Sedimentology of the lower cretaceous gates and moosebar formations, northeast coalfields, British Columbia
The Lower Cretaceous Gates and Moosebar Formations in the Northeast Coalfields of British Columbia comprise a 350-450 m thick interval of marine and non-marine, coal bearing clastic sediments. The Moosebar Formation and lowermost unit of the Gates Formation (the Torrens Member) consist of between 2...
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| Language: | English |
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University of British Columbia
2010
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| Online Access: | http://hdl.handle.net/2429/24275 |