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Article: DYNAMOTHERMAL AUREOLE OF THE BAY OF ISLANDS OPHIOLITE SUITE.

TitleDYNAMOTHERMAL AUREOLE OF THE BAY OF ISLANDS OPHIOLITE SUITE.
Authors
Malpas, John
Issue Date1979
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, 1979, v. 16 n. 11, p. 2086-2101 How to Cite?
AbstractThe Bay of Islands ophiolite suite was displaced from an oceanic environment and emplaced upon the continental margin of Eastern North America during Early to Middle Ordovician times. The displacement tectonics produced a dynamothermal aureole that is found at the stratigraphic base of each ophiolite thrust slice. Structural and chemical studies of the aureole rocks indicate that they were produced by polyphase deformation of tuffaceous sediments and volcanic rocks under conditions of relatively high heat flux.
Persistent Identifierhttp://hdl.handle.net/10722/178115
ISSN
0008-4077
2023 Impact Factor: 1.3
2023 SCImago Journal Rankings: 0.460
ISI Accession Number ID
WOS:A1979HU84200002

 

DC FieldValueLanguage
dc.contributor.authorMalpas, Johnen_US
dc.date.accessioned2012-12-19T09:42:57Z-
dc.date.available2012-12-19T09:42:57Z-
dc.date.issued1979en_US
dc.identifier.citationCanadian Journal Of Earth Sciences, 1979, v. 16 n. 11, p. 2086-2101en_US
dc.identifier.issn0008-4077en_US
dc.identifier.urihttp://hdl.handle.net/10722/178115-
dc.description.abstractThe Bay of Islands ophiolite suite was displaced from an oceanic environment and emplaced upon the continental margin of Eastern North America during Early to Middle Ordovician times. The displacement tectonics produced a dynamothermal aureole that is found at the stratigraphic base of each ophiolite thrust slice. Structural and chemical studies of the aureole rocks indicate that they were produced by polyphase deformation of tuffaceous sediments and volcanic rocks under conditions of relatively high heat flux.en_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.titleDYNAMOTHERMAL AUREOLE OF THE BAY OF ISLANDS OPHIOLITE SUITE.en_US
dc.typeArticleen_US
dc.identifier.emailMalpas, John: jgmalpas@hku.hken_US
dc.identifier.authorityMalpas, John=rp00059en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0018547404en_US
dc.identifier.volume16en_US
dc.identifier.issue11en_US
dc.identifier.spage2086en_US
dc.identifier.epage2101en_US
dc.identifier.isiWOS:A1979HU84200002-
dc.publisher.placeCanadaen_US
dc.identifier.scopusauthoridMalpas, John=7006136845en_US
dc.identifier.issnl0008-4077-

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