Stratigraphy, mud buildups, and carbonate platform development of the Upper Ordovician to Lower Devonian sequence, Ellesmere, Hans, and Devon Islands, Arctic Canada.

The Upper Ordovician to Lower Devonian platform in the Canadian Arctic twice evolved from a ramp to a rimmed shelf profile. Platform backstepping occurred in the fastigatus, acuminatus, cyphus?, sakmaricus (in North Greenland only) and linearis graptolite zones. Two major phases of pinnacle reef dev...

Full description

Bibliographic Details
Main Author: de Freitas, Tim A.
Format: Thesis
Language:unknown
Published: University of Ottawa (Canada) 1991
Subjects:
Online Access:http://hdl.handle.net/10393/7937
https://doi.org/10.20381/ruor-15571