Replacement dolomitization in the Upper Devonian Leduc and Swan Hills formations, Caroline area, Alberta, Canada
Replacement matrix dolomite (RMD) is present throughout the Leduc/Cooking Lake Formation, but is restricted to the bank margin in the Swan Hills Formation. RMD has an average crystal size of 140$ mu$m and fluoresces yellow in the Leduc/Cooking Lake Formation but has an average crystal size of 250$ m...
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| Format: | Others |
| Language: | en |
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McGill University
1990
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| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59892 |