Stratigraphic and Carbon Isotope Evolution of an Ediacaran Mixed Siliciclastic Deep-Marine Base-of-Slope System, First Isaac Carbonate, Windermere Supergroup, Canadian Cordillera, British Columbia.

Stratigraphic and Carbon Isotope Evolution of an Ediacaran Mixed Siliciclastic Deep-Marine Base-of-Slope System, First Isaac Carbonate, Windermere Supergroup, Canadian Cordillera, British Columbia.

The first Isaac carbonate (FIC) is a mixed siliciclastic-carbonate base-of-slope succession in the Neoproterozoic Windermere Supergroup (WSG). Outstanding outcrop exposure at three study areas provided an excellent opportunity to observe the stratigraphic and isotopic evolution of an ancient deepwat...

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Bibliographic Details
Main Author: Cochrane, Dylan
Other Authors: Arnott, Robert
Format: Others
Language:en
Published: Université d'Ottawa / University of Ottawa 2018
Subjects:
Deep-Marine Sedimentology
Carbon Isotope Chemostratigraphy
Neoproterozoic
Ediacaran
Base-of-Slope
Mixed Carbonate-Siliciclastic system
Windermere Supergroup
Online Access:http://hdl.handle.net/10393/37363
http://dx.doi.org/10.20381/ruor-21633

Internet

http://hdl.handle.net/10393/37363
http://dx.doi.org/10.20381/ruor-21633

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