Palaeomagnetism of Permo-Triassic red sandstones from the Northern Calcareous Alps
Item
Title (Dublin Core)
en-US
Palaeomagnetism of Permo-Triassic red sandstones from the Northern Calcareous Alps
Description (Dublin Core)
en-US
It is generally agreed (Gwinner, 1971) that the Northern Calcareous Alps (together with the Northern Grauwackenzone) rest allochthonously on top of a Penninic basement and have been transported into their present position from the South after Upper Eocene. Their complicated structure is characterized by a series of nappes of various lateral extensions and thicknesses. A sketch map of the Western part of the Northern Calcareous Alps (Fig. 1) shows the main nappes (after Gwinner, 1971).
ARK: https://n2t.net/ark:/88439/y004586
Permalink: https://geophysicsjournal.com/article/200
ARK: https://n2t.net/ark:/88439/y004586
Permalink: https://geophysicsjournal.com/article/200
Creator (Dublin Core)
Soffel, H.
Subject (Dublin Core)
en-US
Northern Calcareous Alps
en-US
Permo-Triassic sandstones
en-US
Data
Publisher (Dublin Core)
en-US
Journal of Geophysics
Date (Dublin Core)
1978-12-22
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/200
Source (Dublin Core)
en-US
Journal of Geophysics; Vol 45 No 1 (1978): Journal of Geophysics; 447-450
2643-2986
2643-9271
Language (Dublin Core)
eng
Relation (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/200/160