Palaeomagnetic Results from Lower Devonian Rocks of the Cheviot Hills, Northern England

Palaeomagnetic work has been undertaken on four different rock types from the Cheviot Hills, Northern England. A total of 64 independently oriented handsamples from 21 different sites have been examined for their remanent magnetization. The rocks have been dated (K/Ar) as Lower Devonian. The most re...

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Bibliographic Details
Published inGeophysical Journal of the Royal Astronomical Society Vol. 36; no. 2; pp. 487 - 496
Main Author Thorning, L.
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.02.1974
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Summary:Palaeomagnetic work has been undertaken on four different rock types from the Cheviot Hills, Northern England. A total of 64 independently oriented handsamples from 21 different sites have been examined for their remanent magnetization. The rocks have been dated (K/Ar) as Lower Devonian. The most reliable palaeopole has been obtained from the combined results for the rhyolites and the andesites of the Cheviot volcanic series. It is situated at position 11° S, 140° E (α95= 18°, 11 sites, 35 handsamples, af cleaned). This pole and also some preliminary poles calculated for the metamorphosed andesites and the Cheviot Granite support the existence of a Lower Devonian group of palaeomagnetic north poles in the region of New Guinea as defined by previously published results from other British formations.
Bibliography:istex:518DA37EC4A96C369E27F11381ED561D8293A44B
ark:/67375/HXZ-QTJ51PSS-T
ISSN:0956-540X
0016-8009
1365-246X
DOI:10.1111/j.1365-246X.1974.tb03650.x