Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.

Detalhes bibliográficos
Autor(a) principal: Batiza, Rodey
Data de Publicação: 1982
Outros Autores: O'Hearn, T.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10400.3/4898
Resumo: International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.
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spelling Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.GeochemistryPetrologyVolcanismInternational Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.Major element electron microprobe analyses of over 100 dredged samples of basalt glass from the East Pacific Rise and nine young isolated seamounts near the Rise are presented along with petrographic data for the samples. These data indicate that most suites of samples from seamounts are fractionated suites of low-K₂O mid-ocean ridge basalt similar to many described previously. In addition, however, some seamount lavas differentiate toward higher K₂O, TiO₂ and other incompatible element enrichment without correlation with Mg/Fe ratios. These two types of chemical abundance variation trends do not correlate well with size, age or tectonic settings of the seamounts, however, the absolute amount of chemical diversity observed in the lavas of each seamount does correlate with these other variables. The data indicate that location on fracture zones is neither a necessary or sufficient condition for great chemical diversity of seamount lavas, however, seamounts on fracture zones tend to be large in size. On the other hand, relatively great age (> 3.0 m.y.) and great size (> 200 km³) are sufficient but not necessary conditions for such seamount lava diversity. These patterns may be interpreted in terms of the evolution of young oceanic central volcanoes.Universidade dos AçoresRepositório da Universidade dos AçoresBatiza, RodeyO'Hearn, T.2018-11-28T13:29:52Z1982-071982-07-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10400.3/4898engBATIZA, Rodey; O’HEARN, T. (1982). Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N. "Arquipélago. Série Ciências da Natureza", 3: 201-230.info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2022-12-20T14:33:09Zoai:repositorio.uac.pt:10400.3/4898Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T16:27:13.445183Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.
title Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.
spellingShingle Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.
Batiza, Rodey
Geochemistry
Petrology
Volcanism
title_short Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.
title_full Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.
title_fullStr Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.
title_full_unstemmed Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.
title_sort Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.
author Batiza, Rodey
author_facet Batiza, Rodey
O'Hearn, T.
author_role author
author2 O'Hearn, T.
author2_role author
dc.contributor.none.fl_str_mv Repositório da Universidade dos Açores
dc.contributor.author.fl_str_mv Batiza, Rodey
O'Hearn, T.
dc.subject.por.fl_str_mv Geochemistry
Petrology
Volcanism
topic Geochemistry
Petrology
Volcanism
description International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.
publishDate 1982
dc.date.none.fl_str_mv 1982-07
1982-07-01T00:00:00Z
2018-11-28T13:29:52Z
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dc.identifier.uri.fl_str_mv http://hdl.handle.net/10400.3/4898
url http://hdl.handle.net/10400.3/4898
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv BATIZA, Rodey; O’HEARN, T. (1982). Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N. "Arquipélago. Série Ciências da Natureza", 3: 201-230.
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dc.publisher.none.fl_str_mv Universidade dos Açores
publisher.none.fl_str_mv Universidade dos Açores
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