Title | Laboratory physical characteristics of kimberlites from Smeaton, Saskatchewan |
Download | Download (whole publication) |
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Licence | Please note the adoption of the Open Government Licence - Canada
supersedes any previous licences. |
Author | Katsube, T J; Scromeda, N; Kjarsgaard, B A |
Source | Current research 1999-E/Recherches en cours 1999-E; by Geological Survey of Canada; Geological Survey of Canada, Current Research no. 1999-E, 1999 p. 65-71, https://doi.org/10.4095/210854 Open Access |
Year | 1999 |
Publisher | Natural Resources Canada |
Document | serial |
Lang. | English |
Media | paper; on-line; digital |
Related | This publication is contained in Current research 1999-E
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File format | pdf |
Province | Saskatchewan |
NTS | 73H/07; 73H/10 |
Area | Smeaton |
Lat/Long WENS | -105.0000 -104.5000 53.7500 53.2500 |
Subjects | industrial minerals; sedimentology; drillholes; analyses; bulk density; porosity; electrical resistivity; lithology; tuffs; kimberlites; exploration guidelines; cores; depositional environment; Fort à
la Corne kimberlite field |
Illustrations | analyses; stratigraphic columns |
Program | Canada-Saskatchewan Partnership Agreement on Mineral Development, 1990-1995 |
Released | 1999 09 01 |
Abstract | Bulk density, porosity, and electrical resistivity have been determined for ten kimberlite samples from Smeaton (Fort à la Corne field), Saskatchewan, as part of a basic physical rock property study
underway to provide information required for exploration activity in progress for kimberlite-hosted diamond deposits in Canada.
Results indicate that the range of values, 2.1-2.6 g/mL, 13-20%, and 20-280 ohm-metres for bulk density, porosity,
and electrical resistivity of these samples, respectively, are typical of those previously reported for crater-facies kimberlites, and generally resemble the values for sedimentary rocks. Electrical resistivity variations appear to be independent of
porosity, also a trend consistent with previous findings for crater-facies kimberlite. |
GEOSCAN ID | 210854 |
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