| 000 | 00000cam 2200000zi 4500 |
| 001 | 9.959194 |
| 003 | CaOODSP |
| 005 | 20260122151652 |
| 006 | m o d f |
| 007 | cr |n||||||||| |
| 008 | 260122t20152015oncab ob f|0| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-nt |
| 086 | 1 |aM183-2/7809E-PDF |
| 100 | 1 |aHamblin, Anthony P., |eauthor. |
| 245 | 13|aAn Eocene post-kimberlite maar lake : |blacustrine oil-shale crater-fill deposits, Lac de Gras area, Northwest Territories, Canada / |cA.P. Hamblin. |
| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2015. |
| 264 | 4|c©2015 |
| 300 | |a1 online resource (i, 23 pages) : |billustrations, maps. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aOpen file, |x2816-7155 ; |v7809 |
| 504 | |aIncludes bibliographical references (pages 20-22). |
| 520 | |a"Sedimentology and organic petrology-geochemistry from a 160-metre core have been integrated to study the characteristics of an isolated pocket of fine-grained, siliciclastic Eocene sediments deposited within a small kimberlite crater basin, Lac de Gras, Northwest Territories, Canada. These sediments overlie the “Giraffe Pipe”, a kimberlite occurrence located at about 65°N/110°W, 25 km northeast of the Ekati Diamond Mine. The strata recovered in the studied core represent an overall shallowing-upward succession of lacustrine-peat mire basin-fill, interpreted to portray the deposits of a maar lake, one of the first identified in Canada (and one of the few maars anywhere to be associated with a kimberlitic pipe)"--Abstract, page 1. |
| 650 | 0|aMaars|zNorthwest Territories. |
| 650 | 0|aOil-shales|zNorthwest Territories. |
| 650 | 6|aMaars|zTerritoires du Nord-Ouest. |
| 650 | 6|aSchistes bitumineux|zTerritoire du Nord-Ouest. |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 830 | #0|aOpen file (Geological Survey of Canada)|v7809.|w(CaOODSP)9.506878 |
| 856 | 40|qPDF|s6.13 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-7809-eng.pdf |
| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/296430 |