Anomalous geomagnetic field during the late Ordovician

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

14

Scientific paper

MEASUREMENTS of the Lower Palaeozoic magnetic field in the British Isles1 show that it changed from around D=355°, I=-50° to D=20°, I=-54° (corresponding to an apparent shift of the south palaeomagnetic pole from 0° W to 35 °W along the present Equator) between Ordovician and Devonian times. Following unpublished work by W. E. Tremlett and J. C. Briden, we report here conflicting evidence from the intrusive rocks between Conway and Pwllheli, North Wales. These rocks therefore seem to show either previously unrecognised tectonic rotations or hitherto unsuspected variation in the palaeomagnetic field.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Anomalous geomagnetic field during the late Ordovician does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Anomalous geomagnetic field during the late Ordovician, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Anomalous geomagnetic field during the late Ordovician will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1298864

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.