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Siksikpuk Formation

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—Typical bedding character of bedded chert in <span class="search-highlight">Siksikpuk</span> <span class="search-highlight">Formation</span> of DeLong...
Published: 01 March 1982
FIG. 7 —Typical bedding character of bedded chert in Siksikpuk Formation of DeLong Mountains, although most sections are not as well exposed. Chert beds are 5 to 15 cm thick. Siksikpuk Formation here depositionally overlies light-gray carbonate rocks of Lisburne Group exposed in hill
Journal Article
Journal: Economic Geology
Published: 01 November 2004
Economic Geology (2004) 99 (7): 1385–1414.
... Lisburne Group (Kuna Formation, unnamed drowned shelf facies), and the Pennsylvanian-Permian Siksikpuk Formation. Major base metal sulfide deposits of the region are present only in the Kuna Formation, which in the Red Dog district comprises siliceous black shale and black chert, minor limestone...
FIGURES | View All (12)
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1982
AAPG Bulletin (1982) 66 (3): 348–362.
...FIG. 7 —Typical bedding character of bedded chert in Siksikpuk Formation of DeLong Mountains, although most sections are not as well exposed. Chert beds are 5 to 15 cm thick. Siksikpuk Formation here depositionally overlies light-gray carbonate rocks of Lisburne Group exposed in hill...
FIGURES | View All (10)
Journal Article
Journal: Economic Geology
Published: 01 August 2015
Economic Geology (2015) 110 (5): 1143–1156.
..., Kanayut Conglomerate, and Kayak Shale. Overlying rocks consist of the Carboniferous-Jurassic Etivluk Group, marine-shelf siliciclastic strata that locally include shales and cherts of the Siksikpuk Formation and shales, cherts, and limestones of the Otuk Formation. † Corresponding author: e...
FIGURES | View All (8)
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1962
AAPG Bulletin (1962) 46 (12): 2174–2198.
... of Pennsylvanian(?) and Permian age), 0–1,400 feet thick, overlies the Alapah with probable disconformity. The Siksikpuk Formation (Lower(?) Permian), is more than 600 feet thick and consists mostly of shale. It rests unconformably on the Wahoo Limestone at Galbraith Lake and on the Alapah Limestone west...
FIGURES | View All (7)
Image
F ig . 8. Plots of C organic  vs. Cr (A), C organic  vs. Pd (B), Al 2 O 3  ...
Published: 01 November 2004
F ig . 8. Plots of C organic vs. Cr (A), C organic vs. Pd (B), Al 2 O 3 vs. Ba (C), P 2 O 5 vs. Cu (D), P 2 O 5 vs. La (E), and P 2 O 5 vs. Ce/Ce* (F) in clastic rocks of the Endicott Group, Kuna Formation, drowned shelf facies of the Lisburne Group, and Siksikpuk Formation. Ce/Ce
Image
F ig . 6. A. Plot of C organic  vs. S in clastic rocks of the Endicott Grou...
Published: 01 November 2004
F ig . 6. A. Plot of C organic vs. S in clastic rocks of the Endicott Group, Kuna Formation, drowned shelf facies of the Lisburne Group, and Siksikpuk Formation. B. Detail of A showing field for sulfate- and iron-limited sediments, and regression line for normal oxidized marine sediments ( Berner
Image
—Kuna <span class="search-highlight">Formation</span> and Etivluk Group in fenster at headwaters of Kuna River. K...
Published: 01 March 1982
FIG. 3 —Kuna Formation and Etivluk Group in fenster at headwaters of Kuna River. Kuna Formation (ℙMk) is depositionally overlain by Siksikpuk Formation ( R ¯ Ps ) , Otuk Formation ( J R ¯ 0 ) , and undifferentiated Cretaceous rocks (Ku). High ridges are formed
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F ig . 5. A. Ternary (CaO + Na 2 O) 40 -Al 2 O 3 -(K 2 O) 40  plot of whole...
Published: 01 November 2004
F ig . 5. A. Ternary (CaO + Na 2 O) 40 -Al 2 O 3 -(K 2 O) 40 plot of whole-rock analyses of clastic rocks of the Endicott Group, Kuna Formation, drowned shelf facies of the Lisburne Group, and Siksikpuk Formation calculated on a carbonate- and apatite-free basis. B. (CaO + MgO)-(Al 2 O 3 ∞ 10 2
Image
—Eastward view of north-dipping Kayak Shale (Mk), Kuna <span class="search-highlight">Formation</span> (PAAk), Si...
Published: 01 March 1982
FIG. 6 —Eastward view of north-dipping Kayak Shale (Mk), Kuna Formation (PAAk), Siksikpuk Formation ( R ¯ Ps ) , and Otuk Formation ( J R ¯ 0 ) along upper Otuk Creek at Endicott Mountain front. Late Devonian Kanayut Conglomerate (Dk) forms Endicott Mountains
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—Geologic map of Mount Doonerak area.  TrPCs , Kayak Shale and Lisbume Grou...
Published: 01 June 1976
Fig. 4 —Geologic map of Mount Doonerak area. TrPCs , Kayak Shale and Lisbume Group (Carboniferous), lower part of SadlerocUt Group and Siksikpuk Formation (Permian), and minor amount of Shublik Formation (Triassic). De, Devonian part of Endicott Group, Kanayut Conglomerate, and Hunt Fork Shale
Image
F ig . 3. Generalized stratigraphic column (modified from  Young, 2004 ) an...
Published: 01 November 2004
and Siksikpuk Formations comprise dominantly chert and shale, Ikalukrok unit comprises shale and mudstone with interbedded carbonate, Kivalina unit comprises calcareous shale, Kayak Shale comprises sandstone, shale, and limestone, and Kanayut Conglomerate comprises conglomerate, sandstone and minor shale.
Image
F ig . 6. Comparative stratigraphy of the Wolverine Creek, Red Dog, and Key...
Published: 01 November 2004
F ig . 6. Comparative stratigraphy of the Wolverine Creek, Red Dog, and Key Creek plates in the Red Dog district, by use of key from Figure 5 . There may be a disconformity beneath the Siksikpuk Formation in the Wolverine Creek plate. The general stratigraphic range of concordant mineralization
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F ig . 9. Chondrite-normalized REE plots of selected samples from major str...
Published: 01 November 2004
facies of the Lisburne Group (including siliceous mudstone). D. Bedded siliceous rock, limestone (mostly calcareous radiolarite), and lithic turbidite of the Kuna Formation. E. Phosphate nodule and phosphorite of the Lisburne Group. F. Shale, siltstone, and chert of the Siksikpuk Formation. Chondrite
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F ig . 12. Tectonic discriminant diagrams (after  Bhatia and Crook, 1986 )....
Published: 01 November 2004
rocks of the Kuna Formation include black shale, siliceous black shale and siliceous mudstone, chert, bedded siliceous rock, and lithic turbidite. Samples of the Endicott Group and Siksikpuk Formation include shale, sandstone, and siltstone. Data for average I-, S-, and A-type granites (X inside an open
Image
F ig . 8. North American apparent polar wander path of  Van der Voo (1993) ...
Published: 01 November 2004
F ig . 8. North American apparent polar wander path of Van der Voo (1993) from ~400 Ma to present showing the pole positions for characteristic remanent magnetization B (circles), the sill (star) and the maroon Siksikpuk Formation (diamonds) surrounded by their cones of 95 percent confidence
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F ig . 5. Stereonet of site means (~10 specimens per site) for
the two igne...
Published: 01 November 2004
F ig . 5. Stereonet of site means (~10 specimens per site) for the two igneous intrusion sites (squares, sites 29 and 30) and the two maroon Siksikpuk Formation sites (circles, sites 32 and 33). Plotting conventions as in Figure 4. Notice that sites 32 and 33 are similar to each other but distinct
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F ig . 1. Simplified stratigraphic column for the Red Dog district showing
...
Published: 01 November 2004
to black calcareous shale; in the Ikalukrok unit of the Kuna Formation are black shale and siliceous mudstone, black chert, and gray calcareous radiolarite (limestone); in the Siksikpuk Formation are gray shale, maroon, red, and green siltstone, and gray chert; in the Otuk Formation are gray and black
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1985
AAPG Bulletin (1985) 69 (4): 671.
... formation of the Lisburne Group; and Permian Siksikpuk Formation and Triassic Otuk formation of the Etivluk group. Lower Cretaceous coquinoid limestone and, in some places, orogenic sediments of the Okpikruak Formation cap the allochthon. Total stratigraphic thickness of the Endicott Mountains allochthon...
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F ig . 11. A. Th/Sc vs. Eu/Eu* plot showing the relationship of Brooks Rang...
Published: 01 November 2004
, siliceous black shale and siliceous mudstone, chert, bedded siliceous rock, and lithic turbidite. Samples of the Endicott Group and Siksikpuk Formation include shale, sandstone, and siltstone. Boundaries between fields are approximations only. CAB = average calc-alkaline basalt ( Pearce, 1982 ), DSFLG