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

26Citations
Citations of this article
10Readers
Mendeley users who have this article in their library.

Abstract

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. Copyright © 1974, Wiley Blackwell. All rights reserved

Cite

CITATION STYLE

APA

Thorning, L. (1974). Palaeomagnetic Results from Lower Devonian Rocks of the Cheviot Hills, Northern England. Geophysical Journal of the Royal Astronomical Society, 36(2), 487–496. https://doi.org/10.1111/j.1365-246X.1974.tb03650.x

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free