000 02306cem  2200385za 4500
0019.575338
003CaOODSP
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006m    go  c f      
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008150406s2013    onc    bd a  fo 0   eng d
020 |a978-1-100-21438-2
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-bc
0861 |aM183-1/102-2012E-PDF
1001 |aMcMechan, Margaret E. |q(Margaret Evaline), |d1953-
24510|aGeology, Eight Mile Creek, British Columbia |h[electronic resource] / |c[by] M.E. McMechan.
250 |aPreliminary version
255 |aScale 1:50,000
260 |aOttawa : |bNatural Resources Canada, |cc2013.
300 |a1 map : |bcol.
4901 |aCanadian geoscience map ; |vNo. 102
504 |aIncludes bibliographical references.
5203 |a"The Eight Mile Creek area (94-N/03) in the northernmost Canadian Rocky Mountain Foothills is underlain by Mississippian to Lower Cretaceous strata. In the east, Lower Cretaceous shale unconformably overlies a Lower to Middle Triassic coarsening-upward succession capped by shallow-water sandstone of the Liard Formation. In the west, several hundred metres of Upper Triassic carbonate rocks are preserved and Middle Triassic strata have thickened and changed into a deeper water facies. Folds dominate the structural style. Folds are upright with mixed asymmetry in the eastern part of the area. Folds range from upright to overturned and foreland-vergent farther west. Major fold detachments occur in Lower Triassic and Lower Cretaceous shales. Fold axial traces trend northwest to north. Occasional abrupt swings in orientation occur. Only a few discontinuous mappable thrust faults occur. Most are foreland-vergent and offset fold limbs"--Abstract.
546 |aIncludes abstract in French.
590 |a14-16|b2014-04-17
69207|2gccst|aGeological maps
69207|2gccst|aWatercourses
69207|2gccst|aSurficial geology
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
830#0|aCanadian geoscience map ;|vNo. 102.|w(CaOODSP)9.506260
85640|qPDF|s9.10 MB|uhttps://publications.gc.ca/collections/collection_2014/rncan-nrcan/M183-1-102-2012-eng.pdf
85640|qHTML|sN/A|uhttps://doi.org/10.4095/292046