000 03151nem  2200445za 4500
0019.806239
003CaOODSP
00520230131161135
006m    go  c f      
007cr |||||||||||
008170207s2016    onca   bd a  fo 0   eng d
020 |a978-0-660-03858-2
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-nu
0861 |aM183-1/272-2015E-PDF
1001 |aSteenkamp, H. M.
24510|aGeology, Chidliak Bay (south), Baffin Island, Nunavut, NTS 26-B (south) |h[electronic resource] / |c[authors, H.M. Steenkamp, C. Gilbert, and M.R. St-Onge].
250 |aPreliminary version
255 |aScale 1:100 000 ; |bUniversal Transverse Mercator, zone 19 |c(W 68°00’--W 66°00'/N 64°30'--N 64°00’)
260 |a[Ottawa] : |bNatural Resources Canada, |cc2016.
300 |a1 map : |bcol. + |e1 map information document ([24] p.).
4901 |aCanadian geoscience map ; |v272
4900 |aCanada-Nunavut Science Office, open file map ; |v2016-08
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 Hall Peninsula Integrated Geoscience Program was led by the Canada-Nunavut Geoscience Office, and was designed to increase the geoscience knowledge and assess the economic potential of the area. Eastern Hall Peninsula is dominantly underlain by Archean tonalite to quartz diorite orthogneiss, while Paleoproterozoic supracrustal and intrusive rocks are exposed to the west. The supracrustal rocks are dominated by pelitic, psammitic, amphibolite and calc-silicate units, are interpreted as correlative with the Lake Harbour Group, and are cut by granulite-grade monzogranite to diorite intrusions. Hall Peninsula records three phases of metamorphism and deformation associated with the Trans-Hudson Orogen that have produced thick-skinned, east-verging fold and thrust structures and amphibolite to granulite facies mineral assemblages. Hall Peninsula hosts a highly prospective diamond kimberlite field, as well as mafic and carbonate supracrustal rocks, and ultramafic intrusions that may contain base and/or precious metal, semi-precious gemstone and carving stone resource potential"--Abstract.
546 |aIncludes abstract in French.
69207|2gccst|aGeological maps
69207|2gccst|aStratigraphy
69207|2gccst|aStructural geology
7001 |aGilbert, Celine.
7001 |aSt-Onge, M. R.
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
830#0|aCanadian geoscience map ;|v272.|w(CaOODSP)9.506260
85640|qPDF|s196.24 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1-272-2015-eng.pdf|zMap
85640|qPDF|s2.75 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1-272-2015-1-eng.pdf|zMap information document
85640|qHTML|sN/A|uhttps://doi.org/10.4095/297357|zGEOSCAN DOI