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Interpretation of ground deformation in the Azores

dc.contributor.authorMachado, Frederico
dc.date.accessioned2018-11-30T11:38:59Z
dc.date.available2018-11-30T11:38:59Z
dc.date.issued1982-07
dc.descriptionInternational Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.en
dc.description.abstractGeodetic measurements in Fayal, Pico and San Jorge showed some horizontal expansion of these islands. The total expansion during the interval 1936-1979 amounts to· several metres, being considerably greater than the average sea floor spreading for that area of the Atlantic Ocean. This suggests that the spreading could be a discontinuous phenomenon, depending on short lived epochs of quick strain release. A vertical pulsation on the central part of Pico volcano was also detected; the pulsation has amplitude of about one metre and period close to one year. Its-seems due to periodic changes of pressure inside the magma chamber.en
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationMACHADO, Frederico (1982). Interpretation of ground deformation in the Azores. "Arquipélago. Série Ciências da Natureza", 3: 95-112.pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.3/4914
dc.language.isoengpt_PT
dc.publisherUniversidade dos Açorespt_PT
dc.subjectGeodesyen
dc.subjectGeologyen
dc.subjectVolcanic Soilsen
dc.subjectAzores Archipelagoen
dc.titleInterpretation of ground deformation in the Azoresen
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlacePonta Delgada, Açorespt_PT
oaire.citation.endPage112pt_PT
oaire.citation.startPage95pt_PT
oaire.citation.titleArquipélago. Série Ciências da Naturezapt_PT
oaire.citation.volume3pt_PT
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT

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