The origin and timing of late-stage carbonate cements in Devonian carbonates of the deep Alberta basin : based on fluid inclusion and isotopic evidence
Deep basin Leduc Obed and Swan Hills Simonette calcite fluid inclusions yielded Th ranges of 127 to 172°C and 122 to 158°C; while saddle dolomites have Th from 136 to 148°C and 133 to 162°C, respectively. Calcite data from the subsurface suggest a 20°C/km geothermal gradient and saddle dolomite data...
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| Format: | Others |
| Language: | en |
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McGill University
2001
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| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=31541 |