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...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Author: González-Bonorino, Gustavo
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1990
Subjects:
Online Access:http://dx.doi.org/10.1139/e90-133
http://www.nrcresearchpress.com/doi/pdf/10.1139/e90-133