Major element chemistry of basalt glasses dredged from young isolated volcanoes and the East Pacific rise, 10˚~14˚ N.
Autor(a) principal: | |
---|---|
Data de Publicação: | 1982 |
Outros Autores: | |
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. |
id |
RCAP_4ca0882bfcedfbdc0dfcfd65fecec5f0 |
---|---|
oai_identifier_str |
oai:repositorio.uac.pt:10400.3/4898 |
network_acronym_str |
RCAP |
network_name_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository_id_str |
7160 |
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 |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
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. |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade dos Açores |
publisher.none.fl_str_mv |
Universidade dos Açores |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
instname_str |
Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
instacron_str |
RCAAP |
institution |
RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
repository.mail.fl_str_mv |
|
_version_ |
1799130727203209216 |