GEOSCAN, résultats de la recherche


TitreTracking the Late Jurassic apparent (or true) polar shift in U-Pb-dated kimberlites from cratonic North America (Superior Province of Canada)
AuteurKent, D V; Kjarsgaard, B A; Gee, J S; Muttoni, G; Heaman, L M
SourceGeochemistry, Geophysics, Geosystems (G3) vol. 16, issue 4, 2015 p. 983-994, (Accès ouvert)
Séries alt.Secteur des sciences de la Terre, Contribution externe 20150057
Documentpublication en série
Mediapapier; en ligne; numérique
ProvinceOntario; Manitoba; Territoires du Nord-Ouest; Nunavut; Région extracotière du nord
SNRC41; 42; 43; 53; 54; 55; 56; 57; 58; 59; 63; 64; 65; 66; 67; 68; 69; 76; 77; 78; 79; 86; 87; 88; 89; 96; 97; 98; 99; 106; 107; 116; 117
Lat/Long OENS-152.0000 -88.0000 85.0000 35.0000
Sujetsdérive du pôle; datations au uranium-plomb; datation au uranium-plomb; kimberlites; pôles paléomagnétiques; paléomagnétisme; interprétations paléomagnétiques; Province de Superior ; géochronologie; Mésozoïque; Jurassique
Illustrationslocation maps; plots
ProgrammeDiamands, GEM : La géocartographie de l'énergie et des minéraux
Diffusé2015 04 02
Résumé(disponible en anglais seulement)
Different versions of a composite apparent polar wander (APW) path of variably selected global poles assembled and averaged in North American coordinates using plate reconstructions show either a smooth progression or a large (~30°) gap in mean paleopoles in the Late Jurassic, between about 160 and 145 Ma. In an effort to further examine this issue, we sampled accessible outcrops/subcrops of kimberlites associated with high-precision U-Pb perovskite ages in the Timiskaming area of Ontario, Canada. The 154.9?±?1.1 Ma Peddie kimberlite yields a stable normal polarity magnetization that is coaxial within less than 5° of the reverse polarity magnetization of the 157.5?±?1.2 Ma Triple B kimberlite. The combined ~156 Ma Triple B and Peddie pole (75.5°N, 189.5°E, A95?=?2.8°) lies about midway between igneous poles from North America nearest in age (169 Ma Moat volcanics and the 146 Ma Ithaca kimberlites), showing that the polar motion was at a relatively steady yet rapid (~1.5°/Myr) pace. A similar large rapid polar swing has been recognized in the Middle to Late Jurassic APW path for Adria-Africa and Iran-Eurasia, suggesting a major mass redistribution. One possibility is that slab breakoff and subduction reversal along the western margin of the Americas triggered an episode of true polar wander.
Résumé(Résumé en langage clair et simple, non publié)
Détermination de l'âge et de données intégrée paléomagnétiques sont utilisés pour examiner les processus terre-échelle au cours teh période il ya 160 à 145 Ma.