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Phantom Lake 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; 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 of an exotic...
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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...
Image
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.
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.
Image
Tectonic assemblage map of the central portion of the Amisk collage, showing tectono-stratigraphic assemblages (e.g., Flin Flon, Birch, W. Amisk) and location of geochronological samples reported in this paper. Shear zones: AP–SZ, S. Athapapuskow; IA–SZ, Inlet Arm; IK–SZ, Iskwasoo; MD–SZ, Meridian – West Arm; ML–SZ, Mystic Lake; MO–SZ, Mosher Lake; NE–SZ, Northeast Arm. Plutons: AN, Annabel Lake pluton; BD, Boundary Intrusions; BP, Boot–Phantom pluton; CF, Cliff Lake pluton; KM, Kaminis Lake pluton; LX, Lynx Lake pluton MK, Mikanagan Lake Sill; NS, Neso Lake pluton; RY, Reynard Lake pluton. Successor basins: MA, Missi suite Athapapusko basin; MF, Missi suite Flin Flon basin; SL, Schist Lake basin. FF, town of Flin Flon.
Published: 10 February 2000
, Meridian – West Arm; ML–SZ, Mystic Lake; MO–SZ, Mosher Lake; NE–SZ, Northeast Arm. Plutons: AN, Annabel Lake pluton; BD, Boundary Intrusions; BP, Boot–Phantom pluton; CF, Cliff Lake pluton; KM, Kaminis Lake pluton; LX, Lynx Lake pluton MK, Mikanagan Lake Sill; NS, Neso Lake pluton; RY, Reynard Lake pluton
Image
Inferred tectonic settings for Archean rocks of the Sierra Madre and adjacent parts of the southern Wyoming Province. (A) Deposition of the Vulcan Mountain metavolcanics, Bradley Peak greenstone, and the McDougall Gulch metavolcanics ca. 2.71–2.72 Ga, possibly as a single arc complex. (B) 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 setting and obduction of the Rattlesnake Hills terrane onto the Wyoming (WY) craton ca. 2.65–2.63 Ga. This coincides with plutonism in both the Granite Mountains and the Wind River Range.
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
Image
(A) Initial εNd 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 that intrude these sequences (open symbols). The dominantly juvenile nature of these supracrustal belts is indicated by their mostly positive initial εNd values. The Nd isotopic compositions of samples of the Louis Lake batholith and Circle Bar granites of the Wind River Range and Rattlesnake Hills, respectively, extend to negative initial εNd values and are interpreted to have assimilated some of the older Wyoming Province crust they intrude. The plutons intruding the Bradley Peak and Sierra Madre successions show no displacement towards the composition of Wyoming Province crust, and therefore may have been emplaced in an oceanic or juvenile arc setting. (B) Initial εNd versus time for the isotopically juvenile supracrustal rocks shown in (A) compared with Nd isotopic compositions for other supracrustal belts of the southern Wyoming Province. Source: Koesterer et al. (1987), Frost et al. (1998), Patel et al. (1999), Kruckenberg et al. (2001), Souders and Frost (2006), Grace et al. (2006), C.D. Frost et al. (2006), and this study.
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
Journal Article
Journal: Economic Geology
Published: 01 June 2016
Economic Geology (2016) 111 (4): 849–875.
... to that of the two felsic suites of intrusions, the 1839 Ma Phantom Lake (06-FF-12) and 1866 Ma Annabel Lake intrusions (08-FF-22). Dike 08-FF-07 (see Fig. 4 for location) is isoclinally folded and strongly lineated along the west limb of the Hidden Lake syncline. Dike 08-FF-07 (see Fig. 2 for location...
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Journal Article
Published: 12 January 2007
Canadian Journal of Earth Sciences (2006) 43 (10): 1533–1555.
...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...
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Journal Article
Published: 03 January 2022
American Mineralogist (2022) 107 (1): 82–91.
...David London Abstract The K/Cs ratios of K-feldspars from granitic pegmatites are compared to models derived from the Rayleigh equation. The K/Cs and K/Rb ratios of K-feldspars and micas exhibit decreasing values when plotted against their Cs or Rb contents across cogenetic suites of granites...
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Journal Article
Published: 01 June 2000
Canadian Journal of Earth Sciences (2000) 37 (6): 913–922.
...; HLB, Hanson Lake block. Dots and star show locations of paleomagnetic collections, with those referred to in the text labelled as follows: BI, Big Island gneiss dome; BP, Boot-Phantom granites; DL, Davin Lake pluton; HP, Hanson Lake pluton; LL, Lynn Lake gabbro pipes; MC, Macoun Lake pluton; RE...
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Journal Article
Published: 09 June 2005
Canadian Journal of Earth Sciences (2005) 42 (4): 723–740.
... 65.2 12.1 12.2 1 BPb Boot Lake: gabbro–diorite, 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...
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Journal Article
Journal: Economic Geology
Published: 01 June 2016
Economic Geology (2016) 111 (4): 963–1000.
... syncline, RLF = Ross Lake fault, RWF = Railway fault, TC = 777-Callinan dike swarm. Fe-Ti basalt occurrences: 1 = 1920 unit, 2 = Flin Flon pit, 3 = Phantom, 4 = Reservoir, 5 = South Main. Localities used in text: A = Sipple Hill, B = subsidence structure. The prolific 1.9 to 1.84 Ga Flin Flon belt...
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Journal Article
Published: 01 February 2022
Russ. Geol. Geophys. (2022) 63 (2): 125–136.
...O.V. Lunina; A.A. Gladkov Abstract —We present materials of aerial photography of Cape Rytyi, a unique and most mysterious place on the northwestern shore of Lake Baikal. Photogrammetric survey was carried out using a DJI Phantom 4 Pro V2.0 UAV and provided an orthophoto and a digital terrain model...
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Journal Article
Journal: Geophysics
Published: 14 November 2011
Geophysics (2011) 76 (5): P11–P21.
... are the integer-valued scaled seismic data at the ( p , q ) and ( p + Δ p , q + Δ q ) CDP locations and the delta function, δ ( ξ ) = 1 if ξ = 0 and 0 otherwise. We choose a suite of offsets Δ p and Δ q to represent repetitive patterns...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2009
GSA Bulletin (2009) 121 (1-2): 247–264.
... before analysis. During the southward growth of Laurentia, thick (1–2 km) successions of quartz sandstone were deposited within the orogenic belts. Some of the best examples of these deposits are exposed in the Lake Superior region of the northern United States (Baraboo interval; Dott, 1983...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1975
AAPG Bulletin (1975) 59 (3): 486–509.
... distribution of megacyclothems that contain marine black shales or phantom black shales (†); limestone formations that nucleate these megacyclothems are named; (*) marks formations in which megacyclothem members were designated by Weller (1958) ; Moore (1949) designated all others. Complete megacyclothem...
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Journal Article
Published: 10 October 2003
Canadian Journal of Earth Sciences (2003) 40 (10): 1357–1374.
... reverse the broadly southward younging of supracrustal rocks described above. The Vulcan Mountain metavolcanic suite and lower Phantom Lake metamorphic suite are intruded by the Spring Lake granodiorite ( Houston et al. 1993 ), which has been dated at 2.71 Ga ( Premo and Van Schmus 1989...
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Journal Article
Published: 10 February 2000
Canadian Journal of Earth Sciences (2000) 36 (11): 1807–1827.
..., Meridian – West Arm; ML–SZ, Mystic Lake; MO–SZ, Mosher Lake; NE–SZ, Northeast Arm. Plutons: AN, Annabel Lake pluton; BD, Boundary Intrusions; BP, Boot–Phantom pluton; CF, Cliff Lake pluton; KM, Kaminis Lake pluton; LX, Lynx Lake pluton MK, Mikanagan Lake Sill; NS, Neso Lake pluton; RY, Reynard Lake pluton...
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Journal Article
Journal: Geophysics
Published: 04 January 2024
Geophysics (2024) 89 (1): 1JF–4JF.
..., and a caldera lake bottom, and to quantitatively estimate the volume fractions of melt and fluid in the subsurface of the Quaternary volcanic system. The authors not only provide scientific clues to the urgency and scale of future volcanic eruptions from the melt distribution but also detect an interesting...