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Shunda Creek

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a) The Nordegg Member exposure near the <b>Shunda</b> <b>Creek</b> bridge east of Nordegg...
Published: 01 September 2018
Figure 6. a) The Nordegg Member exposure near the Shunda Creek bridge east of Nordegg, south side of Alberta highway 11 (UTM 567737 E; 5816876N); bedding orientation 220°/75°. Geologist at the shaley interval that produced Amaltheus sp. aff. Gibbosus; b) Nordegg Member with 5 bentonite beds
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1956
AAPG Bulletin (1956) 40 (2): 419.
... of part of the Pekisko and probably the Shunda. The second section follows the strike northward from Pine Creek to the Superior et al. Solomon Creek No. 1 bore hole and thence to Jasper Park (Mount Greenock), Wapiti Lake, B.C. (South Gap), and to the Amerada Crown GF 23-11 bore hole north of Sturgeon Lake...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1956
AAPG Bulletin (1956) 40 (2): 417-418.
... proposed the names Tunnel Mountain, Shunda, and Shunda and Dyson Creek as formations within the Rundle group. Later that year P. S. Warren divided the Rocky Mountain formation into Tunnel Mountain and Norquay members (unpub., 1947). L. M. Clark (AAPG, 1949) cited Beach’s formations though he did not use...
Series: AAPG Special Publication
Published: 01 January 1958
DOI: 10.1306/SV17349C16
EISBN: 9781629812441
... and the more recently amended subdivisions and new names being proposed by the Mississippian Committee for the foothills area in the vicinity of Turner Valley oil field are defined, for adjacent Plains region, in the Shell-Anglo Canadian Pine Creek well. The formation names, Bakken, Banff, Pekisko, Shunda...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1956
AAPG Bulletin (1956) 40 (2): 419-420.
... recently emended subdivisions and new names being proposed by the Mississippian Committee for the Foothills area in the vicinity of Turner Valley oil field are defined, for adjacent Plains region, in Shell-Anglo Pine Creek well. The formation names, Bakken, Banff, Pekisko, Shunda, Turner Valley, and Lower...
Journal Article
Published: 01 September 2014
Bulletin of Canadian Petroleum Geology (2014) 62 (3): 132-156.
... and to establish the chronology of associated faulting. The Gold Creek Collapse Structure formed in three stages during the Mississippian Period. The first stage occurred during deposition of the Exshaw to Shunda Formation interval. The second stage occurred during Debolt Formation deposition and the remaining...
FIGURES | View All (29)
Journal Article
Published: 01 June 1965
Bulletin of Canadian Petroleum Geology (1965) 13 (2): 229-237.
...F. A. Campbell; J. F. Lerbekmo Abstract The constituents MgO, SiO 2 , K 2 O, CaO, Fe 2 O 3 and Sr were determined in 73 carbonate samples using the X-ray fluorescence method. The weighted average composition of the Banff, Pekisko, Shunda, Turner Valley and Mount Head Formations are given in terms...
Journal Article
Published: 29 January 2003
Canadian Journal of Earth Sciences (2003) 40 (1): 45-63.
... at surface is unclear. However, several outcrops, such as those at Shunda Creek, Clearwater River, Limestone Mountain, Cadomin, and Drummond Creek (Fig.  2 ), have a thin (0.8–3.5 m), poorly exposed, highly radioactive shale at the base of the Jurassic section. This shale likely correlates to subunit 1B...
FIGURES | View All (11)
Journal Article
Published: 06 June 2008
Canadian Journal of Earth Sciences (2008) 45 (5): 577-591.
... that links with the Rainbow Paleovalley in Alberta. A third paleovalley is mapped south of the Sahtaneh River (Kyklo Creek Paleovalley) and is either a tributary to, or crosscuts the Kotcho–Hoffard Paleovalley. The Niteal Creek Paleovalley is located between the Fontas and Sikanni Chief rivers. Its geometry...
FIGURES | View All (4)
Image
a)  Amaltheus  sp. aff.  gibbosus  (Schlotheim), collected by Theodore Them...
Published: 01 September 2018
Figure 4. a) Amaltheus sp. aff. gibbosus (Schlotheim), collected by Theodore Them and Rowan Martindale in the shaley bed, about 7.35–7.75 m above the base the Nordegg Member at the Shunda Creek bridge locality ( Fig. 6a , near standing figure). Royal Tyrrell Museum of Palaeontology specimen
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1963
AAPG Bulletin (1963) 47 (6): 1176-1189.
....; Pembina-Willesden Green, Medicine Hat, Swan Hills-Alberta; Boundary Lake, Milligan Creek-B.C. II. E xploratory M ethods Expenditures up $4 million (1.5%) to $261 MM. Seismic down 9 mos. (1.5%) to 604 Mos. Gravity down 12 Mos. (50%) to 11 Mos. Surface Mapping down 69 Mos. (27%) to 191 Mos. III. P roduction...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 January 2001
AAPG Bulletin (2001) 85 (1): 51-84.
... River arch and includes major fields such as Tangent, Teepee, and Gold Creek. Ironically Parkland itself owes little of its production to hydrothermally dolomitized carbonates; instead, most of the reservoir pore volume can be attributed to microintercrystalline porosity within a pervasive replacement...
FIGURES | View All (27)
Image
Debolt Isopach Map. Not all contours are labeled in tightly contoured regio...
Published: 01 September 2014
Figure 14 Debolt Isopach Map. Not all contours are labeled in tightly contoured regions. Maximum contour value is 320 m in the Gold Creek Collapse Structure core. Contour interval is 20 m. Only Shunda penetrations are displayed.
Image
Schematic cross-section at the end of Stage One of the formation of the Gol...
Published: 01 September 2014
Figure 21b Schematic cross-section at the end of Stage One of the formation of the Gold Creek Collapse Structure. At the end of Shunda time, the Leduc reef interior had undergone modest differential compaction. Minimum depth of burial of the Leduc reef at the beginning of stage one
Journal Article
Published: 01 September 2018
Bulletin of Canadian Petroleum Geology (2018) 66 (3): 595-622.
...Figure 6. a) The Nordegg Member exposure near the Shunda Creek bridge east of Nordegg, south side of Alberta highway 11 (UTM 567737 E; 5816876N); bedding orientation 220°/75°. Geologist at the shaley interval that produced Amaltheus sp. aff. Gibbosus; b) Nordegg Member with 5 bentonite beds...
FIGURES | View All (9)
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1963
AAPG Bulletin (1963) 47 (10): 1813-1827.
... in the Mount Head area (1958) and Raasch in the Storm Creek and King Creek areas ( Raasch, 1958 ). Raasch’s King Creek section is separated by a major thrust from the McConnell thrust block, and is itself separated by another thrust from the Storm Creek section. The Exshaw section ( Moore, 1958 ) lies...
FIGURES | View All (17)
Journal Article
Published: 01 March 2005
Bulletin of Canadian Petroleum Geology (2005) 53 (1): 67-83.
... cross-section from Tika Creek to Twisted Mountain, which transects the northwestern portion of the map area of this study (Fig. 5 ). The cross-section illustrates a number of important east–west stratigraphic relationships. Fig. 4. Regional map showing the location of the stratigraphic cross...
FIGURES | View All (25)
Series: GSA Field Guide
Published: 01 January 2017
DOI: 10.1130/2017.0048(01)
... trench ( Lithoprobe Geoscience Project, 1995 ). Simony and Carr (2011) document the timing of emplacement of fault-bounded basement slices above ductile shear zones of the Gwillam Creek shear zone, Monashee décollement, sub-Monashee décollement, and Eocene basal detachment in the Omineca belt...
FIGURES | View All (53)
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1961
AAPG Bulletin (1961) 45 (11): 1810-1846.
FIGURES | View All (27)
Journal Article
Journal: GSA Bulletin
Published: 17 August 2018
GSA Bulletin (2019) 131 (1-2): 318-334.
... is the lack of syndepositional zircon in the most cratonward location of the Cadomin Formation from Shunda Creek (sample 3), consistent with a lack of input from presumed western sources. The relatively large number of discordant analyses (∼600) in our data set are evaluated in an attempt to extract...
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