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Matachewan Ontario

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Journal Article
Published: 01 July 1992
Canadian Journal of Earth Sciences (1992) 29 (7): 1580–1589.
... for Archean gold deposits associated with the LLCB. Along the parts of the LLCB covered by Gowganda Formation in the Matachewan area, Ontario, synsedimentary structures localized along the paleotopographic lineament of the LLCB and deformation structures due to post-Gowganda reactivation of the LLCB...
Journal Article
Published: 01 November 1991
Canadian Journal of Earth Sciences (1991) 28 (11): 1797–1811.
...Gordon F. West; Richard E. Ernst Abstract By digital image processing of federal–provincial aeromagnetic survey data for the south-central Superior Province, we have obtained an improved picture of the distribution of dykes in the huge Matachewan mafic dyke swarm (2454 Ma). We deduce from...
Series: Society of Economic Geologists
Published: 01 January 1991
DOI: 10.5382/GB.11
EISBN: 9781934969649
...Abstract Abstract The Matachewan-Kirkland Lake-Larder Lake gold-copper-ironasbestos-barite mining district is situated in Late Archean rocks of the Canadian Precambrian Shield’s Superior Province, -Abitibi sub-province, southwestern part. The structural setting seems to be comparable...
Series: Society of Economic Geologists
Published: 01 January 1991
DOI: 10.5382/GB.11
EISBN: 9781934969649
Journal Article
Published: 01 August 1990
Canadian Journal of Earth Sciences (1990) 27 (8): 1031–1039.
...T. A. Vandall; D. T. A. Symons Abstract Paleomagnetic measurements have been completed on 400 specimens from dated Archean granites and Matachewan dikes in the Michipicoten and Gamitagama greenstone belts in the western Wawa Subprovince of the Superior Province, Ontario. Detailed alternating-field...
Journal Article
Published: 01 February 1990
Canadian Journal of Earth Sciences (1990) 27 (2): 200–211.
...M. P. Bates; H. C. Halls Abstract The 2.45 Ga Matachewan dykes from the Abitibi Subprovince of the Canadian Shield yield a mean paleomagnetic pole of 42°N, 58°E (α 95 = 3°; N (sites) = 36), which is a composite of new and previously published data. Domains of paleomagnetic polarity are defined...
Journal Article
Journal: Economic Geology
Published: 01 June 1919
Economic Geology (1919) 14 (4): 281–301.
Journal Article
Journal: Economic Geology
Published: 01 August 2012
Economic Geology (2012) 107 (5): 835–857.
...V. Taranovic; C. M. Lesher; M. G. Houlé; J. H. Bédard Abstract The C zone, located in Bannockburn Township approximately 30 km W of Matachewan, Ontario, is one of several komatiite-associated Ni-Cu-(PGE) deposits within the 2710 to 2704 Ma Tisdale volcanic episode of the Abitibi greenstone belt...
FIGURES | View All (21)
Series: Society of Economic Geologists
Published: 01 January 1991
DOI: 10.5382/GB.11
EISBN: 9781934969649
...Abstract Abstract The Matachewan camp is located in the southwestern Abitibi Greenstone Belt of the Superior Province, 55 kilometres west of Kirkland Lake, northeastern Ontario. Gold production from the camp has come entirely from two contiguous mines, the Young-Davidson mine (YDM...
Journal Article
Published: 01 March 1983
Canadian Journal of Earth Sciences (1983) 20 (3): 436–461.
...John Wm. Geissman; David W. Strangway; Ann M. Tasillo-Hirt; Larry S. Jensen Abstract Iron-rich and magnesium-rich basaltic tholeiites of the latest Archean Kinojevis Group, central Abitibi Belt, northeastern Ontario, contain a natural remanent magnetization that is generally multivectorial...
Journal Article
Published: 01 January 1990
Canadian Journal of Earth Sciences (1990) 27 (1): 87–103.
...H. C. Halls; H. C. Palmer Abstract A tea-coloured cloudiness in groundmass feldspars characterizes dykes of two Early Proterozoic swarms (2.45 Ga Matachewan; 2.04 Ga Kapuskasing) that intrude amphibolite to granulite host rocks within the Kapuskasing Structural Zone (KSZ) of northern Ontario...
Journal Article
Published: 01 December 1984
Canadian Journal of Earth Sciences (1984) 21 (12): 1499–1506.
...Richard E. Ernst; Henry C. Halls Abstract Prominent north- to northwest-trending dikes (herein termed the Hearst swarm) west of the Kapuskasing Structural Zone (KSZ) in northern Ontario yield a paleomagnetic pole position of 48.6°N, 69.0°E, dm = 6.9, dp = 3.6 (60 samples from 12 dikes).Using...
Journal Article
Published: 01 August 1965
Canadian Journal of Earth Sciences (1965) 2 (4): 278–298.
... in the world. The other swarms are the Molson dykes (1 445 m.y.) in northeastern Manitoba, the Marathon dykes (1 810 m.y.) just north of Lake Superior, the Sudbury dykes (1 285 m.y.) of southeastern Ontario, the Matachewan dykes (2 485 m.y.) of western Quebec and northeastern Ontario, and the Abitibi dykes (1...
Journal Article
Journal: Economic Geology
Published: 01 August 1987
Economic Geology (1987) 82 (5): 1177–1191.
..., McIntyre-Hollinger, Macassa, Lake Shore, and Ross which are all in Ontario, Canada, and Kalgoorlie in Australia. Examples of lesser deposits are in Hislop Township and in the Matachewan area, Ontario, Canada. With the exception of Hemlo, these are quartz-carbonate vein deposits spatially and temporally...
Series: Society of Economic Geologists
Published: 01 January 2017
DOI: 10.5382/Rev.19.05
EISBN: 9781629491172
...Abstract Abstract The Larder Lake-Cadillac Break is a gold metallotect, which extends for more than 250 km from Matachewan in Ontario to Val-d’Or in Quebec. For much of its length it juxtaposes older komatiitic rocks against younger sedimentary units. Among the adjacent sedimentary rocks...
FIGURES | View All (29)
Journal Article
Published: 03 March 2004
Canadian Journal of Earth Sciences (2004) 41 (3): 255–269.
... : 1206 – 1217 . West G.F. Ernst R.E. 1991 . Evidence from aeromagnetics on the configuration of Matachewan dykes and the tectonic evolution of the Kapuskasing structural zone, Ontario, Canada . Canadian Journal of Earth Sciences , 28 : 1797 – 1811 . Zhang B. 1999...
FIGURES | View All (8)
Journal Article
Journal: Economic Geology
Published: 01 November 2002
Economic Geology (2002) 97 (7): 1577–1606.
... of the Canadian Shield near Sudbury, Ontario. The East Bull Lake intrusive suite is part of a regional Paleoproterozoic magmatic event, extending from 2.49 to 2.44 Ga, which also includes bimodal volcanic rocks, felsic plutons, and the regionally extensive Hearst and Matachewan dike swarms. This regional magmatic...
FIGURES | View All (11)
Journal Article
Published: 18 June 2001
Canadian Journal of Earth Sciences (2001) 38 (6): 963–974.
... mètres de sédiments du Clay Belt dans la région au nord de Matheson, en Ontario. Dans cette région, les roches vertes archéennes de l’Abitibi sont recoupées par au moins trois générations de dykes de diabase fortement magnétiques. L’ensemble de dykes prédominant, le Matachewan, a une direction N–S...
FIGURES | View All (7)
Journal Article
Journal: Geology
Published: 01 August 1997
Geology (1997) 25 (8): 707–710.
...Eva Zaleski; David W. Eaton; Bernd Milkereit; Brian Roberts; Matthew Salisbury; Larry Petrie Abstract A 20 km seismic reflection profile in the Superior province of northwestern Ontario imaged polydeformed Archean terrane, including the Manitouwadge greenstone belt and the adjacent Wawa-Quetico...
Image
Schematic diagram of major geological features of the Matheson area of Nort...
Published: 18 June 2001
-trending Matachewan-type diabase dykes. The towns of Matheson and Val Gagne, as well as the townships of Taylor, Carr, and Beatty, are identified. In the top right inset map, their location with respect to the town of Timmins and the townships of Harker and Holloway, Ontario, is shown.