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1-19 OF 19 RESULTS FOR
Deerhorn Deposit
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Image
(A). Geologic map of the Deerhorn deposit. (B). Cross section across the De...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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.
Image
(A). Cross section of the Deerhorn deposit, showing main-stage alteration a...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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
Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
Irene del Real, Farhad Bouzari, Amelia Rainbow, Thomas Bissig, Jacqueline Blackwell, Ross Sherlock, John F.H. Thompson, Craig J.R. Hart
Journal: Economic Geology
Publisher: Society of Economic Geologists
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. ...
Image
(A). Total alkali silica (TAS) volcanic diagram for volcanic host rock of t...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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
Image
Schematic model of the evolution of the Deerhorn and Southeast zone deposit...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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
Image
Examples of variation diagrams for rocks of the least-a ltered intrusive ho...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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.
Image
(A). Summary of the vein paragenesis in chronological order in the Southeas...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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.
Image
Chondrite-normalized REE abundances of the host rocks of the Deerhorn depos...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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
Image
(A). Immobile trace element variation diagrams for rocks of the Southeast z...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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
Image
(A). 206 Pb/ 204 Pb vs. 207 Pb/2 04 Pb and 206 Pb/ 204 Pb vs. 208 Pb/ 2...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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
Image
LOI vs. K 2 O and alteration diagram (from Davies and Whitehead, 2010 ) fo...
in Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia
> Economic Geology
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
Till geochemistry and mineralogy: vectoring towards Cu porphyry deposits in British Columbia, Canada
Publisher: Geological Society of London
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...
Journal Article
Recognizing Tourmaline in Mineralized Porphyry Cu Systems: Textures and Major-Element Chemistry
Publisher: Mineralogical Association of Canada
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...
Journal Article
Trace Element Characteristics of Tourmaline in Porphyry Cu Systems: Development and Application To Discrimination
Publisher: Mineralogical Association of Canada
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...
Journal Article
Co-Evolution of Volcanic and Lacustrine Systems In Pleistocene Long Valley Caldera, California, U.S.A.
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
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...
Journal Article
Tectonic Controls on Early Mesozoic Paired Alkaline Porphyry Deposit Belts (Cu-Au ± Ag-Pt-Pd-Mo) Within the Canadian Cordillera
Journal: Economic Geology
Publisher: Society of Economic Geologists
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...
Journal Article
SEG Newsletter 106 (July)
Journal: SEG Discovery
Publisher: Society of Economic Geologists
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...
Includes: Supplemental Content
Journal Article
SEG Newsletter 105 (April)
Journal: SEG Discovery
Publisher: Society of Economic Geologists
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...
Includes: Supplemental Content
Journal Article
SEG Newsletter 104 (January)
Journal: SEG Discovery
Publisher: Society of Economic Geologists
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...
Includes: Supplemental Content