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Paleomagnetic study of the Great Foum Zguid dyke (southern Morocco): A positive contact test related to metasomatic processes

dc.contributor.authorSilva, Pedro
dc.contributor.authorHenry, B.
dc.contributor.authorMarques, Fernando O.
dc.contributor.authorMadureira, P.
dc.contributor.authorMiranda, Jorge Miguel
dc.date.accessioned2012-03-21T19:07:03Z
dc.date.available2012-03-21T19:07:03Z
dc.date.issued2006-11-01
dc.description.abstractWhen a paleomagnetic pole is sought for in an igneous body, the host rocks should be subjected to a contact test to assure that the determined paleopole has the age of the intrusion. If the contact test is positive, it precludes the possibility that the measured magnetization is a later effect. Therefore, we investigated the variations of the remanent magnetization along cross-sections of rocks hosting the Foum Zguid dyke (southern Morocco) and the dyke itself. A positive contact test was obtained, but it is mainly related with Chemical/Crystalline Remanent Magnetization due to metasomatic processes in the host-rocks during magma intrusion and cooling, and not only with Thermo-Remanent Magnetization as ordinarily assumed in standard studies. Paleomagnetic data obtained within the dyke then reflect the Earth magnetic field during emplacement of this well-dated (196.9 +/- 1.8 Ma) intrusion.por
dc.identifier.citationSILVA, Pedro F.; [et al] – Paleomagnetic study of the Great Foum Zguid dyke (southern Morocco): A positive contact test related to metasomatic processes.Geophysical Research Letters. ISSN 0094-8276. Vol. 33, N.º 21 (2006), pp. 1-6.por
dc.identifier.doi10.1029/2006GL027498
dc.identifier.issn0094-8276
dc.identifier.urihttp://hdl.handle.net/10400.21/1325
dc.language.isoengpor
dc.peerreviewedyespor
dc.publisherAmer Geophysical Unionpor
dc.subjectMagnetic-Propertiespor
dc.subjectAtlanticpor
dc.subjectPaleomagnetic
dc.subjectFoum Zguid dyke (southern Morocco)
dc.subjectChemical/Crystalline Remanent Magnetization
dc.subjectMetasomatic processes
dc.subjectThermo-Remanent Magnetization
dc.titlePaleomagnetic study of the Great Foum Zguid dyke (southern Morocco): A positive contact test related to metasomatic processespor
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlaceUSApor
oaire.citation.issue21por
oaire.citation.titleGeophysical Research Letterspor
oaire.citation.volume33
person.familyNameSilva
person.givenNamePedro
person.identifier1232178
person.identifier.ciencia-idC314-1157-FD0C
person.identifier.orcid0000-0002-9178-3623
person.identifier.ridB-8512-2008
person.identifier.scopus-author-id55431034700
rcaap.rightsrestrictedAccesspor
rcaap.typearticlepor
relation.isAuthorOfPublication54c96e27-8c3a-42d9-b751-ebc637c2f478
relation.isAuthorOfPublication.latestForDiscovery54c96e27-8c3a-42d9-b751-ebc637c2f478

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