Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/44217
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dc.contributor.authorHimi, M.en_US
dc.contributor.authorRodriguez-Gonzalez, A.en_US
dc.contributor.authorTapias, J. C.en_US
dc.contributor.authorPerez-Torrado, F.en_US
dc.contributor.authorCasas, A.en_US
dc.date.accessioned2018-11-21T21:07:53Z-
dc.date.available2018-11-21T21:07:53Z-
dc.date.issued2015en_US
dc.identifier.isbn9781510814127-
dc.identifier.urihttp://hdl.handle.net/10553/44217-
dc.description.abstractMaar are a singular type of volcanic structure generated by explosive phreatomagmatic eruptions as a result of interaction between rising magma and groundwater. This kind of structures are characterised by circular craters, often filled with water and/or lacustrine sediments and surrounded by a ring of pyroclastic deposits. The whole of the volcano, including the pyroclastic ring surrounding the crater maar is called maar-diatreme. Recently borehole was drilled at the bottom of the volcanic crater which penetrated about 8.7 m in its sedimentary sequence and the paleobotanical study has supplied the first evidence of paleoenvironmental evolution during the Holocene on the Gran Canaria Island. The possibility of its sedimentary fill extends beyond of the Holocene is extremely attractive, since, for example, and there are few paleoenvironmental data regarding how much the last glaciation that affected the Canary Islands. In these circumstances, the knowledge of the total thickness of the lacustrine sediments is crucial to design a deeper borehole in the next future. Therefore, the subsurface characterisation provided by geophysics is essential for determining thickness and geometry of the sedimentary filling.en_US
dc.languageengen_US
dc.relation.ispartofNear Surface Geoscience 2015 - 21st European Meeting of Environmental and Engineering Geophysicsen_US
dc.sourceNear Surface Geoscience 2015 - 21st European Meeting of Environmental and Engineering Geophysics, p. 401-405en_US
dc.subject250621 Vulcanologíaen_US
dc.subject.otherERTen_US
dc.subject.otherLa Calderilla volcanic calderaen_US
dc.subject.otherGran Canaria islanden_US
dc.titleERT characterisation of la calderilla volcanic caldera (Gran Canaria Island, Spain)en_US
dc.typeinfo:eu-repo/semantics/conferenceObjectes
dc.typeConferenceObjectes
dc.relation.conference21st European Meeting of Environmental and Engineering Geophysics, Near Surface Geoscience 2015
dc.identifier.doi10.3997/2214-4609.201413744-
dc.identifier.scopus84958073308-
dc.contributor.authorscopusid23034244800-
dc.contributor.authorscopusid25959720400-
dc.contributor.authorscopusid35612596700-
dc.contributor.authorscopusid57202615546-
dc.contributor.authorscopusid6602207526
dc.contributor.authorscopusid8676295200-
dc.contributor.authorscopusid37042205700
dc.description.lastpage405-
dc.description.firstpage401-
dc.investigacionCienciasen_US
dc.type2Actas de congresosen_US
dc.date.coverdateEnero 2015
dc.identifier.conferenceidevents121572
dc.identifier.ulpgces
item.fulltextSin texto completo-
item.grantfulltextnone-
crisitem.event.eventsstartdate06-09-2015-
crisitem.event.eventsenddate10-09-2015-
crisitem.author.deptGIR IUNAT: Geología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR IUNAT: Geología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0003-0688-0531-
crisitem.author.orcid0000-0002-4644-0875-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.fullNameRodríguez González, Alejandro-
crisitem.author.fullNamePérez Torrado, Francisco José-
Appears in Collections:Actas de congresos
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