A paleomagnetic and U–Pb geochronology study of the western end of the Grenville dyke swarm: Rapid changes in paleomagnetic field direction at ca. 585Ma related to polarity reversals?

Author:

Halls Henry C.,Lovette AlanORCID,Hamilton Mike,Söderlund Ulf

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference59 articles.

1. Incompatible Ediacaran paleomagnetic directions suggest an equatorial geomagnetic dipole hypothesis;Abrajevitch;Earth Planet. Sci. Lett.,2010

2. U–Pb ages of metarhyolites of the Catoctin and Mount Rogers formations, central and southern Appalachians: evidence for two pulses of Iapetan rifting;Aleinikoff;Am. J. Sci.,1995

3. Axial vs. equatorial dipolar dynamo models with implications for planetary magnetic fields;Aubert;Earth Planet. Sci. Lett.,2004

4. Diabase dykes and the Grenville Front southwest of Sudbury, Ontario;Bethune,1988

5. Geochronological constraints on terminal Neoproterozoic events and the rise of Metazoans;Bowring,2003

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