Precambrian bedrock geology, Southampton Island, Nunavut / [Authors: M. Sanborn-Barrie ... [et al.]].: M183-1/132-2013E-PDF
"Southampton Island, Nunavut, is situated between the Archean-dominated western Churchill Province and the Paleoproterozoic Baffin-Ungava segment of the Trans-Hudson Orogen. The island exposes a highland of Precambrian basement across much of its eastern half and flat-lying Paleozoic carbonate strata across its western half. The Precambrian basement complex consists predominantly of 3000–2700 Ma tonalitegranodiorite-granite gneiss, containing enclaves and inclusions of ca. 3 Ga maficultramafic-anorthositic plutonic rocks and lesser metasedimentary rocks. A smaller proportion of Paleoproterozoic gabbroic and granitic plutons also occurs. These rocks experienced profound amphibolite- to granulite-facies tectono-metamorphic reworking at 1880–1820 Ma, during the Trans-Hudson Orogen collision between the Rae and Superior cratons, resulting in their strongly foliated to gneissic character, followed by exhumation and cooling at 1790–1780 Ma"--Abstract.
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| Title | Precambrian bedrock geology, Southampton Island, Nunavut / [Authors: M. Sanborn-Barrie ... [et al.]]. |
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| Publication type | Monograph - View Master Record |
| Language | [English] |
| Format | Digital map |
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| Description | 1 map : col. + 1 map information document ([15] p.). |
| ISBN | 978-1-100-22028-4 |
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| Departmental catalogue number | 293328 |
| Cartographic data | Scale 1:250,000 ; Universal Transverse Mercator, zone 17 (W 85°15’--W 80°00'/N 65°30'--N 63°40’) |
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