| 000 | 00000nem 2200000za 4500 |
| 001 | 9.575338 |
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| 003 | CaOODSP |
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| 005 | 20230131161133 |
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| 006 | m go c f |
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| 007 | cr ||||||||||| |
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| 008 | 150406s2013 onc bd a fo 0 eng d |
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| 020 | |a978-1-100-21438-2 |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn-bc |
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| 086 | 1 |aM183-1/102-2012E-PDF |
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| 100 | 1 |aMcMechan, Margaret E. |q(Margaret Evaline), |d1953- |
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| 245 | 10|aGeology, Eight Mile Creek, British Columbia |h[electronic resource] / |c[by] M.E. McMechan. |
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| 250 | |aPreliminary version |
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| 255 | |aScale 1:50,000 |
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| 260 | |aOttawa : |bNatural Resources Canada, |cc2013. |
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| 300 | |a1 map : |bcol. |
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| 490 | 1 |aCanadian geoscience map ; |vNo. 102 |
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| 504 | |aIncludes bibliographical references. |
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| 520 | 3 |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. |
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| 546 | |aIncludes abstract in French. |
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| 590 | |a14-16|b2014-04-17 |
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| 692 | 07|2gccst|aGeological maps |
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| 692 | 07|2gccst|aWatercourses |
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| 692 | 07|2gccst|aSurficial geology |
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| 710 | 1 |aCanada. |bNatural Resources Canada. |
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| 710 | 2 |aGeological Survey of Canada. |
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| 830 | #0|aCanadian geoscience map ;|vNo. 102.|w(CaOODSP)9.506260 |
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| 856 | 40|qPDF|s9.10 MB|uhttps://publications.gc.ca/collections/collection_2014/rncan-nrcan/M183-1-102-2012-eng.pdf |
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| 856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/292046 |
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| 986 | |a292046 |
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