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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11963
DC FieldValueLanguage
dc.date.accessioned2018-10-22T06:43:14Zen
dc.date.available2018-10-22T06:43:14Zen
dc.date.issued2018-04en
dc.identifier.urihttp://hdl.handle.net/2122/11963en
dc.descriptionResearch Focus on Geologyen
dc.description.abstractPaleomagnetic records from sedimentary sequences have a fundamental importance, both for tectonic and stratigraphic studies (Kodama, 2012). However, despite many decades of research on sedimentary paleomagnetism (the first study was published 80 years ago; McNish and Johnson, 1938), details concerning the mechanism(s) by which sediments become magnetized are still poorly understood.en
dc.language.isoEnglishen
dc.relation.ispartofGeologyen
dc.relation.ispartofseries/46 (2018)en
dc.titleNew insights on sediment magnetic remanence acquisition point out complexity of magnetic mineral diagenesisen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber383-384en
dc.identifier.URLhttps://pubs.geoscienceworld.org/gsa/geology/article/46/4/383/529551/new-insights-on-sediment-magnetic-remanenceen
dc.subject.INGVpaleomagnetismen
dc.identifier.doi10.1130/focus042018.1en
dc.description.obiettivoSpecifico1A. Geomagnetismo e Paleomagnetismoen
dc.description.journalTypeJCR Journalen
dc.contributor.authorSagnotti, Leonardoen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.orcid0000-0003-3944-201X-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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