The polarity of the Silurian magnetic field; indications from a global data compilation

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doi: 10.1144/gsjgs.150.5.0823
Authors:Trench, A.; McKerrow, W. S.; Torsvik, T. H.; Li, Z. X.; McCracken, S. R.
Author Affiliations:Primary:
University of Western Australia, Department of Geology, Perth, West. Aust., Australia
Other:
University of Oxford, United Kingdom
Geological Survey of Norway, Norway
Volume Title:Journal of the Geological Society of London
Source:Journal of the Geological Society of London, Vol.150(Part 5), p.823-831. Publisher: Geological Society of London, London, United Kingdom. ISSN: 0016-7649
Publication Date:1993
Note:In English. 101 refs.; geol. sketch maps, strat. cols.
Summary:A generalized magnetic polarity history for the Silurian is presented. Preliminary inferences are that most of Silurian time was characterized by periods of mixed polarity, though Wenlock times mainly had a magnetic field of normal polarity. There are indications that the frequency of magnetic field reversals increased from Ordovician to Silurian times (to < 2 m.y. intervals). [R.A.H.]
Subjects:Llandovery; Lower Silurian; Ludlow; Magnetic field; Magnetostratigraphy; Paleomagnetism; Paleozoic; Pridoli; Reversals; Silurian; Upper Silurian; Wenlock
Abstract Numbers:94M/2651
Record ID:1993038146
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom
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