Tempestite frequency curves: a key to Late Ordovician and Early Silurian subsidence, sea-level change, and orbital forcing in the Anticosti foreland basin, Quebec, Canada

Following partial closure of the northern Iapetus Ocean along the Newfoundland segment of the St. Lawrence Promontory, subsidence along the Anticosti Platform was influenced by residual thermal subsidence, renewed tectonic loading by thrust sheets to the south, and sediment loading. Basement subside...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Author: Long, D GF
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2007
Subjects:
Online Access:http://dx.doi.org/10.1139/e06-099
http://www.nrcresearchpress.com/doi/pdf/10.1139/e06-099