1-20 OF 1943 RESULTS FOR

Hunter Mine

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 April 1992
Canadian Journal of Earth Sciences (1992) 29 (4): 783–792.
...Jean-Yves Labbé; Real Daigneault; Pierre A. Cousineau Abstract The Lyndhurst discontinuity is a major east–west structure located some 40 km north of Rouyn–Noranda. It separates the rhyolitic and sedimentary units of the Hunter Mine Group to the north from the basalts of the Kinojévis Group...
Journal Article
Journal: Economic Geology
Published: 01 October 1993
Economic Geology (1993) 88 (6): 1341–1358.
... to rhyodacite, with low high field strength element and relatively high REE ratios (La N /Yb N = 8-20), represented by the upper Skead Group, the Quebec Hunter Mine Group, and the Upper cycle Chibougamau rocks; and group V, mafic to felsic alkalic volcanic rocks, with high REE ratios (La N /Yb N = 12-62...
Journal Article
Journal: Economic Geology
Published: 01 November 2008
Economic Geology (2008) 103 (7): 1531–1562.
... and are associated with abundant and highly vesicular volcaniclastic rocks that display a compositional continuum from andesite to rhyolite. Other weakly mineralized FII districts (e.g., Hunter mine, Gemini-Turgeon) are characterized instead by bimodal flow-dome sequences. The FIIIa-type rhyolites occur mainly...
FIGURES | View All (12)
Journal Article
Published: 01 September 1989
Canadian Journal of Earth Sciences (1989) 26 (9): 1747–1763.
... unit of the Hunter Mine Group; 2714 ± 2 Ma for a rhyolite at the base of the mainly tholeiitic to komatiitic Stoughton–Roquemaure Group; 2701 ± 2 Ma for porphyritic rhyolite of the Blake River Group; 2701 ± 2 Ma for a tuff of the Skead Group; and for a pyroclastic unit at the base of the Larder Lake...
Image
Geological setting of the Abitibi greenstone belt and stratigraphic column showing the placement of the Hunter Mine Group (after Powell et al., 1995; Mueller and Mortensen, 2002).
Published: 01 May 2015
Figure 1. Geological setting of the Abitibi greenstone belt and stratigraphic column showing the placement of the Hunter Mine Group (after Powell et al., 1995 ; Mueller and Mortensen, 2002 ).
Image
Location of the Coeur d’Alene district and the map area inset. The map shows the location of the Lucky Friday and Gold Hunter mines and the two major structural features, the Osburn and the Placer Creek faults. Also shown are the major intrusions of this area, the Late Cretaceous Gem stocks. The Gem-Gold Hunter and Golconda-Lucky Friday mineral belts are part of a system of well-defined parallel to sub-parallel mineral belts in the Coeur d’Alene district (e.g., Fryklund 1964).
Published: 01 February 2011
F igure 2. Location of the Coeur d’Alene district and the map area inset. The map shows the location of the Lucky Friday and Gold Hunter mines and the two major structural features, the Osburn and the Placer Creek faults. Also shown are the major intrusions of this area, the Late Cretaceous Gem
Image
Simplified geologic map, showing sample and VMS deposit locations. A. Joutel (modified from Legault et al., 2002). JVC = Joutel Volcanic Complex. B. Chibougamau (modified from Daigneault and Allard, 1990). WF = Waconichi Formation. C. Normétal (upper part: modified from Lafrance et al., 2000) and Hunter (lower part: modified from Mueller and Donaldson (1992). HMG = Hunter Mine Group, NVC = Normétal Volcanic Complex. D. Quévillon area (modified from Lacroix et al., 1993).
Published: 01 November 2008
et al., 2000 ) and Hunter (lower part: modified from Mueller and Donaldson (1992) . HMG = Hunter Mine Group, NVC = Normétal Volcanic Complex. D. Quévillon area (modified from Lacroix et al., 1993 ).
Journal Article
Journal: Economic Geology
Published: 01 August 2016
Economic Geology (2016) 111 (5): 1073–1098.
... steep bedding-parallel faults and veins that link up with the arrays of low-displacement W-dipping faults. Fig. 2 Interpreted cross sections of the main Ballarat East goldfield. (A). Historic section of mine workings that illustrates the W-dipping leather jacket lodes (from Brown and Hogan, 1932...
FIGURES | View All (19)
Image
A, Generalized geological map of the Abitibi subprovince indicating the distributions of major komatiite-bearing sequences and the Northern and Southern Volcanic Zones of Chown et al. (1992). 1 = Kidd Volcanic Center; 2 = Tisdale Group; 3 = Hunter Mine Group rhyolites/Stoughton-Roquemaure Group komatiites and komatiitic basalts; 4 = Malartic Block; L=Larder Lake Group; K=Kinojevis Group; and B=Blake River Group; after Stott (1997) and Chown et al. (1992). B, Malartic Composite Block and structural domains of Desrochers et al. (1993); the possible location of the Heva Formation; Louvicourt Township; and the map area for figure 3A.
Published: 01 November 1999
Figure 1. A , Generalized geological map of the Abitibi subprovince indicating the distributions of major komatiite-bearing sequences and the Northern and Southern Volcanic Zones of Chown et al. ( 1992 ). 1 = Kidd Volcanic Center; 2 = Tisdale Group; 3 = Hunter Mine Group rhyolites
Journal Article
Journal: Economic Geology
Published: 01 May 2013
Economic Geology (2013) 108 (3): 463–482.
... to the commencement of mining and ore treatment. Domaining in the context of geometallurgy is defined as delineating volumes of material that exhibit consistent mineral processing response. Such domains are defined using a combination of mineralogy and metal deportment and are typically controlled by changes in basic...
FIGURES | View All (11)
Journal Article
Journal: Economic Geology
Published: 01 December 2005
Economic Geology (2005) 100 (8): 1565–1582.
...B. Jane Barron; L. M. Barron; G. Duncan Abstract At Bingara-Copeton in the Phanerozoic New England fold belt, New South Wales, Australia, about two million diamonds were mined from Tertiary alluvial deposits that are more than 1,500 km distant from the nearest craton. The diamonds contain unique...
FIGURES | View All (8)
Image
Regional geological map of the central Abitibi belt modified from Lacroix et al. (1990), and Lacroix and Sawyer (1995). Geochronology sample locations of six plutons are indicated. Lithostratigraphic units: CD, Chicobi domain; CaD, Cartwright domain; JRD, Joutel–Raymond domain; NLD, Normétal–Ligneris domain; NTD, north Taibi domain; SND, south Normétal domain; STD, south Taibi domain; BRG, Blake River Group; HMG, Hunter Mine Group: KIG, Kinojevis Group; MAG, Malartic Group; SRG, Stoughton–Roquemaure Group. Plutons: CoP, Colombourg; LAP, Lac Abitibi; LSP, LaSarre; PaP, Palmorolle; PoP, Poularies; TaP, Taschereau; VGP, Val St. Gilles. Faults: CBF, Casa Berardi; HF, Harricana; LF, Laberge; LyF, Lyndhurst; MF, Macamic; NCF, north Chicobi; NTF, north Taibi; DPF, Destor–Porcupine.
Published: 02 April 2000
, Normétal–Ligneris domain; NTD, north Taibi domain; SND, south Normétal domain; STD, south Taibi domain; BRG, Blake River Group; HMG, Hunter Mine Group: KIG, Kinojevis Group; MAG, Malartic Group; SRG, Stoughton–Roquemaure Group. Plutons: CoP, Colombourg; LAP, Lac Abitibi; LSP, LaSarre; PaP, Palmorolle; PoP
Journal Article
Journal: Economic Geology
Published: 01 August 2003
Economic Geology (2003) 98 (5): 865–891.
.... The principal Reliance nickel sulfide deposits are confined to flow fields in the north and west, occur within lava channel complexes (Trojan and Shangani mines, Damba-Silwane and Hunters Road prospects) and a fissure vent (Epoch mine), and include type 1 basal sequences of massive to matrix to disseminated...
FIGURES | View All (17)
Journal Article
Published: 01 May 2018
Jour. Geol. Soc. India (2018) 91 (5): 554–562.
... the European settlement 150 years ago. Currently there have been renewed human activities in the south central part of the region for coal mining, leading to clearance of vegetation and disturbance of soil. The present study addresses the issue of soil erosion in a part of Hunter Region by employing...
FIGURES | View All (8)
Journal Article
Published: 01 February 2011
American Mineralogist (2011) 96 (2-3): 261–267.
...F igure 2. Location of the Coeur d’Alene district and the map area inset. The map shows the location of the Lucky Friday and Gold Hunter mines and the two major structural features, the Osburn and the Placer Creek faults. Also shown are the major intrusions of this area, the Late Cretaceous Gem...
FIGURES | View All (7)
Series: Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.250.01.15
EISBN: 9781862394988
... based on hunter-gatherer and small-scale farming activities, with the bulk of the population residing in self-sufficient rainforest and coastal villages. Melanesians have a particularly strong cultural attachment to land, which is considered to be within the custodianship of the community at large...
FIGURES | View All (6)
Journal Article
Published: 01 May 2005
American Mineralogist (2005) 90 (5-6): 1000–1007.
... and Fe-Zn partitioning between fahlore and sphalerite, we estimate that fahlore compositions were frozen in by about 235 °C, roughly 40 °C above corresponding temperatures obtained for the Gold Hunter vein of the Lucky Friday Mine. This result and the absence of readily detectable diaphorite (~Pb 2 Ag 3...
FIGURES | View All (6)
Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2010
DOI: 10.5382/SP.15.1
EISBN: 9781629490397
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1983
AAPG Bulletin (1983) 67 (9): 1454.
..., Goonyella, Peak Downs, German Creek, Blackwater, Baralaba, Tolmeis and Moura Mines of the Bowen basin of Queensland and the unique Blair Athol mine at the far western edge of Bowen basin. In New South Wales these include the Hunter Valley area Singleton Coal Measures represented by the Foyebrook-Liddell...
Journal Article
Published: 01 September 1922
American Mineralogist (1922) 7 (9): 154–158.
...George F. Black Abstract The Schuyler Copper-mine at North Arlington, New Jersey, is believed to be the oldest in the United States. It is situated on property secured by Captain William Sanford of the British Army by a patent, issued on July 4th, 1668, conveying to him about ten thousand acres...