The tectonic implications of Solundian (Upper Devonian) magnetization of the Devonian rocks of Kvamshesten, western Norway

T. H. Torsvik; B. A. Sturt; D. M. Ramsay; H. J. Kisch; D. Bering

doi:10.1016/0012-821X(86)90115-9

The tectonic implications of Solundian (Upper Devonian) magnetization of the Devonian rocks of Kvamshesten, western Norway

T. H. Torsvik, B. A. Sturt, D. M. Ramsay, H. J. Kisch, D. Bering

Department of Earth and Environmental sciences

Research output: Contribution to journal › Article › peer-review

46 Scopus citations

Abstract

The allochthonous Old Red Sandstone of Kvamshesten, western Norway, records polyphase orogenic deformation, and palaeomagnetic results from both the Devonian sediments and mylonites associated with the basal thrust define a syn- (to post-) tectonic magnetization with D = 218°, I = +3° and α₉₅ = 9.7°. The corresponding pole position (lat. 21°S, long. 324°E) suggests a Late Devonian/Early Carboniferous magnetization age (Solundian), and probably dates the time of thrust movements.

Original language	English
Pages (from-to)	337-347
Number of pages	11
Journal	Earth and Planetary Science Letters
Volume	80
Issue number	3-4
DOIs	https://doi.org/10.1016/0012-821X(86)90115-9
State	Published - 1 Jan 1986

ASJC Scopus subject areas

Geophysics
Geochemistry and Petrology
Earth and Planetary Sciences (miscellaneous)
Space and Planetary Science

Access to Document

10.1016/0012-821X(86)90115-9

Cite this

@article{5e32d443a0774cf5b32bfa86d144b426,

title = "The tectonic implications of Solundian (Upper Devonian) magnetization of the Devonian rocks of Kvamshesten, western Norway",

abstract = "The allochthonous Old Red Sandstone of Kvamshesten, western Norway, records polyphase orogenic deformation, and palaeomagnetic results from both the Devonian sediments and mylonites associated with the basal thrust define a syn- (to post-) tectonic magnetization with D = 218°, I = +3° and α95 = 9.7°. The corresponding pole position (lat. 21°S, long. 324°E) suggests a Late Devonian/Early Carboniferous magnetization age (Solundian), and probably dates the time of thrust movements.",

author = "Torsvik, {T. H.} and Sturt, {B. A.} and Ramsay, {D. M.} and Kisch, {H. J.} and D. Bering",

note = "Funding Information: This project has been supported by Elf Aqm-tame Norway (Devoman Project). T.H.T and D B acknowledge the Norwegian Research Councd for the Humanmes and Science for flnancml support Comments on the manuscnpt by Prof. J.C Brlden and helpful correcttons by anonymous referees are gratefully acknowledged. Mr H. Walderhaug and K Breyholdz are thanked for laboratory assistance and figure drawings Norwegian Lithosphere Contribution (06)",

year = "1986",

month = jan,

day = "1",

doi = "10.1016/0012-821X(86)90115-9",

language = "English",

volume = "80",

pages = "337--347",

journal = "Earth and Planetary Science Letters",

issn = "0012-821X",

publisher = "Elsevier BV",

number = "3-4",

}

TY - JOUR

T1 - The tectonic implications of Solundian (Upper Devonian) magnetization of the Devonian rocks of Kvamshesten, western Norway

AU - Torsvik, T. H.

AU - Sturt, B. A.

AU - Ramsay, D. M.

AU - Kisch, H. J.

AU - Bering, D.

N1 - Funding Information: This project has been supported by Elf Aqm-tame Norway (Devoman Project). T.H.T and D B acknowledge the Norwegian Research Councd for the Humanmes and Science for flnancml support Comments on the manuscnpt by Prof. J.C Brlden and helpful correcttons by anonymous referees are gratefully acknowledged. Mr H. Walderhaug and K Breyholdz are thanked for laboratory assistance and figure drawings Norwegian Lithosphere Contribution (06)

PY - 1986/1/1

Y1 - 1986/1/1

N2 - The allochthonous Old Red Sandstone of Kvamshesten, western Norway, records polyphase orogenic deformation, and palaeomagnetic results from both the Devonian sediments and mylonites associated with the basal thrust define a syn- (to post-) tectonic magnetization with D = 218°, I = +3° and α95 = 9.7°. The corresponding pole position (lat. 21°S, long. 324°E) suggests a Late Devonian/Early Carboniferous magnetization age (Solundian), and probably dates the time of thrust movements.

AB - The allochthonous Old Red Sandstone of Kvamshesten, western Norway, records polyphase orogenic deformation, and palaeomagnetic results from both the Devonian sediments and mylonites associated with the basal thrust define a syn- (to post-) tectonic magnetization with D = 218°, I = +3° and α95 = 9.7°. The corresponding pole position (lat. 21°S, long. 324°E) suggests a Late Devonian/Early Carboniferous magnetization age (Solundian), and probably dates the time of thrust movements.

UR - http://www.scopus.com/inward/record.url?scp=0022887970&partnerID=8YFLogxK

U2 - 10.1016/0012-821X(86)90115-9

DO - 10.1016/0012-821X(86)90115-9

M3 - Article

AN - SCOPUS:0022887970

SN - 0012-821X

VL - 80

SP - 337

EP - 347

JO - Earth and Planetary Science Letters

JF - Earth and Planetary Science Letters

IS - 3-4

ER -

The tectonic implications of Solundian (Upper Devonian) magnetization of the Devonian rocks of Kvamshesten, western Norway

Abstract

ASJC Scopus subject areas

Access to Document

Other files and links

Fingerprint

Cite this