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Labrieville

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Journal Article
Published: 17 July 2002
Canadian Journal of Earth Sciences (2002) 39 (6): 983–997.
...Brent E. Owens; Paul B. Tomascak Abstract Mesoproterozoic lamprophyre dikes occur at four localities within the ∼1010 Ma Labrieville anorthosite in the Grenville Province of southern Quebec. All dikes are thin (<20 cm wide), oriented ∼N57 W, and steeply dipping. Three are biotite lamprophyres...
FIGURES | View All (8)
Journal Article
Published: 01 February 1995
American Mineralogist (1995) 80 (1-2): 144–161.
...Brent E. Owens; Robert F. Dymek Abstract Newly discovered orthopyroxene and clinopyroxene megacrysts (OPMs and CPMs) in the Labrieville massif provide additional constraints on megacryst origins and their significance in massif anorthosite petrogenesis. Pyroxene megacrysts (~ 1–15 cm across) occur...
Journal Article
Published: 01 March 1992
The Canadian Mineralogist (1992) 30 (1): 163–190.
Journal Article
Published: 01 December 1966
American Mineralogist (1966) 51 (11-12): 1671–1711.
...Alfred T. Anderson, Jr. Abstract The Labrieville anorthosite massif is an example of crystallization differentiation in a plutonic environment. As in other St. Urbain-type anorthosites (characterized in particular by andesine anti-perthite and hemo-ilmenite), the lithologic sequence is: anorthosite...
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Simplified geologic sketch map of the <span class="search-highlight">Labrieville</span> massif showing locations ...
Published: 17 July 2002
Fig. 1. Simplified geologic sketch map of the Labrieville massif showing locations and orientations of lamprophyre dikes. Dike sizes are greatly exaggerated. The inset shows the location of the Labrieville massif (LBV) relative to the Lac-Saint-Jean (LSJ) and Saint-Urbain (STU) massifs. AMB
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Chondrite-normalized rare-earth element (REE) abundances in <span class="search-highlight">Labrieville</span> lam...
Published: 17 July 2002
Fig. 2. Chondrite-normalized rare-earth element (REE) abundances in Labrieville lamprophyres. Normalizing values are REE concentrations reported by Anders and Ebihara ( 1982 ) multiplied by 1.38, which represents a least-squares best-fit to the earlier chondrite composite data of Haskin et al
Journal Article
Published: 07 December 2005
Canadian Journal of Earth Sciences (2005) 42 (10): 1699–1718.
...- to post-tectonic ∼1060–1010 Ma andesine anorthosite belt that includes the Château-Richer, St. Urbain, and Labrieville massifs. The dominant rock type at MAT is foliated andesine anorthosite or leuconorite, and orientations of foliations indicate that the pluton has the shape of a dome. MAT contains...
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Journal Article
Journal: Economic Geology
Published: 01 July 2001
Economic Geology (2001) 96 (4): 797–815.
... the Château-Richer, Labrieville, and St. Urbain massifs in Quebec; from the Roseland massif in Virginia; and from the Carthage massif in New York. Our data set includes X-ray fluorescence (XRF) and instrumental neutron activation (INA) analyses of whole-rock samples, as well as electron-microprobe (EMP...
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F ig  4. Plot of wt percent Fe 2 O 3 (T) versus parts per
million Sc in who...
Published: 01 July 2001
F ig 4. Plot of wt percent Fe 2 O 3 (T) versus parts per million Sc in whole-rock samples of nelsonite and oxide-apatite gabbronorite. Symbols for nelsonites are explained in Figure 3 . Symbols for oxide-apatite gabbronorites are the following: STU = St. Urbain, LBV-I = Labrieville-inner, LBV-O
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F ig . 1. Photomicrographs illustrating textures of nelsonites (plane-polar...
Published: 01 July 2001
F ig . 1. Photomicrographs illustrating textures of nelsonites (plane-polarized light; each photograph covers an area of approximately 2 cm × 3 cm; white = apatite, dark = Fe-Ti oxide). A. St. Urbain–Bignell (sample STU85-692). B. Labrieville (sample LV88-116B). C. Roseland (sample RLD95-960). Note
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F ig . 2. Photomicrographs illustrating textures of oxide-apatite gabbronor...
Published: 01 July 2001
F ig . 2. Photomicrographs illustrating textures of oxide-apatite gabbronorites (plane-polarized light; each photograph covers an area of approximately 2 cm × 3 cm; black = Fe-Ti oxide, gray = pyroxene, white = plagioclase + apatite). A. St. Urbain (CHV80-205). B. Labrieville–inner (LV87-071). C
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F ig . 10. Chondrite-normalized REE plots for apatites from (A) St. Urbain,...
Published: 01 July 2001
F ig . 10. Chondrite-normalized REE plots for apatites from (A) St. Urbain, (B) Labrieville, and (C) Roseland. OAGN = oxide-apatite gabbronorites.
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F ig . 14. Calculated REE patterns for melts in equilibrium with apatite fr...
Published: 01 July 2001
F ig . 14. Calculated REE patterns for melts in equilibrium with apatite from St. Urbain, Labrieville, and Roseland. D-values are taken from Roelandts and Duchesne (1978). OAGN = oxide-apatite gabbronorites.
Journal Article
Published: 28 November 2005
Canadian Journal of Earth Sciences (2005) 42 (10): 1865–1880.
...-type Lac St. Jean Anorthositic Suite, ( iii ) a 1082–1045 Ma unnamed plutonic suite, and ( iv ) the 1020–1008 Ma andesine-type Valin Anorthositic Suite. The Valin Anorthositic Suite includes the 1016 ± 2 Ma andesine-type Mattawa Anorthosite, the 1010–1008 Ma andesine-type Labrieville Alkalic...
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Journal Article
Published: 01 November 2016
The Canadian Mineralogist (2016) 54 (6): 1563–1593.
... in similarly young, alkalic anorthosites in the Grenville Province of Québec ( e.g ., St-Urbain, Labrieville, Château-Richer, Mattawa). Such differences indicate that the Virginia anorthosites crystallized under low f O 2 conditions compared to their Québec counterparts, despite higher silica activity. We...
FIGURES | View All (19)
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Chondrite-normalized REE plot for Montpelier and Roseland samples. Data for...
Published: 01 November 2016
Fig. 12. Chondrite-normalized REE plot for Montpelier and Roseland samples. Data for Roseland from Owens & Dymek (1999) . Also shown for comparison is a field for anorthosites from the Labrieville, Québec massif ( Owens & Dymek 2001 ). Normalizing values from Boynton (1984) .
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Whole-rock normative feldspar compositions for Montpelier (A) and Roseland ...
Published: 01 November 2016
Fig. 13. Whole-rock normative feldspar compositions for Montpelier (A) and Roseland (B), with compositions of Labrieville and St-Urbain plotted for comparison (massive and gneissic varieties at Montpelier are not distinguished on A). Isotherms calculated at 5 kb using the SOLVCALC program of Wen
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Schematic representation of the system FeO–Fe 2 O 3 –TiO 2  illustrating co...
Published: 01 November 2016
Fig. 18. Schematic representation of the system FeO–Fe 2 O 3 –TiO 2 illustrating compositions of the ilmenite + rutile assemblages at Montpelier and Roseland, and typical ilmenite ss compositions at St-Urbain and Labrieville. Also shown is the experimentally determined rutile + ilmenite ss
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Total intensity aeromagnetic map of the region shown in Fig.  2 . Warm colo...
Published: 07 December 2005
Fig. 3. Total intensity aeromagnetic map of the region shown in Fig.  2 . Warm colors (red, purple) indicate high intensity; cool colors (pale green, blue) indicate lower intensity. c and b, core and border zones at Mattawa, respectively; LBV, Labrieville Anorthosite Massif; MAT, Mattawa
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Various whole-rock comparisons between Montpelier and Roseland, and the St-...
Published: 01 November 2016
Fig. 17. Various whole-rock comparisons between Montpelier and Roseland, and the St-Urbain and Labrieville, Québec, anorthosites. (A) wt.% K 2 O versus wt.% Na 2 O; (B) wt.% K 2 O versus ppm Ba; (C) wt.% K 2 O versus ppm Rb; and (D) ppm Sr versus ppm Ba.