The tectono-magnetic signature of the old red sandstone and pre-Devonian strata in the HÅSteinen Area, western Norway, and implications for the later stages of the Caledonian Orogeny-Reference-Cited by-同舟云学术

The tectono-magnetic signature of the old red sandstone and pre-Devonian strata in the HÅSteinen Area, western Norway, and implications for the later stages of the Caledonian Orogeny

Published:1987-06 Issue:3 Volume:6 Page:305-322
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Torsvik T. H.,Sturt B. A.,Ramsay D. M.,Vetti V.

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://www.agu.org/journals/tc/v006/i003/TC006i003p00305/TC006i003p00305.pdf

Reference34 articles.

1. The magnetic opaque petrological response to hydrothermal alteration;Ade-Hall;Geophys. J.R. Astron. Soc.,1971

2. Structural analysis of the Grøneheia area, Eikefjord, western Norway;Bryhni;Nor. Geol. Tidsskr.,1962

3. Relasjonen mellom senkaledonsk tektonikk og sedimentasjon ved Hornelens og Håsteinens devon;Bryhni;Bull. Nor. Geol. Unders.,1964

4. Flood deposits in the Hornelen Basin, West Norway (Old Red Sandstone);Bryhni;Nor. Geol. Tidsskr.,1978

5. Mekanismen bak Devon bassengenes mektighet, (abstract);Bryhni;Geolognytt.,1982

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