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Phantom Lake Metamorphic Suite

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Journal Article
Published: 01 October 1979
Rocky Mountain Geology (1979) 17 (2): 111-133.
Journal Article
Published: 12 January 2007
Canadian Journal of Earth Sciences (2006) 43 (10): 1557-1577.
...A. Kate Souders; A. Kate Souders; Carol D. Frost Abstract The 2.68 Ga Phantom Lake metamorphic suite of the Sierra Madre is a volcanogenic, volcaniclastic, and siliciclastic sequence that may have been deposited on or near the margin of the Wyoming Province or, alternatively, it may represent part...
FIGURES | View All (10)
Journal Article
Journal: GSA Bulletin
Published: 01 November 1983
GSA Bulletin (1983) 94 (11): 1257-1274.
...KARL E. KARLSTROM; ANDREW J. FLURKEY; ROBERT S. HOUSTON Abstract Metasedimentary rocks in the Medicine Bow Mountains and Sierra Madre are divided into four groups. The > 3-km-thick Phantom Lake Metamorphic Suite contains strongly deformed metavolcanic and metasedimentary rocks that are crosscut...
Journal Article
Journal: Economic Geology
Published: 01 June 2016
Economic Geology (2016) 111 (4): 849-875.
... is primarily a biotite (± hornblende) granodiorite that was emplaced at 1866 ± 4 Ma (U/Pb zircon, Stern and Lucas, 1994 ) in sharp discordant contact with the volcanic rocks. Two younger suites of intrusions, the Boundary and Phantom Lake intrusions ( Fig. 2 ), cut across both volcanic rocks and Missi...
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Journal Article
Published: 03 September 2009
Canadian Journal of Earth Sciences (2009) 46 (7): 481-508.
... in thickness; thicknesses are commonly exaggerated because of dilation by mafic sills. Along the west side of Louis Lake and continuing south to the east side of Phantom Lake, the mafic tuff is locally strongly epidote–quartz-altered and contains sporadic sulphide mineralization marked by prominent iron...
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Journal Article
Published: 03 September 2009
Canadian Journal of Earth Sciences (2009) 46 (7): 509-527.
...) = +8.5–+9.6, and 204 Pb/ 206 Pb = 23.9. The basaltic flows that dominate the Hidden formation have Nb/Th mn = 0.16–0.29, εNd (1.9Ga) = +1.7–+4.4, εHf (1.9Ga) = +7.0–+11.8 and 204 Pb/ 206 Pb = 16.9–18.6). The Carlisle Lake basaltic–andesite (top of Hidden formation) is characterized by Nb/Th mn = 0.16...
FIGURES
Journal Article
Published: 10 February 2000
Canadian Journal of Earth Sciences (2000) 36 (11): 1767-1788.
... tuff, flows: higher Zr/Ti, REE, and HFSE than rhyolites associated with tholeiitic and calc-alkaline arc suites Few if any associated rhyolites Synvolcanic intrusions Large, multiphase, tonalitic, shallow synvolcanic intrusions (e.g., Snow Lake) coeval with volcanic rocks Locally abundant...
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Journal Article
Published: 10 February 2000
Canadian Journal of Earth Sciences (2000) 36 (11): 1807-1827.
... Lake tonalite FF92-5 Tonalite Igneous 2518 7 4 2 David and Syme 1994 Athapapuskow granite FF92-16 Granite Igneous 2553 6 6 1 This study Evolved arc Mystic Lake intrusive suite 9023-0053 Quartz diorite Igneous 1883 4 4 9 Heaman et al. 1992 Athapapuskow (West...
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Journal Article
Journal: Economic Geology
Published: 01 June 2016
Economic Geology (2016) 111 (4): 817-847.
... characteristics similar to those of postvolcanic 1839 Ma Phantom dike suite intrude the Footwall Basaltic unit (drill core TX1515; Fig. 4 ) (cf. Lafrance et al., 2016 ; this study). All lithostratigraphic units at the Trout Lake deposit underwent greenschist facies metamorphism and polyphase synvolcanic...
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Journal Article
Journal: Economic Geology
Published: 01 June 2016
Economic Geology (2016) 111 (4): 877-901.
... are intruded by the ca. 1.84 Ga late successor arc mafic to ultramafic Boundary and bimodal Phantom intrusive suites ( Fig. 2 ; Stern et al., 1999 ). The deformation history recorded in outcrops in the Flin Flon mining district has been the subject of numerous studies ( Stockwell, 1960 ; Bailes and Syme...
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Image
Rare-earth element (REE) patterns for Archean rocks of the Sierra Madre. (A...
Published: 12 January 2007
Fig. 4. Rare-earth element (REE) patterns for Archean rocks of the Sierra Madre. (A) Jack Creek quartzite, (B) Silver Lake metavolcanics, (C) Bridger Peak quartzite (all are all members of the Phantom Lake metamorphic suite, and (D) granitoids and gneiss.
Journal Article
Published: 17 June 2005
Canadian Journal of Earth Sciences (2005) 42 (4): 685-706.
... ca. 1770 Ma ( Bickford et al. 1987 ; Chiarenzelli 1989 ; Wortman et al. 1999 ) post-collisional granites and pegmatites, collectively termed the Jan Lake suite in the central Reindeer Zone, are also affected by the youngest phase of folding. Post-metamorphic uplift along late and (or) reactivated...
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Journal Article
Published: 22 December 2006
Canadian Journal of Earth Sciences (2006) 43 (10): 1445-1466.
..., transects the Sacawee block and was studied at two locations, the Beulah Belle Lake area and West Sage Hen Rocks. U–Pb analyses of magmatic zircon from a sheared amphibolite within the high-strain zone of the Beulah Belle Lake area constrain the age of the Neoarchean deformation to be later than 2688 ± 5 Ma...
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Journal Article
Published: 09 June 2005
Canadian Journal of Earth Sciences (2005) 42 (4): 723-740.
..., diabase 1840±2 11, 105 83.5 59.5 12.3 12.6 2 BP P Phantom Lake: granodiorite, granite 1837±3 7, 72 86.6 66.6 8.5 8.8 2 BP Boot–Phantom pluton 1839±3 18, 177 84.6 62.4 7.9 8.0 2 CA Clearwater complex: gabbro, anorthosite 1878±39 8, 114 48.2 6.5 2.2 3.7 3 DGd...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2017
GSA Bulletin (2017) 129 (3-4): 259-280.
... and recycling deserves to be studied closely. We present geologic, petrologic, geochemical, and isotopic descriptions of Paleoarchean gneisses in the central Wyoming Province. We identify two groups of gneisses: a bimodal suite of amphibolite and tonalite-trondhjemite-granodiorite (TTG) layered gneisses (3385...
FIGURES
Image
Inferred tectonic settings for Archean rocks of the Sierra Madre and adjace...
Published: 12 January 2007
) Intrusions in the Sierra Madre and at Bradley Peak coinciding with deposition of the Phantom Lake metamorphic suite and the Miners Delight Formation at South Pass ca. 2.67–2.69 Ga. (C) Ca. 2.65 Ga plutonism in both the Granite Mountains and the Sierra Madre. (D) Tectonic shortening within the oceanic arc
Journal Article
Journal: Economic Geology
Published: 01 June 2016
Economic Geology (2016) 111 (4): 963-1000.
... metamorphic grade increases from mid- to upper greenschist from south to north, toward the Kisseynew belt. A prehnite-pumpellyite isograd exists on the east side of the Burley Lake fault (outside of Fig. 3 ) and 1.5 km south of the 1.9 Mt Schist-Mandy precious metal-rich Cu-Zn VMS deposits within the Flin...
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Journal Article
Published: 10 February 2000
Canadian Journal of Earth Sciences (2000) 36 (11): 1917-1938.
... the Amisk Lake and Athapapuskow domains. The Athapapuskow Lake shear zone (ALSZ) separates the Athapapuskow Domain from the Namew gneiss complex to the east, and metamorphic studies indicate that the offset on the ALSZ in the area of Athapapuskow Lake is 10–15 km ( Syme 1988 ; Leclair et al. 1997...
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Journal Article
Published: 01 January 2012
Rocky Mountain Geology (2012) 47 (1): 1-35.
... of similarities between outcrop characteristics, structural style, and comparison of detrital zircon age spectra, we correlate the two southern localities with a regional suite of quartzite successions deposited ca. 1.70 Ga following the culmination of the Yavapai orogeny. The northern succession represents...
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Image
(A) Initial ε Nd  versus time for supracrustal rocks (filled symbols) from ...
Published: 12 January 2007
Fig. 10. (A) Initial ε Nd versus time for supracrustal rocks (filled symbols) from the South Pass, Rattlesnake Hills, Bradley Peak suites (this study), and the Phantom Lake metamorphic suite of the Sierra Madre ( Souders and Frost 2006 ). Also plotted are data for samples of granitoid plutons