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Michikamau Intrusion

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Journal Article
Published: 01 August 1976
Canadian Journal of Earth Sciences (1976) 13 (8): 1052–1057.
...R. F. Emslie; E. Irving; J. K. Park Abstract Newly available isotopic age measurements and paleomagnetic results on rocks of the Michikamau Intrusion and its surroundings have made possible more precise estimates of the position and age of the paleomagnetic pole. Results from six new collecting...
Journal Article
Published: 01 August 1965
Canadian Journal of Earth Sciences (1965) 2 (4): 385–399.
...Ronald F. Emslie Abstract The Michikamau Intrusion is a large, unmetamorphosed anorthositic mass lying within the broad belt of anorthositic bodies extending from southeastern Ontario to Labrador. Potassium–argon biotite dates place the time of crystallization of the intrusion at approximately 1...
Journal Article
Published: 01 October 1968
Canadian Journal of Earth Sciences (1968) 5 (5): 1139–1144.
...G. S. Murthy; W. F. Fahrig; D. L. Jones Abstract Twenty-nine oriented cores have been collected from six sites in the Michikamau Intrusion in Labrador. This had previously been well dated at 1400 m.y. by the potassium–argon method. A fold test has been applied to the paleomagnetic results after...
Image
Published: 01 June 2000
F IG . 9. Schematic cross section of the 2,000 km 2 Michikamau anorthositic intrusion, southeastern Labrador, Canada (modified from Emslie, 1970 ). The Michikamau intrusion is dominated by a lower Layered Series of leucotroctolitic and troctolitic cumulates overlain by a thick
Image
Regional map of Labrador showing the Nain Plutonic Suite’s Coastal and Interior Trend AMCG associations as well as major structural corridors in the region. Peralkaline igneous centres are shown in red. H – Harp Lake intrusion; HT – Hettasch intrusion; K – Kiglapait intrusion; MA – Makhavinekh pluton; MC – Michikamau intrusion; MS – Mistastin Batholith; N – Nain anorthosite; NI – Newark Island intrusion; NK – Napeu Kainiut quartz monzonite; NO – Notakwanon Batholith; TBP – Three Bays Pluton; U – Umiakovik Batholith. Modified from Emslie et al. (1994) and Kerr (2011). Pluton abbreviations after Emslie et al. (1994). Inset area is shown in detail in Figure 2.
Published: 20 May 2021
– Makhavinekh pluton; MC – Michikamau intrusion; MS – Mistastin Batholith; N – Nain anorthosite; NI – Newark Island intrusion; NK – Napeu Kainiut quartz monzonite; NO – Notakwanon Batholith; TBP – Three Bays Pluton; U – Umiakovik Batholith. Modified from Emslie et al. ( 1994 ) and Kerr ( 2011 ). Pluton
Journal Article
Published: 01 August 2010
The Canadian Mineralogist (2010) 48 (4): 705–710.
... of the Michikamau anorthositic intrusion, Labrador . Nature 202 , 172 – 173 . Emslie , R.F. ( 1965 ): The Michikamau anorthositic intrusion, Labrador . Can. J. Earth Sci . 2 , 385 – 399 . Emslie , R.F. ( 1969 ): Crystallization and differentiation of the Michikamau intrusion...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 June 2000
Economic Geology (2000) 95 (4): 677–701.
...F IG . 9. Schematic cross section of the 2,000 km 2 Michikamau anorthositic intrusion, southeastern Labrador, Canada (modified from Emslie, 1970 ). The Michikamau intrusion is dominated by a lower Layered Series of leucotroctolitic and troctolitic cumulates overlain by a thick...
FIGURES | View All (15)
Journal Article
Published: 01 December 1979
Journal of the Geological Society (1979) 136 (6): 725–736.
... L. Henderson R. G. Interative three-dimensional solution of gravity anomaly data using a digital computer Geophysics 1968 33 596 601 Emslie R. F. The Michikamau Anorthositic Intrusion, Labrador Can. J. Earth Sci 1965 2 385 99 Emslie R. F. The geology...
Journal Article
Published: 01 January 1973
Canadian Journal of Earth Sciences (1973) 10 (1): 54–71.
... to constitute an 'anorthosite suite' without prejudgement as to genetic implications.About 700 rock analyses, largely from the literature but supplemented by previously unpublished analyses from the Michikamau and Morin intrusions have been used to examine some of the chemical characteristics of the anorthosite...
Image
Comparison of Fo contents of olivine with An content of plagioclase from massif-type anorthosites and selected layered intrusions. Note that compositions of Zebra Mountain samples are more magnesian and calcic than in anorthosite massifs elsewhere. Figure modified after Ashwal (1993). HL = Harp Lake; MM = Mealy Mountains; PL = Paul Island; Mi = Michikamau; Ki = Kiglapait; Sk = Skaergaard; St = Stillwater.
Published: 01 August 2013
Fig. 6 Comparison of Fo contents of olivine with An content of plagioclase from massif-type anorthosites and selected layered intrusions. Note that compositions of Zebra Mountain samples are more magnesian and calcic than in anorthosite massifs elsewhere. Figure modified after Ashwal (1993) . HL
Journal Article
Published: 01 November 2004
Russ. Geol. Geophys. (2004) 45 (11): 1326–1336.
.... , The Michikamau anorthositic intrusion, Labrador , Canad. J. Earth Sci. , 2 , 385 – 399 , 1965 . 15. Emslie , R.F. , Geology and petrology of the Harp Lake Complex , Central Labrador: an example of Elsonian magmatism, Geol. Surv. Canad. Bull...
FIGURES
Journal Article
Published: 09 April 2024
Canadian Journal of Earth Sciences (2024) 61 (7): 750–759.
... anorthosite ( Martignole et al. 1993 ) (Pe in Fig. 1 ) and the 1327 ± 16 Ma ( Hébert et al. 2005 ) De La Blache massif (D in Fig. 1 ), both occurring within the “cold orogenic lid” region of the eastern Grenville Province. The rest—and collectively more voluminous—(Michikamau, Harp Lake, and Nain intrusive...
FIGURES
Image
Plots illustrating the temporality of several types of anorthosite. Age uncertainties are omitted for clarity, but are given in Table 1. (a) Age versus areal extent as a proxy for anorthosite volume. Although ages of massif-type anorthosites range from ~2.6 Ga to ~0.5 Ga, the largest examples, representing ~90% of the exposed massifs, are restricted from ~1.0 to ~1.8 Ga. These include the Kunene (KUN), Lac-Saint-Jean (LSJ), Harp Lake (HL), Nain (NA), Duluth (DUL), Lac Allard (LAL), Geransky (GER), Adirondack (ADK), Riga (RIG), Mealy Mountains (MM), Korosten (KOR), Flowers River (FL), Morin (MOR) and Michikamau (MIC) massifs. (b) Age versus An content of plagioclase. In most cases, the entire reported range of An content in consanguineous rocks is shown. For layered mafic intrusions, only An contents for anorthositic rocks are plotted.
Published: 01 August 2010
River (FL), Morin (MOR) and Michikamau (MIC) massifs. (b) Age versus An content of plagioclase. In most cases, the entire reported range of An content in consanguineous rocks is shown. For layered mafic intrusions, only An contents for anorthositic rocks are plotted.
Journal Article
Published: 01 January 1984
Jour. Geol. Soc. India (1984) 25 (1): 35–44.
.... EMSLIE, R. F., (1970) The geology of the Michikamau intrusion. Geol. Surr. Can. Pub., pp.57-68. FORBES, W. C. and FLOWER, M. F. J., (1974) Phase relations of titan-phlogopite, K2Mg4Ti A12Si6020 (OH)4: a refractory phase in the upper mantle? Earth planet. Sci. Lett., v. 22, pp. 60-66. GREEN, D. H...
Journal Article
Published: 03 June 2002
Canadian Journal of Earth Sciences (2002) 39 (5): 795–829.
..., and is the oldest. It may not be unique, however, as a coeval and lithologically similar body occupies a comparable tectonic setting in the eastern Churchill Province east of Michikamau Lake. South of the Trans-Labrador batholith, dated rocks include the Grady Island layered mafic intrusion and White Bear Arm...
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Journal Article
Published: 01 August 2010
The Canadian Mineralogist (2010) 48 (4): 729–750.
... anorthosites, nor do they follow the iron-enrichment, silica-depletion differentiation trend characteristic of anorthositic magmas ( Scoates 1994 , 2008 , Morisset et al. 2009 ). It is generally agreed that a link exists between layered mafic intrusions and massif anorthosites ( Morse 1968 , Ashwal...
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Journal Article
Journal: Economic Geology
Published: 01 August 2013
Economic Geology (2013) 108 (5): 953–986.
...Fig. 6 Comparison of Fo contents of olivine with An content of plagioclase from massif-type anorthosites and selected layered intrusions. Note that compositions of Zebra Mountain samples are more magnesian and calcic than in anorthosite massifs elsewhere. Figure modified after Ashwal (1993) . HL...
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Journal Article
Published: 01 December 2001
South African Journal of Geology (2001) 104 (4): 355–363.
... with features transitional between massif-type anorthosites and layered intrusions such as the Duluth and Michikamau intrusions. Table 1. Compositional data for rocks from the Tete Complex Sample Name LDA 11 LDA 19 LDA 3 LDA 5b D 467 TRDAN MASS CB 117...
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Journal Article
Journal: Geology
Published: 01 June 2005
Geology (2005) 33 (6): 513–516.
...Joshua M. Feinberg; Gary R. Scott; Paul R. Renne; Hans-Rudolf Wenk Abstract Submicroscopic, needle-shaped titanomagnetite inclusions exsolved in silicate minerals commonly occur in mafic intrusive rocks and are protected from alteration by their silicate hosts, making them excellent candidates...
FIGURES
Journal Article
Published: 01 August 2010
The Canadian Mineralogist (2010) 48 (4): 887–923.
... by a poorly exposed monzosyenite unit to the southwest. The sequence described here stands in contrast to the layered units of Michikamau Intrusion, Labrador ( Emslie 1970 ), where anorthosite overlies more mafic layers, a relationship to be expected if buoyancy alone controlled the formation of layering...
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