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Submarine volcanoes East and South of Izu Peninsula, Central Japan

dc.contributor.authorAramaki, Shigeo
dc.date.accessioned2018-11-28T11:38:58Z
dc.date.available2018-11-28T11:38:58Z
dc.date.issued1982-07
dc.descriptionInternational Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.en
dc.description.abstractMore than 50 volcanic centers are recognized as positive topography on the sea floor east and south of Izu Peninsula. Most of them are probably late Quaternary basaltic cones resting on the basement of Miocene submarine volcanic rocks. Recent dredge hauls have revealed that those submarine volcanoes located close to Izu Peninsula belong to the high-Al and/or high alkali basalts while those further south are either low alkali tholeiites or calk-alaki rhyolites associated with high-Al basalts. Submarine volcanoes dose to Izu Peninsula are contemporaneous with a group of basaltic (and minor rhyolitic) monogenetic volcanic centers clustered in the central Izu Peninsula, which were active during the last 100,000 years. […].en
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationARAMAKI, Shigeo (1982). Submarine volcanoes East and South of Izu Peninsula, Central Japan. "Arquipélago. Série Ciências da Natureza", 3: 253-254.pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.3/4892
dc.language.isoengpt_PT
dc.publisherUniversidade dos Açorespt_PT
dc.subjectVolcanismen
dc.subjectIzu Peninsulaen
dc.subjectJapanen
dc.titleSubmarine volcanoes East and South of Izu Peninsula, Central Japanen
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlacePonta Delgada, Açorespt_PT
oaire.citation.endPage254pt_PT
oaire.citation.startPage253pt_PT
oaire.citation.titleArquipélago. Série Ciências da Naturezapt_PT
oaire.citation.volume3pt_PT
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT

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