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...
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
2007
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Online Access: | http://dx.doi.org/10.1139/e06-099 http://www.nrcresearchpress.com/doi/pdf/10.1139/e06-099 |