000 03484cem  2200445za 4500
0019.557309
003CaOODSP
00520221107133920
006m    go  c f      
007cr |||||||||||
008160715s2015    onc    bd a  fo 0   iku d
020 |a978-0-662-03884-9
040 |aCaOODSP|beng
041 |aiku|beng
043 |an-cn-nu
0861 |aM183-1/215-2015S-PDF
24500|a[Geology, Terra Nivea, Baffin Island, Nunavut] |h[electronic resource] / |c[authors, M.R. St-Onge … [et al.]].
250 |aPreliminary version
255 |aScale 1:100 000 ; |bUniversal Transverse Mercator, zone 10 |c(W 120°45’--W 121°11'/N 50°20'--N 50°35’)
260 |a[Ottawa] : |bNatural Resources Canada, |cc2015.
300 |a1 map : |bcol. + |e1 map information document ([20] p.).
4901 |aCanadian geoscience map ; |v215S
4900 |aCanada-Nunavut Geoscience Office open file map ; |v2015-02S
500 |aIssued also in English.
500 |aEnglish title supplied by the publisher.
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"This map synthesizes the field observations and initial interpretations for the Terra Nivea area following five weeks of regional and targeted bedrock mapping on the eastern Meta Incognita Peninsula, Baffin Island, Nunavut. Under the Geo-mapping for Energy and Minerals (GEM) Program, this area was targeted in 2014 to upgrade the geoscience knowledge and document the economic potential of the greater Iqaluit area south of Frobisher Bay. Field observations have constrained the distribution of metasedimentary units comprising quartzite, marble, psammite, pelite, and semipelite, all of which can be correlated with the contiguous middle Paleoproterozoic Lake Harbour Group in the type area north of Kimmirut. The full range of siliciclastic and minor carbonate rock types can be traced to the easternmost tip of Meta Incognita Peninsula. The distribution and eastern limit of high-grade felsic and mafic plutonic rocks, tentatively interpreted as part of the middle Paleoproterozoic Cumberland Batholith, were delineated. Three distinct phases of deformation and one metamorphic episode were recognized. The deformation and metamorphic events can be correlated with similar features and assemblages previously documented both on Baffin Island and on the Ungava Peninsula of northern Quebec, and will be utilized to compare, and improve on, existing regional tectonic models"--Abstract.
546 |aText in Inuktitut, abstract in English.
69207|2gccst|aGeological maps
69207|2gccst|aGeological maps
69207|2gccst|aStructural geology
7001 |aSt-Onge, M. R.
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
77508|tGeology, Terra Nivea, Baffin Island, Nunavut |w(CaOODSP)9.557271
830#0|aCanadian geoscience map ;|v215S.|w(CaOODSP)9.512575
85640|qPDF|s225.45 MB|uhttps://publications.gc.ca/collections/collection_2016/rncan-nrcan/M183-1-215-2015-1-iku.pdf|zMap
85640|qPDF|s2.40 MB|uhttps://publications.gc.ca/collections/collection_2016/rncan-nrcan/M183-1-215-2015-iku.pdf|zMap information document
85640|qHTML|sN/A|uhttps://doi.org/10.4095/296105|zGEOSCAN DOI