NJG49-3-03
1969
The paleomagnetism of the Kvamhesten Old Red sequence, southwest Norway
49
3
241-249

The inferred pole position (22°N, 170°E) for the Kvamshesten Old Red sequence is in fairly good harmony with other Old Red data of southern Norway. However, a deviation in declination of about 15° is thought to have arisen from a rotation (anti-clockwise) of this complex, a conclusion which is compatible with the geological observations. The stable remanence is considered as a moderate temperature viscous magnetization acquired during the time of diagenesis.

0029-196X
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