Early development and flysch sedimentation in Ordovician Taconic foreland basin, west-central Newfoundland
During the Early to Late Ordovician the Taconic foredeep in west-central Newfoundland evolved from an underfilled to an overfilled state in response to cratonward advance, thickening, and erosion of the Taconic Orogen. Early orogen-derived sediment in the foreland basin consisted of middle(?) to lak...
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
1990
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Online Access: | http://dx.doi.org/10.1139/e90-133 http://www.nrcresearchpress.com/doi/pdf/10.1139/e90-133 |