Abstract
Palaeomagnetic inclination records are demonstrated for the first time to be repeatable between lakes. These magnetic variations can now be interpreted with confidence as being a true geomagnetic record. New radiocarbon age determinations refine the time scale of secular changes recorded in Britain over the last 104 years. The paired D & I magnetic measurements form a detailed master curve of 23 features for dating European sediments. The improved records and time scale show that neither the declination nor inclination fluctuations have been periodic. Tight or clockwise looping of the geomagnetic vector has been dominant over Britain since 10,000 B.P.
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.
