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![Outcrop study area at Bullmoose Mountain outlined by the 5500’ (1676 m) and 6000’ (1829 m) contours. Measured sections are marked by triangles and cored coal wells as circles. The map also shows locations of cross-sections A–A′(Fig. 5) and B–B′ (Fig. 7) and outcrop photo mosaic (Fig. 8).]()
![Paleogeography of the Falher C in the Bullmoose Mountain region. Basinward is to the north-northwest. See text for discussion.]()
![Location map of the outcrop study area for this investigation. The Bullmoose Mountain area (shaded) is shown in detail in Figure 3.]()
![—Various locations suggested for Peace River arch. Central position runs through Bullmoose Mountain and south of Dawson Creek and Peace River.]()
![Cross-section of the non-marine sediments of the Gates Formation from the Bullmoose Mine area near Bullmoose Mountain, B.C. foothills, based on logged core, gamma and density logs. Eleven cycles or partial cycles are recognized, with each cycle comprising a drying-upwards succession (DU) and a wetting-upwards succession (WU). These non-marine cycles are correlated to the subsurface Falher transgressive–regressive cycles (as suggested on the RHS of the figure – see text for discussion). Refer to Figure 2 for definitions of abbreviations.]()
![Photo mosaic facing west of the Falher C exposure on the north side of Bullmoose Mountain. Falher C packages are highlighted in magenta. Locations of the measured sections are annotated. The clinoforming surfaces are formed as a result of episodic storm events. The geometry of the clinoforms in the photo is due in part to the orientation of the cirque and in part to depositional orientation. Location shown in Figure 3.]()
![—Paleoflow data in unit 10C. Plan views of Mt. Spieker beach berms show east-west strike. On north side of berms clasts dip northwest, which is not interpreted as an imbrication, but indicates disk-shaped clasts lying on berm face (open sea to north and northwest). Same unit crops out on Bullmoose Mountains, where imbrication appears similar.]()
![Paleogeographic reconstruction of the Upper Mannville (Albian) Falher and Gates units (from Leckie and Smith, 1992). The shoreline trend was approximately east–west near the thrust belt. Both the outcrop study area near Bullmoose Mountain and the subsurface study area in the Elmworth Field (indicated by arrows) may have been influenced by differential subsidence associated with the former Peace River Arch.]()
![Deposition of facies associations within the C2 stratal unit on Bullmoose Mountain during the falling stage systems tract. A) Continuous progradation of conglomeratic shoreface facies during fair weather conditions and falling relative sea level. B) Storm events migrate wave base basinward. Sediments are eroded from the upper shoreface and foreshore and transported seaward as geostrophic flows. C) Fair weather conditions resume and progradation of the shoreface continues.]()
![Map of Alberta Foreland Basin, Canada, showing the location of the study area. The isopach contours represent thickness of the Lower Mannville Group (modified from Cant & Abrahamson, 1994 and after Diessel et al., 2000) which can be used as a proxy for regional subsidence and accommodation patterns. This map suggests that the study area lies within a region of high to very high accommodation. The inset map shows cross-section locations. The regional Gates Formation cross-section A–A′ (Fig. 3) integrates subsurface data in the north with oucrop data in the south. The regional Falher Member cross-section B–B′ (Fig. 7) runs approximately parallel to A–A′. The detailed Gates Formation cross-section C–C′ (Fig. 9) from Bullmoose Mountain area is located approximately 40 km northwest of section A–A′. The white dashed line shows approximate position of the Peace River Arch (PRA). Location of wells from which coals samples have been obtained is indicated by black stars.]()
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1-20 OF 63 RESULTS FOR
Bullmoose Mountain
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Journal Article
Outcrop sedimentology and stratal architecture of the Lower Albian Falher C sub-Member, Spirit River Formation, Bullmoose Mountain, northeastern British Columbia Available to Purchase
Publisher: Canadian Society of Petroleum Geologists
Published: 01 March 2004
Bulletin of Canadian Petroleum Geology (2004) 52 (1): 4–22.
... 05 2002 © The Society of Canadian Petroleum Geologists 2004 Outcrop sedimentology and stratal architecture of the Lower Albian Falher C sub-Member, Spirit River Formation, Bullmoose Mountain, northeastern British Columbia, Le sous-membre lithostratigraphique de Fahler C de la formation...
FIGURES
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Image
Outcrop study area at Bullmoose Mountain outlined by the 5500’ (1676 m) and... Available to Purchase
in Outcrop sedimentology and stratal architecture of the Lower Albian Falher C sub-Member, Spirit River Formation, Bullmoose Mountain, northeastern British Columbia
> Bulletin of Canadian Petroleum Geology
Published: 01 March 2004
Fig. 3. Outcrop study area at Bullmoose Mountain outlined by the 5500’ (1676 m) and 6000’ (1829 m) contours. Measured sections are marked by triangles and cored coal wells as circles. The map also shows locations of cross-sections A–A′(Fig. 5 ) and B–B′ (Fig. 7 ) and outcrop photo mosaic (Fig. 8 ).
Image
Paleogeography of the Falher C in the Bullmoose Mountain region. Basinward ... Available to Purchase
in Outcrop sedimentology and stratal architecture of the Lower Albian Falher C sub-Member, Spirit River Formation, Bullmoose Mountain, northeastern British Columbia
> Bulletin of Canadian Petroleum Geology
Published: 01 March 2004
Fig. 10. Paleogeography of the Falher C in the Bullmoose Mountain region. Basinward is to the north-northwest. See text for discussion.
Journal Article
THE LOWER CRETACEOUS NOTIKEWIN MEMBER (FORT ST. JOHN GROUP), NORTHEASTERN BRITISH COLUMBIA: A PROGRADATIONAL BARRIER ISLAND SYSTEM Available to Purchase
Publisher: Canadian Society of Petroleum Geologists
Published: 01 March 1985
Bulletin of Canadian Petroleum Geology (1985) 33 (1): 39–51.
... brackish conditions and locally form banks. The Ostrea beds provide a good local stratigraphic marker in the Bullmoose Mountain area. Sedimentary structures in interbedded sandstones, siltstones and shales, as well as reversing paleoflow directions, indicate a low-wave-energy coast dominated by tidal-flat...
Image
Location map of the outcrop study area for this investigation. The Bullmoos... Available to Purchase
in Outcrop sedimentology and stratal architecture of the Lower Albian Falher C sub-Member, Spirit River Formation, Bullmoose Mountain, northeastern British Columbia
> Bulletin of Canadian Petroleum Geology
Published: 01 March 2004
Fig. 1. Location map of the outcrop study area for this investigation. The Bullmoose Mountain area (shaded) is shown in detail in Figure 3 .
Image
—Various locations suggested for Peace River arch. Central position runs th... Available to Purchase
in Rates, Controls, and Sand-Body Geometries of Transgressive-Regressive Cycles: Cretaceous Moosebar and Gates Formations, British Columbia
> AAPG Bulletin
Published: 01 May 1986
Figure 18 —Various locations suggested for Peace River arch. Central position runs through Bullmoose Mountain and south of Dawson Creek and Peace River.
Image
Cross-section of the non-marine sediments of the Gates Formation from the B... Available to Purchase
in Stratigraphic style of coal and non-marine strata in a high accommodation setting: Falher Member and Gates Formation (Lower Cretaceous), western Canada
> Bulletin of Canadian Petroleum Geology
Published: 01 September 2003
Fig. 9. Cross-section of the non-marine sediments of the Gates Formation from the Bullmoose Mine area near Bullmoose Mountain, B.C. foothills, based on logged core, gamma and density logs. Eleven cycles or partial cycles are recognized, with each cycle comprising a drying-upwards succession (DU
Image
Photo mosaic facing west of the Falher C exposure on the north side of Bull... Available to Purchase
in Outcrop sedimentology and stratal architecture of the Lower Albian Falher C sub-Member, Spirit River Formation, Bullmoose Mountain, northeastern British Columbia
> Bulletin of Canadian Petroleum Geology
Published: 01 March 2004
Fig. 8. Photo mosaic facing west of the Falher C exposure on the north side of Bullmoose Mountain. Falher C packages are highlighted in magenta. Locations of the measured sections are annotated. The clinoforming surfaces are formed as a result of episodic storm events. The geometry
Image
—Paleoflow data in unit 10C. Plan views of Mt. Spieker beach berms show eas... Available to Purchase
in Storm-and Tide-Dominated Shorelines in Cretaceous Moosebar-Lower Gates Interval—Outcrop Equivalents of Deep Basin Gas Trap in Western Canada
> AAPG Bulletin
Published: 01 February 1982
on Bullmoose Mountains, where imbrication appears similar.
Image
Paleogeographic reconstruction of the Upper Mannville (Albian) Falher and G... Available to Purchase
in Stratigraphic style of coal and non-marine strata in a high accommodation setting: Falher Member and Gates Formation (Lower Cretaceous), western Canada
> Bulletin of Canadian Petroleum Geology
Published: 01 September 2003
Fig. 1. Paleogeographic reconstruction of the Upper Mannville (Albian) Falher and Gates units (from Leckie and Smith, 1992 ). The shoreline trend was approximately east–west near the thrust belt. Both the outcrop study area near Bullmoose Mountain and the subsurface study area in the Elmworth
Image
Deposition of facies associations within the C2 stratal unit on Bullmoose M... Available to Purchase
in Outcrop sedimentology and stratal architecture of the Lower Albian Falher C sub-Member, Spirit River Formation, Bullmoose Mountain, northeastern British Columbia
> Bulletin of Canadian Petroleum Geology
Published: 01 March 2004
Fig. 9. Deposition of facies associations within the C2 stratal unit on Bullmoose Mountain during the falling stage systems tract. A) Continuous progradation of conglomeratic shoreface facies during fair weather conditions and falling relative sea level. B) Storm events migrate wave base
Image
Map of Alberta Foreland Basin, Canada, showing the location of the study ar... Available to Purchase
in Stratigraphic style of coal and non-marine strata in a high accommodation setting: Falher Member and Gates Formation (Lower Cretaceous), western Canada
> Bulletin of Canadian Petroleum Geology
Published: 01 September 2003
Member cross-section B–B′ (Fig. 7 ) runs approximately parallel to A–A′. The detailed Gates Formation cross-section C–C′ (Fig. 9 ) from Bullmoose Mountain area is located approximately 40 km northwest of section A–A′. The white dashed line shows approximate position of the Peace River Arch (PRA
Journal Article
Rates, Controls, and Sand-Body Geometries of Transgressive-Regressive Cycles: Cretaceous Moosebar and Gates Formations, British Columbia Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 May 1986
AAPG Bulletin (1986) 70 (5): 516–535.
...Figure 18 —Various locations suggested for Peace River arch. Central position runs through Bullmoose Mountain and south of Dawson Creek and Peace River. ...
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Journal Article
Storm-and Tide-Dominated Shorelines in Cretaceous Moosebar-Lower Gates Interval—Outcrop Equivalents of Deep Basin Gas Trap in Western Canada Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 February 1982
AAPG Bulletin (1982) 66 (2): 138–157.
... on Bullmoose Mountains, where imbrication appears similar. ...
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Journal Article
Triassic petroleum geology, Western Canada Basin and neighbouring Yukon Territory and American regions: bibliography and summary Available to Purchase
Publisher: Canadian Society of Petroleum Geologists
Published: 01 December 1993
Bulletin of Canadian Petroleum Geology (1993) 41 (4): 437–452.
... thrust fault sheets, similar to fields northward in the Sukunka-Bullmoose area within Peace River Embayment (e.g., Barss and Montandon, 1981). Gas at the Basing Field occurs in the "Coquina bed" of the Sulphur Mountain Formation, Spray River Group and the reservoir consists of argillaceous iltstones...
Journal Article
Stratigraphic style of coal and non-marine strata in a high accommodation setting: Falher Member and Gates Formation (Lower Cretaceous), western Canada Available to Purchase
Publisher: Canadian Society of Petroleum Geologists
Published: 01 September 2003
Bulletin of Canadian Petroleum Geology (2003) 51 (3): 275–303.
...Fig. 9. Cross-section of the non-marine sediments of the Gates Formation from the Bullmoose Mine area near Bullmoose Mountain, B.C. foothills, based on logged core, gamma and density logs. Eleven cycles or partial cycles are recognized, with each cycle comprising a drying-upwards succession (DU...
FIGURES
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Journal Article
SUKUNKA-BULLMOOSE GAS FIELDS: MODELS FOR A DEVELOPING TREND IN THE SOUTHERN FOOTHILLS OF NORTHEAST BRITISH COLUMBIA Available to Purchase
Publisher: Canadian Society of Petroleum Geologists
Published: 01 September 1981
Bulletin of Canadian Petroleum Geology (1981) 29 (3): 293–333.
... estimates on reservoir conformance toprediction will not be available until the individual pools have been produced for some time. GEOLOGICAL SETTING The Sukunka/Bullmoose fi ld area is located within the Rocky Mountain Inner Foothills belt of British Columbia (Fig. 1), about 100 km southwest of Dawson...
Journal Article
Gas isotope reversals in fractured gas reservoirs of the western Canadian Foothills: Mature shale gases in disguise Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 August 2011
AAPG Bulletin (2011) 95 (8): 1399–1422.
... al., 2004 ), represents the lower part of the oldest clastic wedge in the WCSB. It is at its thickest in the general study area (Bullmoose-Sukunka structural trend; Cooper et al., 2004 ) and thins to the north. 3 1 2011 15 6 2010 16 8 2010 28 9 2010 Copyright ©2011...
FIGURES
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Journal Article
Coalbed Methane Characteristics of Gates Formation Coals, Northeastern British Columbia: Effect of Maceral Composition Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 11 December 1993
AAPG Bulletin (1993) 77 (12): 2062–2076.
... in the Bullmoose mine area range in reflectance (R o max) from 1.02 to 1.14% ( Kalkreuth and Leckie, 1989 ), which corresponds to a coal rank range of high-volatile A to medium-volatile bituminous. Figure 1 —Location map showing the study area and Bullmoose mine sampling site. Black areas indicate major...
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Journal Article
Burial History and Thermal Maturity, Rocky Mountain Front Ranges, Foothills, and Foreland, East-Central British Columbia and Adjacent Alberta, Canada Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 November 1988
AAPG Bulletin (1988) 72 (11): 1395–1410.
.... A. Stewart , 1966 , Structure, seismic data and orogenic evolution of southern Canadian Rocky Mountains : Canadian Petroleum Geology Bulletin , v. 14 , p. 337 – 381 . Barss , D. L. and F. A. Montandon , 1981 , Sukunka-Bullmoose gas fields: models for a developing trend in the southern...
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