The Palaeomagnetism of some Scottish Tertiary Dykes and their Baked Contacts
This paper presents results of measurements of the directions of magnetization of dyke samples and the associated baked sediments collected from Ayrshire in Scotland. The results suggest that these reversely and normally magnetized rocks are due to inversions of the Earth's magnetic field rather than to any self-reversal mechanism
CitationRaja, P. K. S. (1964). The palaeomagnetism of some Scottish Tertiary dykes and their baked contacts. Geophysical Journal International, 9(1), 15-19.
University of Nairobi