Abstract
Abstract The results of palaeomagnetic measurements are given both for the Tertiary basalts of North Eastern Ireland, and for the Cretaceous sediments in the south of England. The direction of magnetization of the basalts is consistently shallower than the present dipole field direction by about 8°. The Cretaceous results are shown to be much less likely to be reliable, but also indicate a shallower dip than that of the present dipole field. A simple and reliable statistical treatment is developed for use with palaeomagnetic data.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
