Paleomagnetism of Jurassic sediments from the western border of the Rheingraben, Alsace (France)
Item
Title (Dublin Core)
en-US
Paleomagnetism of Jurassic sediments from the western border of the Rheingraben, Alsace (France)
Description (Dublin Core)
en-US
Upper Bajocian oolithic limestones and Pliensbachian marls and marly ovoids from 9 sites distributed over 4 exposures at the western border of the Rheingraben (mean coordinates 47.8° N, 7.5° E) were sampled by 92 samples. The carriers of the natural remanent magnetization in the limestones are goethite and magnetite, and in the marls and ovoids the carrier is magnetite. After tectonic correction, the characteristic component of NRM isolated in the cleaning processes was mostly of normal polarity. The mean direction is D = 30.1°, I = 53.2° (N = 7, k = 92, α95 = 6.3°) and the pole position is 63.1° N, 120.1° E. It is close to the Jurassic reference data for the stable European plate.
ARK: https://n2t.net/ark:/88439/y066400
Permalink: https://geophysicsjournal.com/article/122
ARK: https://n2t.net/ark:/88439/y066400
Permalink: https://geophysicsjournal.com/article/122
Creator (Dublin Core)
Kadzialko-Hofmokl, M.
Kruczyk, J.
Westphal, M.
Subject (Dublin Core)
en-US
Paleomagnetism
en-US
Jurassic
en-US
Bajocian
en-US
France
en-US
Sediments
en-US
Data
Publisher (Dublin Core)
en-US
Journal of Geophysics
Date (Dublin Core)
1987-11-05
Type (Dublin Core)
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US
Peer-reviewed Article
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/122
Source (Dublin Core)
en-US
Journal of Geophysics; Vol 62 No 1 (1988): Journal of Geophysics; 102-108
2643-2986
2643-9271
Language (Dublin Core)
eng
Relation (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/122/84