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Article: Bay of Islands and Little Port complexes, revisited: age, geochemical and isotopic evidence confirm suprasubduction-zone origin

TitleBay of Islands and Little Port complexes, revisited: age, geochemical and isotopic evidence confirm suprasubduction-zone origin
Authors
Issue Date1991
PublisherN R C Research Press. The Journal's web site is located at http://www.nrc.ca/cgi-bin/cisti/journals/rp/rp2_desc_e?cjes
Citation
Canadian Journal Of Earth Sciences, 1991, v. 28 n. 10, p. 1635-1652 How to Cite?
AbstractThe Bay of Islands Complex of the Humber Arm allochthon, west Newfoundland, contains the best-exposed ophiolite in the Appalachian Orogen. Associated structural slices, the Little Port and Skinner Cove complexes, also contain rocks formed in an oceanic domain, although their relationship to the Bay of Islands Complex remains controversial. To constrain the origin of the complexes and obtain a better understanding of the geology of the Humber Arm allochthon, we have undertaken an integrated geochronological, geochemical, and isotopic study. An alternative model to explain the relationships between the two complexes interprets the Little Port as arc-related and the Bay of Islands as a suprasubduction-zone ophiolite. -from Authors
Persistent Identifierhttp://hdl.handle.net/10722/178182
ISSN
2015 Impact Factor: 1.19
2015 SCImago Journal Rankings: 0.811

 

DC FieldValueLanguage
dc.contributor.authorJenner, GAen_US
dc.contributor.authorDunning, GRen_US
dc.contributor.authorMalpas, Jen_US
dc.contributor.authorBrown, Men_US
dc.contributor.authorBrace, Ten_US
dc.date.accessioned2012-12-19T09:43:17Z-
dc.date.available2012-12-19T09:43:17Z-
dc.date.issued1991en_US
dc.identifier.citationCanadian Journal Of Earth Sciences, 1991, v. 28 n. 10, p. 1635-1652en_US
dc.identifier.issn0008-4077en_US
dc.identifier.urihttp://hdl.handle.net/10722/178182-
dc.description.abstractThe Bay of Islands Complex of the Humber Arm allochthon, west Newfoundland, contains the best-exposed ophiolite in the Appalachian Orogen. Associated structural slices, the Little Port and Skinner Cove complexes, also contain rocks formed in an oceanic domain, although their relationship to the Bay of Islands Complex remains controversial. To constrain the origin of the complexes and obtain a better understanding of the geology of the Humber Arm allochthon, we have undertaken an integrated geochronological, geochemical, and isotopic study. An alternative model to explain the relationships between the two complexes interprets the Little Port as arc-related and the Bay of Islands as a suprasubduction-zone ophiolite. -from Authorsen_US
dc.languageengen_US
dc.publisherN R C Research Press. The Journal's web site is located at http://www.nrc.ca/cgi-bin/cisti/journals/rp/rp2_desc_e?cjesen_US
dc.relation.ispartofCanadian Journal of Earth Sciencesen_US
dc.titleBay of Islands and Little Port complexes, revisited: age, geochemical and isotopic evidence confirm suprasubduction-zone originen_US
dc.typeArticleen_US
dc.identifier.emailMalpas, J: jgmalpas@hku.hken_US
dc.identifier.authorityMalpas, J=rp00059en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0026268642en_US
dc.identifier.volume28en_US
dc.identifier.issue10en_US
dc.identifier.spage1635en_US
dc.identifier.epage1652en_US
dc.publisher.placeCanadaen_US
dc.identifier.scopusauthoridJenner, GA=7006027534en_US
dc.identifier.scopusauthoridDunning, GR=7006724186en_US
dc.identifier.scopusauthoridMalpas, J=7006136845en_US
dc.identifier.scopusauthoridBrown, M=7405388149en_US
dc.identifier.scopusauthoridBrace, T=6508064224en_US

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