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Callum Creek Fault

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Journal Article
Published: 01 March 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (1): 1–13.
... and is the main upper detachment of the triangle zone. Strike seismic lines reveal evidence of major lateral ramps and folding of the Big Coulee Fault. Backthrusts above the upper detachment ( e.g. Co-op, Waldron and Callum Creek) die out southward near Crowsnest River and folding of these faults decreases...
Journal Article
Published: 01 June 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (2): 195–201.
... within Paleozoic arbonate strata carried in thrust- faulted structures. These include the Pincher Creek, Waterton and Sorge fields. At surface, the region across the triangle zone is that of subdued relief, with Upper Cretaceous clastic strata exposed mainly along drainage banks. Farther west, relief...
Journal Article
Published: 01 June 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (2): 269–281.
..., the Willson Creek, Limestone Mountain (labelled on Fig. 1), Limes and Ram (both north of Fig. 1) fields are excellent examples of footwall-ramp-col lapse duplexes related to the Brazeau Thrust. The easternmost mappable thrust fault of the southern Alberta Foothills is commonly foreland-dipping and forms...
Journal Article
Published: 01 June 1993
Bulletin of Canadian Petroleum Geology (1993) 41 (2): 232–243.
... of Bluff Mountain and the geomorphology of the valley of Gold Creek. THE FAULT AT BLUFF MOUNTAIN Norris (1955, 1989) mapped a fault along the east side of Bluff Mountain which he correlated with the Turtle Mountain thrust. However, this correlation involves an anomaly. In Section 13, Township 8, Range 4, W...
Journal Article
Published: 01 September 1995
Bulletin of Canadian Petroleum Geology (1995) 43 (3): 320–342.
... and other unnamed faults (Price, 1962). Carbondale tributary is delineated from Crowsnest Channel by non-conglomeratic l thologies occurring between the two channels and a slightly different paleocurrent trend than Crowsnest Channel. Channel widths vary from 220 m wide at Screwdriver Creek to the -22 km...
Journal Article
Journal: GSA Bulletin
Published: 01 March 2011
GSA Bulletin (2011) 123 (3-4): 507–533.
... strata is well constrained near the Canada-U.S. border, where 94–96 Ma plutons crosscut the St. Mary and Hall Lake thrusts ( Price and Sears, 2000 ). In northwestern Montana, the Moyie fault deformed the margin of the 71 Ma Dry Creek stock ( Fillipone and Yin, 1994 ), but earlier episodes of slip along...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1959
AAPG Bulletin (1959) 43 (5): 992–1025.
... in the foothills is the weak sequence of shale, siltstone, coal, and sandstone comprising the Fernie and Kootenay formations. At least four major thrusts (Mill Creek, Livingstone, Bear Creek, and Dyson Mountain faults) and many minor ones have reached the surface in these beds. Moreover, in numerous wells...
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Journal Article
Published: 01 September 2001
Bulletin of Canadian Petroleum Geology (2001) 49 (3): 408–425.
... ). Southwest of Calgary, the McConnell thrust sheet is divided into three segments by the Stony Creek and Fullerton tear faults (Fig. 1 ). Paleozoic strata form the dominant level of exposure in the McConnell thrust sheet from its northern termination east of Jasper to the Stoney Creek Fault. South...
FIGURES | View All (17)
Image
Reinterpretation of seismic reflection data originally interpreted by  Lawt...
Published: 01 December 2001
Formation, M = Mississippian, BCF = Big Coulee Fault, CF = Co-op Fault, WF = Waldron Fault, CCF = Callum Creek Fault. Seismic line location indicated in Figures 5 and 8 . Top: migrated uninterpreted section. Bottom: interpreted section. See text for discussion.
Journal Article
Published: 01 August 1977
Bulletin of Canadian Petroleum Geology (1977) 25 (4): 842–867.
.... A third thrust, the Mill Creek fault, involving displacement of mainly Upper Cretaceous trata, is also traceable for a considerable distance. The objective of this paper is a synthesis of the Upper Cretaceous tratigraphy and micropaleontology of the Crowsnest Pass - Waterton area of the southern Alberta...
Journal Article
Published: 01 September 1966
Bulletin of Canadian Petroleum Geology (1966) 14 (3): 337–381.
... published by Robertson (1963) revealed the presence of an intra-base- ment reflection dipping from 7.5 km depth in the east to 14 km dept h in the west . The Pincher Creek structure is rather obscure on this section, du e to the small throw on the fault (between 500 and 1,000 feet) . The struc- ture...
Journal Article
Published: 01 June 1973
Bulletin of Canadian Petroleum Geology (1973) 21 (2): 153–177.
... Maycroft Till is overlai n by Maunsell Till near the latter's terminal zone in the vicinity of the Old - man River and Callum Creek confluence . In the Foothills of the northern part of the study area, the Laurentide ice blocked drainage from the west and formed a proglacial lake in th e Willow Creek...
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1951
AAPG Bulletin (1951) 35 (11): 2316–2347.
..., as well as an excellent summary of the history of work concerning folded faults in Alberta. Also published in 1950 is a memoir by Douglas (5) on the Callum Creek, Langford Creek, and Gap map-areas, and a map by the same author (6) of the Mount Head area, both concerning the southern foothills...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 November 2011
AAPG Bulletin (2011) 95 (11): 1821–1849.
...-trending tear faults that are kinematically linked to slip on the underlying Livingstone thrust. The four cross-strike discontinuities that occur in the study area ( Figure 3 ) separate the LRA into five distinct segments, four of which were mapped in detail during this study. The Green Creek–Morin...
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Journal Article
Published: 01 September 1972
Bulletin of Canadian Petroleum Geology (1972) 20 (3): 583–607.
...P. E. Gretener ABSTRACT This paper concentrates on some aspects of thrust faulting in a layered sequence. First, the fact that thrust faulting, as the name implies, constitutes duplication of the sequence is considered. The effects of loading due to an advancing thrust sheet are studied...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1971
AAPG Bulletin (1971) 55 (2): 292–306.
... of décollement at various levels overlying the crystalline basement, which was not itself involved ( Bally et al. , 1966 ; Keating, 1966 ). Faults other than thrusts are rare in the area under discussion. In this paper the term “fault” is used to denote thrust faults. The Sylvester Creek and Brewster...
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Journal Article
Published: 01 June 2004
Bulletin of Canadian Petroleum Geology (2004) 52 (2): 139–155.
... Creek and Lundbreck formations (Fig. 9 ). In river exposures the moderately dipping Lundbreck Formation is overridden by a foreland-directed thrust fault (labelled TF1 in Fig. 9 ) carrying sub-horizontal Virgelle Formation. This thrust, which places a hanging wall ramp on a footwall flat, is easily...
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Journal Article
Published: 01 June 1970
Bulletin of Canadian Petroleum Geology (1970) 18 (2): 156–165.
... evidence that shows that the Willow Creek beds are cut by low-angle thrust faults which do not penetrat e the Porcupine Hills strata . Douglas (1950) mapped an erosional contact between the two formations on the west side of the Porcupine Hills . The Willow Creek strata have been intensively deformed...
Journal Article
Published: 01 September 1970
Bulletin of Canadian Petroleum Geology (1970) 18 (3): 332–406.
...) or a folded back-limb fault (Figs . 15 and 16) or, if it were sufficiently extensive, a folded out-of- the-syncline fault. That uplift from below is not the only way of folding thrusts is shown by the folded back-limb fault at Dizzy Creek (Fig . 17) . The Brazeau Range is a very large asymmetric anticline...
Journal Article
Published: 01 June 1969
Bulletin of Canadian Petroleum Geology (1969) 17 (2): 234–246.
... between Cat e Creek and Haig Brook. It is about 2,500 ft long from north to south , 300 ft wide, and about 500 ft from top to bottom . Previously (Price , 1965) , it had been mapped as a bedrock mass in fault contact with the TERTIARY KI,SHENEHN FORMATION 24 1 Kishenehn. However, the contact on both sides...