000 03578nem  2200505zi 4500
0019.883867
003CaOODSP
00520230124091746
006m     o  d f      
007cr cn|||||||||
008200123t20202020onca   bh a  fo 0   eng d
020 |a9781100202754
040 |aCaOODSP|beng|erda|cCaOODSP
0410 |aeng|beng|bfre
043 |an-cn-yk
0861 |aM183-1/71-2020E-PDF
1001 |aLane, Larry Stephen, |d1953- |eauthor.
24510|aBedrock geology, Mount Raymond, Yukon, NTS 116-I/8 / |cauthor: L.S. Lane.
255 |aScale 1:50,000 ; |bUniversal Transverse Mercator, zone 8 |c(W 136°30'--W 136°00'/N 66°30'--N 66°15')
264 1|a[Ottawa] : |bNatural Resources Canada = Ressources naturelles Canada, |c2020.
264 4|c©2020
300 |a1 online resource (1 map) : |bcolour + |e1 map information document (10 unnumbered pages).
336 |acartographic image|bcri|2rdacontent
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aCanadian geoscience map ; |v71
500 |aIncorporates the western limb of the Richardson anticlinorium, southern Richardson Mountains, northern Yukon.
500 |aRelief shown by contours.
500 |aThis record only includes the map and the "map information document" in PDF; the complete data set with all the files in various formats is available for free download at http://geoscan.nrcan.gc.ca/.
504 |aIncludes bibliographical references.
5203 |a"The Mount Raymond map area incorporates the western limb of the Richardson anticlinorium, southern Richardson Mountains, northern Yukon. It is underlain by four Paleozoic sedimentary successions: middle Cambrian Slats Creek Formation, Cambrian to Early Devonian Road River Group, Devonian Canol Formation, and Late Devonian to Carboniferous Imperial and Tuttle formations. The Richardson trough depositional setting of the first three successions is succeeded by a deep-marine, turbiditic, Ellesmerian, orogenic foredeep setting for the Imperial-Tuttle succession. Several major thrust faults and related folds transect the map area from north to south. The carbonate-dominated Road River Group defines a west-dipping homocline, modified by the Mount Raymond thrust fault together with minor folds in its footwall. In the overlying Imperial-Tuttle succession, map-scale folds are defined where shales are interbedded with persistent sandstones. Steep reverse faults in the east may have reactivated Cambrian rift faults. The structural geometry reflects Late Cretaceous - Cenozoic regional Cordilleran tectonism"--Abstract.
546 |aIncludes abstracts in English and French.
650 0|aGeology|zYukon|vMaps.
650 6|aGéologie|zYukon|vCartes.
655 7|aGeological maps|2lcgft
655 7|aDigital maps|2lcgft
655 7|aCartes géologiques|2rvmgf
655 7|aCartes géographiques numériques|2rvmgf
7101 |aCanada. |bNatural Resources Canada, |eissuing body.
794 |tBedrock geology, Mount Raymond, Yukon, NTS 116-I/8 / |b2nd edition (2022)|w(CaOODSP)9.910402
830#0|aCanadian geoscience map ;|v71.|w(CaOODSP)9.506260
85640|qPDF|s8.88 MB|uhttps://publications.gc.ca/collections/collection_2022/rncan-nrcan/m183-1/M183-1-71-2020-eng.pdf|zMap
85640|qPDF|s721 KB|uhttps://publications.gc.ca/collections/collection_2022/rncan-nrcan/m183-1/M183-1-71-2020-1-eng.pdf|zMap information document
85640|qHTML|sN/A|uhttps://doi.org/10.4095/290066|zComplete data set