Ordovician to Devonian sea-level changes in western and northern Canada

Lower Paleozoic sediments of central, Cordilleran, and arctic Canada are dominated by two megafacies: supratidal to shallow subtidal carbonates and minor evaporites of the platformal (cratonic) areas, and deeper water dark shales and dark limestones of the slope and basinal areas. Large areas of the...

Full description

Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Author: Lenz, A. C.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1982
Subjects:
Online Access:http://dx.doi.org/10.1139/e82-170
http://www.nrcresearchpress.com/doi/pdf/10.1139/e82-170