertical wall below 560. m asl and an upward flaring wall above 560. m asl. Coarse grained volcanic breccia fills the diatreme, the deposits of which can be divided into 6 units based on lithological and structural characteristics. The upper half of the diatreme is filled with landslide deposits, mainly derived from the surrounding crater wall. The bottom of the diatreme is occupied by massive explosion breccia. Some coherent blocks were detached from the wall of the diatreme and preserved in the diatreme fill. The Y-shaped cross-sectional geometry of the Suoana diatreme is the result of a combination of an underground subsidence in the lower part of the diatreme and the surface landslide in its upper part. The inwardly-inclined stratification of pyroclastic rock units and development of many small faults in the diatreme-filling breccia indicate successive collapse and deformation of these materials within the diatreme during the eruption. The upper part of the diatreme was formed by the landslides of the crater wall induced by the subsidence of the crater floor. Discharge of tephra from the bottom of the diatreme caused infill subsidence, which induced sliding of the inner wall of the crater. As a result, the topographic diameter of the crater became much larger than that of the diatreme itself. The tephra ring surrounding the crater consists mainly of pyroclastic fall deposits. © 2010 Elsevier B.V. 2011 true true true false false NONE 2025-12-21 false 49 0 49 43 0 48 49 44 28 44 44 38 38 43 6 0 49 43 49 43 0 4 4 Folyóiratcikk Journal Article 24 45 Könyvrészlet Chapter in Book 25 4 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 2012 0 1 1 1 1 2013 0 2 2 2 2 2014 0 6 5 6 5 2015 0 8 6 8 6 2016 0 4 4 4 4 2017 0 5 4 5 4 2018 0 3 3 3 3 2019 0 2 1 2 1 2020 0 3 2 3 2 2021 0 2 2 2 2 2022 0 4 4 4 4 2023 0 1 1 1 1 2024 0 5 5 5 5 2025 0 3 3 3 3 Q1 A false false false false 2013-01-03T01:23:32.000+0000 2012-10-05T00:23:32.000+0000 1 2 0 3 0 true 10003133 Language 10002 /api/language/10002 Angol Angol English true 2 true PersonAuthorship 1561786 /api/authorship/1561786 Geshi, N 1 0.33333334 true false Geshi N true false false AuthorshipType 1 /api/authorshiptype/1 Szerző 0 true 0 true false 12230664 true PersonAuthorship 1561787 /api/authorship/1561787 Németh, K [Németh, Károly (Vulkanológia, sze...), szerző] 2 0.33333334 false false Author 10015050 /api/author/10015050 Németh Károly (Vulkanológia, szedimentológia) Németh Károly true 10015050 true Németh K true false false AuthorshipType 1 /api/authorshiptype/1 Szerző 0 true 0 true false 12230663 true PersonAuthorship 1561788 /api/authorship/1561788 Oikawa, T 3 0.33333334 false true Oikawa T true false false AuthorshipType 1 /api/authorshiptype/1 Szerző 0 true 0 true false 12230662 true PublicationIdentifier 367768 /api/publicationidentifier/367768 DOI: 10.1016/j.jvolgeores.2010.11.012 PlainSource 6 /api/publicationsource/6 DOI PublicationSourceType 10001 /api/publicationsourcetype/10001 DOI true true true DOI DOI https://doi.org/@@@ true true 6 true false IDENTICAL 10.1016/j.jvolgeores.2010.11.012 https://doi.org/10.1016/j.jvolgeores.2010.11.012 false 211714 true PublicationIdentifier 367766 /api/publicationidentifier/367766 WoS: 000289963900003 PlainSource 1 /api/publicationsource/1 WoS PublicationSourceType 10003 /api/publicationsourcetype/10003 Indexelő adatbázis false true true WoS WoS https://www.webofscience.com/wos/woscc/full-record/@@@ true true 1 true false IDENTICAL 000289963900003 https://www.webofscience.com/wos/woscc/full-record/000289963900003 false 211715 true PublicationIdentifier 367767 /api/publicationidentifier/367767 Scopus: 79953045902 PlainSource 3 /api/publicationsource/3 Scopus PublicationSourceType 10003 /api/publicationsourcetype/10003 Indexelő adatbázis false true true Scopus Scopus http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-@@@ true true 3 true false NO 79953045902 http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-79953045902 false 211716 true Classification 10399 /api/classification/10399 Föld- és kapcsolódó környezettudományok true true Keyword 1002891 /api/keyword/1002891 MAAR true 1002891 true Keyword 1002941 /api/keyword/1002941 diatreme true 1002941 true Keyword 1002984 /api/keyword/1002984 phreatomagmatic eruption true 1002984 true Keyword 1003033 /api/keyword/1003033 volcano true 1003033 true Keyword 1048394 /api/keyword/1048394 Miyakejima true 1048394 true MtaRating 11435122 /api/mtarating/11435122 X. Földtudományok Osztálya:A JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH 0377-0273 1872-6097 RatingType 10031 /api/ratingtype/10031 X. Földtudományok Osztálya X. FTO Institute 70 /api/institute/70 X. Földtudományok Osztálya XFO 0 false false false X. Földtudományok Osztálya HAS Section of Earth Sciences (X.) true 70 true true true A true true SjrRating 5699230 /api/sjrrating/5699230 sjr:Q1 (2011) Scopus - Geochemistry and Petrology JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH 0377-0273 1872-6097 19 0.24 journal RatingType 10002 /api/ratingtype/10002 sjr sjr true true ClassificationExternal 1906 /api/classificationexternal/1906 Scopus - Geochemistry and Petrology true 1906 true Q1 DIRECT true 5699230 true Reference 1254355 /api/reference/1254355 1. Acocella, V., Understanding caldera structure and development: an overview of analogue models compared to natural calderas (2007) Earth Sci. Rev., 85, pp. 125-160 1 false true Reference 1254356 /api/reference/1254356 2. 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Growth of phreatomagmatic explosion craters: A model inferred from Suoana crater in Miyakejima Volcano, Japan. (2011) JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH 0377-0273 1872-6097 201 1-4 30-38<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" >Geshi N </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10015050"><a href="/gui2/?type=authors&mode=browse&sel=10015050" target="_blank">Németh K (<span class="authorship-author-name">Németh Károly</span> <span class="authorAux-mtmt"> Vulkanológia, szedimentológia</span>) </a> </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Oikawa T </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;1506098" target="_blank">Growth of phreatomagmatic explosion craters: A model inferred from Suoana crater in Miyakejima Volcano, Japan</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 30-38 </span> <span class="year">(2011)</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.2010.11.012" target="_blank" href="https://doi.org/10.1016/j.jvolgeores.2010.11.012"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000289963900003" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000289963900003"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="79953045902" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-79953045902"> 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: 49</span> | Független: 43 | Függő: 6 | Nem jelölt: 0 | WoS jelölt: 44 | Scopus jelölt:&nbsp;28 | WoS/Scopus jelölt:&nbsp;44 | DOI jelölt:&nbsp;49 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;1506098&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 4 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 1506098</span> | <span class="status-data status-ADMIN_APPROVED"> Admin láttamozott </span> <span class="oldId">Régi azonosító: 1506098</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: 2022.03.04. 19:45 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>: Megjegyzés-21630189 : FN Thomson Reuters Web of Knowledge WC: Geosciences, Multidisciplinary Összes idézések száma a WoS-ban: 0</pre> </div></div>