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Cenozoic diatreme field in Chubut (Argentina) as evidence of phreatomagmatic volcanism accompanied with extensive Patagonian plateau basalt volcanism?
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In Patagonia, Argentina, at the northern border of the Patagonian Cenozoic mafic plateau lava fields, newly discovered diatremes stand about 100 m above the surrounding plain. These diatremes document phreatomagmatic episodes associated with the formation of the volcanic fields. The identified pyroclastic and intrusive rocks are exposed lower diatremes of former phreatomagmatic volcanoes and their feeding dyke systems. These remotely located erosional remnants cut through Paleozoic granitoids and Jurassic/Cretaceous alternating siliciclastic continental successions that are relatively easily eroded. Plateau lava fields are generally located a few hundreds of metres above the highest level of the present tops of the preserved diatremes suggesting a complex erosional history and potential interrelationships between the newly identified diatremes and the surrounding lava fields. Uprising magma from the underlying feeder dyke into the diatreme root zone intruded the clastic debris in the diatremes, inflated them and mingled with the debris to form subterranean peperite. The significance of identifying diatremes in Patagonia are twofold: 1) in the syn-eruptive paleoenvironment, water was available in various "soft-sediments ", commonly porous, media aquifer sources, and 2) the identified abundant diatremes that form diatreme fields are good source candidates for the extensive lava fields with phreatomagmatism facilitating magma rise with effective opening of fissures before major lava effusions.
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/api/publication/1384538
<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" > Martin, U </span> <span class="author-type"> </span> ; <span class="author-name" > Haller, MJ </span> <span class="author-type"> </span> ; <span class="author-name" > Alric, VL </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;1384538" mtid="1384538" target="_blank">Cenozoic diatreme field in Chubut (Argentina) as evidence of phreatomagmatic volcanism accompanied with extensive Patagonian plateau basalt volcanism?</a></div> <div class="pub-info"> <span class="journal-title">EPISODES</span> <span class="journal-volume">30</span> : <span class="journal-issue">3</span> <span class="page"> pp. 217-223. , 7 p. </span> <span class="year">(2007)</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="000250386300005" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000250386300005"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="35648956725" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-35648956725"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="deleted-record">Zárolt</span> <span class="short-pub-mtid"> Közlemény:1384538 </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: 16</span> | Független: 11 | Függő: 5 | Nem jelölt: 0 | WoS jelölt: 15 | Scopus jelölt: 11 | WoS/Scopus jelölt: 16 | DOI jelölt: 16 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<img title="Forrásközlemény" style="float: left" src="/frontend/resources/grid/publication-core-icon.png">
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<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>)
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</span>
;
<span class="author-name" >Martin U
</span>
;
<span class="author-name" >Haller MJ
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;
<span class="author-name" >Alric VL
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;1384538" target="_blank">Cenozoic diatreme field in Chubut (Argentina) as evidence of phreatomagmatic volcanism accompanied with extensive Patagonian plateau basalt volcanism?</a></div> <div> <span class="journal-title">EPISODES</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0705-3797">0705-3797</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/2586-1298">2586-1298</a>)</span>:
<span class="journal-volume">30</span> <span class="journal-issue">3</span>
<span class="page">
pp 217-223
</span> <span class="year">(2007)</span>
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<span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 16</span>
| Független: 11
| Függő: 5
| Nem jelölt: 0
| WoS jelölt: 15
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Idézett közlemények száma: 3
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<div class="mtid"><span class="long-pub-mtid">Közlemény: 1384538</span>
| <span class="status-data status-ADMIN_APPROVED"> Admin láttamozott
</span>
<span class="oldId">Régi azonosító: 1384538</span> |
Forrás Idéző
| <span class="type-subtype">Folyóiratcikk
( Szakcikk
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| <span class="pub-category">Tudományos</span>
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<div class="lastModified">Utolsó módosítás: 2022.03.03. 18:17 Boros Annamária (MTMT Központi admin)
</div>
<div class="lockedBy">Ideiglenesen zárolva 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</pre>
</div></div>