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Article: Bay of Islands and Little Port complexes, revisited: age, geochemical and isotopic evidence confirm suprasubduction-zone origin
Title | Bay of Islands and Little Port complexes, revisited: age, geochemical and isotopic evidence confirm suprasubduction-zone origin |
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Authors | |
Issue Date | 1991 |
Publisher | N 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? |
Abstract | The 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 Identifier | http://hdl.handle.net/10722/178182 |
ISSN | 2023 Impact Factor: 1.3 2023 SCImago Journal Rankings: 0.460 |
ISI Accession Number ID |
DC Field | Value | Language |
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dc.contributor.author | Jenner, GA | en_US |
dc.contributor.author | Dunning, GR | en_US |
dc.contributor.author | Malpas, J | en_US |
dc.contributor.author | Brown, M | en_US |
dc.contributor.author | Brace, T | en_US |
dc.date.accessioned | 2012-12-19T09:43:17Z | - |
dc.date.available | 2012-12-19T09:43:17Z | - |
dc.date.issued | 1991 | en_US |
dc.identifier.citation | Canadian Journal Of Earth Sciences, 1991, v. 28 n. 10, p. 1635-1652 | en_US |
dc.identifier.issn | 0008-4077 | en_US |
dc.identifier.uri | http://hdl.handle.net/10722/178182 | - |
dc.description.abstract | The 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 | en_US |
dc.language | eng | en_US |
dc.publisher | N 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 | en_US |
dc.relation.ispartof | Canadian Journal of Earth Sciences | en_US |
dc.title | Bay of Islands and Little Port complexes, revisited: age, geochemical and isotopic evidence confirm suprasubduction-zone origin | en_US |
dc.type | Article | en_US |
dc.identifier.email | Malpas, J: jgmalpas@hku.hk | en_US |
dc.identifier.authority | Malpas, J=rp00059 | en_US |
dc.description.nature | link_to_subscribed_fulltext | en_US |
dc.identifier.scopus | eid_2-s2.0-0026268642 | en_US |
dc.identifier.volume | 28 | en_US |
dc.identifier.issue | 10 | en_US |
dc.identifier.spage | 1635 | en_US |
dc.identifier.epage | 1652 | en_US |
dc.identifier.isi | WOS:A1991GV40000012 | - |
dc.publisher.place | Canada | en_US |
dc.identifier.scopusauthorid | Jenner, GA=7006027534 | en_US |
dc.identifier.scopusauthorid | Dunning, GR=7006724186 | en_US |
dc.identifier.scopusauthorid | Malpas, J=7006136845 | en_US |
dc.identifier.scopusauthorid | Brown, M=7405388149 | en_US |
dc.identifier.scopusauthorid | Brace, T=6508064224 | en_US |
dc.identifier.issnl | 0008-4077 | - |