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Deerhorn Deposit

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(A). Geologic map of the <span class="search-highlight">Deerhorn</span> <span class="search-highlight">deposit</span>. (B). Cross section across the De...
Published: 01 November 2017
Fig. 11. (A). Geologic map of the Deerhorn deposit. (B). Cross section across the Deerhorn deposit. (C). Lithologic photos correspond to (A) volcanic sandstone, (B) plagioclase phyric andesite, (C) monzonite-D, and (D) monzonite-A.
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(A). Cross section of the <span class="search-highlight">Deerhorn</span> <span class="search-highlight">deposit</span>, showing main-stage alteration a...
Published: 01 November 2017
Fig. 15. (A). Cross section of the Deerhorn deposit, showing main-stage alteration assemblages. (B). Representative samples of the different alteration stages of the Deehorn deposit. (A) = K-silicate alteration, (B) = chlorite-epidote-pyrite alteration, (C) = illite alteration, (D) = dusty red
Journal Article
Journal: Economic Geology
Published: 01 November 2017
Economic Geology (2017) 112 (7): 1673–1717.
...Fig. 11. (A). Geologic map of the Deerhorn deposit. (B). Cross section across the Deerhorn deposit. (C). Lithologic photos correspond to (A) volcanic sandstone, (B) plagioclase phyric andesite, (C) monzonite-D, and (D) monzonite-A. ...
FIGURES | View All (27)
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(A). Total alkali silica (TAS) volcanic diagram for volcanic host rock of t...
Published: 01 November 2017
Fig. 12. (A). Total alkali silica (TAS) volcanic diagram for volcanic host rock of the Deerhorn deposit ( Le Bas et al., 1986 ). (B). TAS plutonic diagram ( Cox et al., 1979 ) for least altered intrusive host rocks of the Deerhorn deposit. (C)-(F) correspond to major oxides and trace elements
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Schematic model of the evolution of the <span class="search-highlight">Deerhorn</span> and Southeast zone <span class="search-highlight">deposit</span>...
Published: 01 November 2017
Fig. 21. Schematic model of the evolution of the Deerhorn and Southeast zone deposits. (A). Calc-alkalic volcanism deposited the plagioclase-phyric andesite after previous units of the Nicola Group. (B). Emplacement of the Takomkane batholith (specifically the Woodjam Creek unit) together
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Examples of variation diagrams for rocks of the least-a ltered intrusive ho...
Published: 01 November 2017
Fig. A2. Examples of variation diagrams for rocks of the least-a ltered intrusive host rocks of the Deerhorn deposit, using mobile and immobile elements.
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(A). Summary of the vein paragenesis in chronological order in the Southeas...
Published: 01 November 2017
Fig. 16. (A). Summary of the vein paragenesis in chronological order in the Southeast Deerhorn deposit. (B). Representative samples of (A) main-stage magnetite + quartz + chalcopyrite veins, (B) intermediate-stage quartz + chalcopyrite + pyrite vein.
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Chondrite-normalized REE abundances of the host rocks of the <span class="search-highlight">Deerhorn</span> depos...
Published: 01 November 2017
Fig. 13. Chondrite-normalized REE abundances of the host rocks of the Deerhorn deposit. For comparison the monzonite- A main values are shown to contrast with monzonite-D, plagioclase-phyric andesite and the volcanic sandstone; the same is displayed for monzonite-A, using the volcanic sandstone
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(A). Immobile trace element variation diagrams for rocks of the Southeast z...
Published: 01 November 2017
Fig. 19. (A). Immobile trace element variation diagrams for rocks of the Southeast zone, Deerhorn, and Takom deposits. Monzonite-A values can be scattered due to hydrothermal alteration. The blue in the background shows the two major lithologic clusters. (B). Chondritenormalized REE abundances
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(A).  206 Pb/ 204 Pb vs.  207 Pb/2 04 Pb and  206 Pb/ 204 Pb vs.  208 Pb/ 2...
Published: 01 November 2017
Fig. 20. (A). 206 Pb/ 204 Pb vs. 207 Pb/2 04 Pb and 206 Pb/ 204 Pb vs. 208 Pb/ 204 Pb for the Deerhorn and Southeast zone deposits. The analytical uncertainty is not plotted in the figure as it is smaller than the size of the plot symbols. Mantle, orogeny, and upper crust evolution curves
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LOI vs. K 2 O and alteration diagram (from  Davies and Whitehead, 2010 ) fo...
Published: 01 November 2017
Fig. A3. LOI vs. K 2 O and alteration diagram (from Davies and Whitehead, 2010 ) for all rocks of the Southeast zone, Deerhorn, and Takom deposits. Least altered samples and samples selected for this study are depicted as the larger icons in the diagrams.
Journal Article
Published: 09 August 2016
Geochemistry: Exploration, Environment, Analysis (2016) 16 (3-4): 213–232.
.... Glacial striations shown on the map were measured as part of this survey. Mineral occurrences are from MINFILE (2015) . The Deerhorn, Megabuck, Takom, and Spellbound zones are Cu-Au-Mo alkalic porphyry-type deposits occurring as quartz stockwork within the contact zones of satellite intrusion...
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Journal Article
Published: 10 March 2023
The Canadian Journal of Mineralogy and Petrology (2023) 61 (1): 3–29.
...-alkalic intrusions (del Real et al . 2017). The only deposits that contain TSM are DH and TK, and samples from both were examined. At Deerhorn, TSM are observed in syn- to post-ore Py-Qz-Chl±Hem±TSM veins with distinctive white halos dominated by illite (del Real et al . 2017). The TSM are found...
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Journal Article
Published: 10 March 2023
The Canadian Journal of Mineralogy and Petrology (2023) 61 (1): 31–60.
... the Deerhorn deposit (157.6 m depth). In the companion study to this ( Beckett-Brown et al . 2023 ), the textural and major/minor element characteristics of TSM from the seven porphyry systems discussed above were described and evaluated. Tourmaline should be considered a significant phase in porphyry...
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Journal Article
Published: 01 October 2016
Journal of Sedimentary Research (2016) 86 (10): 1129–1146.
...), the resulting caldera was partially filled by a large lake, within which volcaniclastic, chemical, and biogenic sediments were deposited. Contrary to previous interpretations, Long Valley Lake was initially evaporative and did not become relatively fresh and deep until later in its history. This observation...
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Journal Article
Journal: Economic Geology
Published: 01 June 2014
Economic Geology (2014) 109 (4): 827–858.
...James M. Logan; Mitchell G. Mihalynuk Abstract Paired belts of alkalic and calc-alkalic porphyry deposits are genetically linked to early Mesozoic volcanic arcs preserved as the Quesnel and Stikine terranes in western Canada. These parallel arc terranes extend for 2,000 km along the axis...
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Journal Article
Journal: SEG Discovery
Published: 01 July 2016
SEG Discovery (2016) (106): 1–64.
... Quantum Minerals Ltd., Callao 3461, Las Condes, Santiago, Chile ABSTRACT INTRODUCTION Exploration for porphyry copper Lithocaps are large rock volumes deposits beneath barren or poorly mineralized, advanced argillic originally 1 to 2 km thick and lithocaps is becoming common- place; however, there have...
Journal Article
Journal: SEG Discovery
Published: 01 April 2016
SEG Discovery (2016) (105): 1–64.
... Southeast zone), pre-accretion al- kalic type (New Afton, Copper Mountain, and Woodjam Deerhorn and Megabuck zones), and post-accretion calc-alkalic types (Huckleberry and Maggie). The geology and mineralization of these diverse deposit types will be examined; their similarities and differences, ore...
Journal Article
Journal: SEG Discovery
Published: 01 January 2016
SEG Discovery (2016) (104): 1–68.
..., and Woodjam Deerhorn and Megabuck zones), and post-accretion calc-alkalic types (Huckleberry and Maggie). The geology and mineralization of these diverse deposit types will be examined; their similarities and differences, ore reserves, mining methods, metallurgy, economics, and environmental considerations...