000 03280nem  2200409za 4500
0019.859164
003CaOODSP
00520230131161139
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008180716s2015    quc    bd a  fo 0   eng d
020 |a978-1-100-21439-9
0341 |aa|b50000|dW117000|eW116000|fN071480|gN071300
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-nt
0861 |aM183-1/103-2012E-PDF
24500|aGeology, Nalluryuaq, Victoria Island, Northwest Territories |h[electronic resource] / |c[Authors: J.H. Bédard ... [et al.]].
250 |aPreliminary version
255 |aScale 1:50,000 ; |bUniversal Transverse Mercator, zone 11 |c(W 117°00’--W 116°00'/N 71°48'--N 71°30’)
260 |aOttawa : |bNatural Resources Canada, |c2015.
300 |a1 map : |bcol. + |e1 map information document ([11] p.).
4901 |aCanadian geoscience map ; |v103
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"NTS 87-G/9 (Nalluryaq) and the southernmost part of NTS 87-G/16 are mostly underlain by Neoproterozoic Shaler Supergroup sedimentary rocks, with limestone and dolostone of the Boot Inlet and Jago Bay formations, quartz arenite of the Fort Collinson Formation, and gypsum evaporite of the Minto Inlet Formation. The latter locally form quarryable alabaster deposits as a result of contact metamorphism. Sedimentary rocks are injected by basaltic sills and dykes of Franklin age (ca. 720 Ma) that can be divided into older, more olivine-rich Type 1 intrusions and younger diabasic to feldspar-porphyritic Type 2 intrusions. Fe-oxide exoskarns are developed in the hangingwall panels of some synmagmatic normal faults. Strata are either flat-lying, or dip gently to the north or south to either side of the Walker Bay Anticline. Steeper bedding orientations occur near faults as a result of structural entrainment. A regional-scale basal unconformity separates Paleozoic clastic and carbonate rocks in the north from underlying Proterozoic rocks to the south, but the contact is often faulted, and isolated domains of Paleozoic rocks are preserved within graben. North-northwest-trending syn-magmatic (Proterozoic) and east-northeast-trending (Phanerozoic) normal faults are ubiquitous, breaking up the outcrop pattern into a series of polygonal blocks"--Abstract.
546 |aIncludes abstract in French.
69207|2gccst|aGeological maps
69207|2gccst|aGeomorphology
69207|2gccst|aSurficial geology
7001 |aBédard, Jean H., |d1955-
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
830#0|aCanadian geoscience map ;|v103.|w(CaOODSP)9.506260
85640|qPDF|s27.48 MB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-103-2012-eng.pdf|zMap
85640|qPDF|s786 KB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-103-2012-1-eng.pdf|zMap information document
85640|qHTML|sN/A|uhttps://doi.org/10.4095/297284|zGEOSCAN DOI