| 000 | 00000cam 2200000zi 4500 |
| 001 | 9.959929 |
| 003 | CaOODSP |
| 005 | 20260213105143 |
| 006 | m o d f |
| 007 | cr |n||||||||| |
| 008 | 260213t20152015oncdab ob f|0| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-nt |
| 086 | 1 |aM183-2/7975E-PDF |
| 100 | 1 |aKabanov, P., |eauthor. |
| 245 | 10|aShield to Selwyn Basin activity (Mackenzie Project, GEM) : |breport for 2015 : updates on Devonian stratigraphic study of Mackenzie River Corridor / |cP. Kabanov. |
| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2015. |
| 264 | 4|c©2015 |
| 300 | |a1 online resource (ii, 15 pages) : |bcharts, illustrations, maps. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aOpen file, |x2816-7155 ; |v7975 |
| 504 | |aIncludes bibliographical references (pages 13-15). |
| 520 | |a"The Devonian of the Mackenzie Project area is a thick (locally over 1 km) stratal package composed of carbonates, evaporites, and siliciclastics, recording the evolution of depositional environments from the passive-margin carbonate platform through the sediment-starved epiplatform anoxic basin to the foreland basin. The activity focuses on the economically prospective Lower Devonian Peel, Arnica, Landry, and Bear Rock / Fort Norman formations dominated by shallow-water carbonates and the Middle-Upper Devonian Horn River Group (Hare Indian, Ramparts, and Canol formations) dominated by kerogen-rich shales"--Abstract, page i. |
| 650 | 0|aGeology, Stratigraphic|yDevonian. |
| 650 | 0|aSedimentary rocks|zNorthwest Territories|zMackenzie River Valley|xComposition. |
| 650 | 6|aStratigraphie|yDévonien. |
| 650 | 6|aRoches sédimentaires|zTerritoires du Nord-Ouest|zMackenzie, ValleĢe du|xComposition. |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 830 | #0|aOpen file (Geological Survey of Canada)|v7975.|w(CaOODSP)9.506878 |
| 856 | 40|qPDF|s1.82 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-7975-eng.pdf |
| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/297311 |