Dual-Polarity Early Carboniferous Remagnetization of the Fisset Brook Formation, Cape Breton Island, Nova Scotia

Red siltstones and volcanic flows of the Fisset Brook Formation of Cape Breton Island, Nova Scotia, were folded or tilted in two phases, one of Late Tournaisian and the other of Mid-Namurian age. Upon thermal demagnetization, both rock types yield three components of magnetization, herein denoted as...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Johnson, Rex J. E., Van der Voo, Rob
Format: Text
Language:English
Published: Oxford University Press 1989
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/97/2/259
https://doi.org/10.1111/j.1365-246X.1989.tb00500.x