Contemporaneous faulting and clastic intrusions in the Quirke Lake Group, Elliot Lake, Ontario
Contemporaneous faults and clastic intrusions near Elliot Lake are common within the Espanola Formation of the Quirke Lake Group. Contemporaneous faults formed in response to differential vertical displacements which controlled regional paleocurrents and basin slope. The normal faults within the sed...
Published in: | Canadian Journal of Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1970
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Online Access: | http://dx.doi.org/10.1139/e70-021 http://www.nrcresearchpress.com/doi/pdf/10.1139/e70-021 |