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Tsezotene Formation

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Journal Article
Published: 01 October 1981
Canadian Journal of Earth Sciences (1981) 18 (10): 1572–1580.
...J. K. Park Abstract A paleomagnetic study was conducted on a regionally extensive diabase sill intruding the upper part of the Helikian (?) Tsezotene Formation located in the Mackenzie Mountains Supergroup of northwestern Canada. Twelve sites, one from a lower sill at one locality, were sampled...
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Ar – Ar data for detrital muscovites from the <b>Tsezotene</b> <b>Formation</b> of the Ma...
Published: 26 August 2005
Table 4. Ar – Ar data for detrital muscovites from the Tsezotene Formation of the Mackenzie Mountains Supergroup (sample DT-95-11-1B; J f = 0.01944 ± 0.00019; Z4539; 64.8466°N, 133.1149°E). Laser power a Volume 39 Ar (×10 –11  cm 3 ) %Atm. 40 Ar
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Ar – Ar data for detrital muscovites from the <b>Tsezotene</b> <b>Formation</b> of the Ma...
Published: 26 August 2005
Table 4. Ar – Ar data for detrital muscovites from the Tsezotene Formation of the Mackenzie Mountains Supergroup (sample DT-95-11-1B; J f = 0.01944 ± 0.00019; Z4539; 64.8466°N, 133.1149°E). Laser power a Volume 39 Ar (×10 –11  cm 3 ) %Atm. 40 Ar
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Ar – Ar data for detrital muscovites from the <b>Tsezotene</b> <b>Formation</b> of the Ma...
Published: 26 August 2005
Table 4. Ar – Ar data for detrital muscovites from the Tsezotene Formation of the Mackenzie Mountains Supergroup (sample DT-95-11-1B; J f = 0.01944 ± 0.00019; Z4539; 64.8466°N, 133.1149°E). Laser power a Volume 39 Ar (×10 –11  cm 3 ) %Atm. 40 Ar
Image
Ar – Ar data for detrital muscovites from the <b>Tsezotene</b> <b>Formation</b> of the Ma...
Published: 26 August 2005
Table 4. Ar – Ar data for detrital muscovites from the Tsezotene Formation of the Mackenzie Mountains Supergroup (sample DT-95-11-1B; J f = 0.01944 ± 0.00019; Z4539; 64.8466°N, 133.1149°E). Laser power a Volume 39 Ar (×10 –11  cm 3 ) %Atm. 40 Ar
Image
Ar – Ar data for detrital muscovites from the <b>Tsezotene</b> <b>Formation</b> of the Ma...
Published: 26 August 2005
Table 4. Ar – Ar data for detrital muscovites from the Tsezotene Formation of the Mackenzie Mountains Supergroup (sample DT-95-11-1B; J f = 0.01944 ± 0.00019; Z4539; 64.8466°N, 133.1149°E). Laser power a Volume 39 Ar (×10 –11  cm 3 ) %Atm. 40 Ar
Journal Article
Published: 01 February 1982
Canadian Journal of Earth Sciences (1982) 19 (2): 316–323.
... the base of the Windermere Supergroup. Rb–Sr isochron dates of 766 ± 24 and 769 ± 27 Ma have been obtained for two of the these diabase sheets, which intruded the Tsezotene Formation of the Mackenzie Mountains Supergroup. The emplacement of the diabase sills and dikes may be related to either of two...
Journal Article
Published: 01 November 1989
Canadian Journal of Earth Sciences (1989) 26 (11): 2194–2203.
... to the dominantly clastic Late Proterozoic Tsezotene Formation and Katherine Group of the Mackenzie Mountains Supergroup. Tests of Carey's orocline hypothesis for the arc using linear regression and a plan-view application of the fold test suggest, in line with earlier structural studies, that the arc is largely...
Journal Article
Published: 01 March 1986
Canadian Journal of Earth Sciences (1986) 23 (3): 308–323.
..., whose probable primary pole lies at the beginning of the sequence, near the younger end of the Grenville Track (0.88 Ga). The end of the apparent polar wander (APW) sequence may be defined by a primary pole from sills intruding the Tsezotene Formation below the Katherine. We relate the sills, dated...
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Release spectra for  40 Ar –  39 Ar muscovite ages of six detrital white mi...
Published: 26 August 2005
Fig. 8. Release spectra for 40 Ar – 39 Ar muscovite ages of six detrital white mica grains from the Tsezotene Formation of the Mackenzie Mountains Supergroup. Data in Table  4 .
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Probability density diagrams and histograms for detrital zircon samples fro...
Published: 30 June 2017
Figure 6. Probability density diagrams and histograms for detrital zircon samples from Tsezotene Formation and Katherine Group sandstones of the Mackenzie basin. Age ranges of potential source regions are highlighted with colored bars. 207 Pb/ 206 Pb ages are plotted on x -axis only
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Probability density plots (dashed lines) and kernel density estimates (soli...
Published: 17 July 2019
source: Rae Group (Gp)— Turner et al. (2016) ; Rainbird et al. (2017) ; Tsezotene Formation (Fm) and Katherine Gp— Rainbird et al. (2017) ; Uy Gp— Rainbird et al. (1998) ; Khudoley et al. (2015) ; Diaoyutai Fm— Yang et al. (2012) ; this study; Qiaotou Fm—this study; Xinxing Fm— Yang et al. (2012
Journal Article
Published: 16 December 2008
Canadian Journal of Earth Sciences (2008) 45 (10): 1159–1184.
... maps ( Blusson 1972 ; Gabrielse et al. 1972 a , 1972 b , 1973 ; Aitken 1974 ; Aitken et al. 1974 ; Aitken and Cook 1979 a , 1979 b ; Norris 1982 a , 1982 b ). Thickness data for the Tsezotene Formation and isopach maps for the Katherine Group ( Fig. 3 ) support the contention...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 30 June 2017
GSA Bulletin (2017) 129 (11-12): 1408–1423.
...Figure 6. Probability density diagrams and histograms for detrital zircon samples from Tsezotene Formation and Katherine Group sandstones of the Mackenzie basin. Age ranges of potential source regions are highlighted with colored bars. 207 Pb/ 206 Pb ages are plotted on x -axis only...
FIGURES | View All (10)
Journal Article
Published: 01 June 1984
Bulletin of Canadian Petroleum Geology (1984) 32 (2): 139–146.
... the subsur- face distribution of the four lowest formations of the 'Mackenzie Mountains upergroup' (Fig. 2) in the area of interest (Fig. 1). In downward succession, they are Kather- ine Group, Tsezotene Formation, Map-unit H1 (of Aitken et a l . , 1982) and sub-H1 beds. The Katherine consists of grey...
Journal Article
Published: 26 August 2005
Canadian Journal of Earth Sciences (2005) 42 (6): 1045–1071.
...Table 4. Ar – Ar data for detrital muscovites from the Tsezotene Formation of the Mackenzie Mountains Supergroup (sample DT-95-11-1B; J f = 0.01944 ± 0.00019; Z4539; 64.8466°N, 133.1149°E). Laser power a Volume 39 Ar (×10 –11  cm 3 ) %Atm. 40 Ar...
FIGURES | View All (10)
Journal Article
Journal: Geology
Published: 01 December 2003
Geology (2003) 31 (12): 1053–1056.
... ), the regionally extensive 18–60-m-thick Concajou Canyon sill is exposed over a distance of ∼200 km ( Park, 1981 ). The sill intrudes the upper part of the Proterozoic Tsezotene Formation of the Mackenzie Mountains Supergroup and is part of a regionally extensive suite of mafic rocks that intrudes the sedimentary...
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Journal Article
Published: 01 January 2007
Russ. Geol. Geophys. (2007) 48 (1): 32–45.
... of the Precambrian Little Dal Group, Mackenzie Mountains, Northwest Territories, Canada . Can. J. Earth Sci. 21 , 371 – 375 . Park , J.K. , Aitken , J.D. , 1986 . Paleomagnetism of the late Proterozoic Tsezotene Formation of northwest Canada . J. Geophys. Res. 91 , 4955 – 4970 . Park...
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Journal Article
Journal: GSA Bulletin
Published: 17 June 2019
GSA Bulletin (2020) 132 (3-4): 710–738.
... variability in the tilts permitted a fold test to be robustly conducted. Additionally, true polar wander (TPW) or large plate motions may have been averaged in the mean formation poles, as the virtual geomagnetic poles (VGPs) from the uppermost member (Walcott Member) were 30° away from the underlying VGPs...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 June 2015
Lithosphere (2015) 7 (3): 275–295.
... ). It is not clear if this thinning is due to stratigraphic or structural truncation. The contact between the Kikiktat volcanics and the underlying siliciclastic strata of the Neruokpuk Formation (sensu Robinson et al., 1989 ), or O.G. map unit ( Macdonald et al., 2009 ), is generally structural, although at some...
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