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Belloy Formation

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Journal Article

THE BELLOY FORMATION (PERMIAN), PEACE RIVER AREA, NORTHERN ALBERTA AND NORTHEASTERN BRITISH COLUMBIA Available to Purchase

I. H. Naqvi
Published: 01 March 1972
Bulletin of Canadian Petroleum Geology (1972) 20 (1): 58–88.
DOI: https://doi.org/10.35767/gscpgbull.20.1.058
...I. H. Naqvi ABSTRACT The Belloy Formation (Wolfcampian to Guadalupian age) consists of sandy or silty dolomites, quartzose sandstones, phosphorites, cherts and minor dolomites. The formation thickens towards the southwest, from an erosional edge to over 600 ft west of Fort St. John. The thickening...
View PDF for article title, THE <span class="search-highlight">BELLOY</span> <span class="search-highlight">FORMATION</span> (PERMIAN), PEACE RIVER AREA, NORTHERN ALBERTA AND NORTHEASTERN BRITISH COLUMBIA
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Image
Boundary between the light grey, bioclastic Permian Belloy Formation and the dark brown, laminated siltstone of the Griesbachian Montney Formation in the Talisman Altares 16-17-083-25W6M well. Base of core is to the left and top of core is to the right. Depths are metres below KB.

Boundary between the light grey, bioclastic Permian Belloy Formation and th... Available to Purchase

Published: 01 September 2014
Figure 4 Boundary between the light grey, bioclastic Permian Belloy Formation and the dark brown, laminated siltstone of the Griesbachian Montney Formation in the Talisman Altares 16-17-083-25W6M well. Base of core is to the left and top of core is to the right. Depths are metres below KB.
Journal Article

Sedimentary facies, petrology, reservoir characteristics, conodont biostratigraphy and sequence stratigraphic framework of a continuous (395m) full diameter core of the Lower Triassic Montney Fm, northeastern British Columbia Available to Purchase

Thomas F. Moslow, Beth Haverslew, Charles M. Henderson
Published: 01 March 2018
Bulletin of Canadian Petroleum Geology (2018) 66 (1): 259–287.
... of the underlying Paleozoic Belloy Formation and base of the overlying Middle Triassic Doig-Phosphate Formation. An informally named “Middle Montney” sequence boundary is regionally correlatable and coincident with the Smithian-Spathian contact. This surface is associated with significant erosion, brecciation...
FIGURES | View All (23)
View PDF for article title, Sedimentary facies, petrology, reservoir characteristics, conodont biostratigraphy and sequence stratigraphic framework of a continuous (395m) full diameter core of the Lower Triassic Montney Fm, northeastern British Columbia
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Journal Article

An exceptional record of the sedimentology and biostratigraphy of the Montney and Doig formations in British Columbia Available to Purchase

M.L. Golding, M.J. Orchard, J.-P. Zonneveld, C.M. Henderson, L. Dunn
Published: 01 September 2014
Bulletin of Canadian Petroleum Geology (2014) 62 (3): 157–176.
DOI: https://doi.org/10.2113/gscpgbull.62.3.157
...Figure 4 Boundary between the light grey, bioclastic Permian Belloy Formation and the dark brown, laminated siltstone of the Griesbachian Montney Formation in the Talisman Altares 16-17-083-25W6M well. Base of core is to the left and top of core is to the right. Depths are metres below KB. ...
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View PDF for article title, An exceptional record of the sedimentology and biostratigraphy of the Montney and Doig <span class="search-highlight">formations</span> in British Columbia
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Journal Article

Dynamic casting and growth faulting: Dawson Creek Graben Complex, Carboniferous–Permian Peace River Embayment, Western Canada Available to Purchase

J.E. Barclay, F.F. Krause, R.I. Campbell, J. Utting
Published: 01 December 1990
Bulletin of Canadian Petroleum Geology (1990) 38A (1): 115–145.
DOI: https://doi.org/10.35767/gscpgbull.38a.1.115
..., tandis que les lits plats de la formation Belloy à l’intérieur et au-delà des bornes de graben indiquent une subsidence sur une grande étendue mais assez limitée, de nouveaux points de sédimentation maximum, et un équilibre tectonique (Permien inférieur). Le CGDC fut un bassin contrôlé surtout par des...
View PDF for article title, Dynamic casting and growth faulting: Dawson Creek Graben Complex, Carboniferous–Permian Peace River Embayment, Western Canada
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Journal Article

PERMIAN STRATIGRAPHY, PEACE RIVER AREA, NORTHEAST BRITISH COLUMBIA Available to Purchase

A. McGugan
Published: 01 March 1967
Bulletin of Canadian Petroleum Geology (1967) 15 (1): 82–90.
DOI: https://doi.org/10.35767/gscpgbull.15.1.082
... at Chowade Creek headwaters. No definite correlation with units of the Belloy Formation in the Peace River subsurface is yet possible, but it is thought that in many wells only the upper portion of the Belloy is referable to the Permian.. 1 Manuscript received November 30, 1966; revised manuscript...
View PDF for article title, PERMIAN STRATIGRAPHY, PEACE RIVER AREA, NORTHEAST BRITISH COLUMBIA
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Secondary migration model for Montney and Gordondale sources indicating migration direction and simulated petroleum saturation (%). Model accumulations match observed accumulations that occur in the (1) Peace River Lower Cretaceous Mannville Group, (2) Peace River Charlie Lake Formation, (3) Charlie Lake and Montney formations stratigraphic subcrop traps, (4) Belloy Formation reservoirs, (5a) Montney and Doig formations. unconventional plays, and (5b) Montney Formation stratigraphic plays in turbiditic sandstones. Arrows indicate the migration directions. Petroleum generated in Montney Formation occurs primarily in Montney Formation and underlying Belloy Formation. Petroleum generated 135–119 mya. In Gordondale and Doig formations, migrates vertically with subsequent migration, 97.5–57.8 mya directed primarily up-dip. East of the Doig Formation Subcrop, petroleum migrates from the Cadomin and Triassic formations. after 79.5 mya into the Mannville Group (from Ducros et al., 2017, their Figure 14).

Secondary migration model for Montney and Gordondale sources indicating mig... Available to Purchase

Published: 23 May 2018
Formation, (3) Charlie Lake and Montney formations stratigraphic subcrop traps, (4) Belloy Formation reservoirs, (5a) Montney and Doig formations. unconventional plays, and (5b) Montney Formation stratigraphic plays in turbiditic sandstones. Arrows indicate the migration directions. Petroleum generated
Image
—Palinspastically-restored section AA′, BB′, and CC′ extending from Paleozoic exposures in the west, across the Foothills, into the adjacent undeformed strata, and longitudinal section DD′ across the Peace River Valley showing thickness of stratigraphic units and estimated maximum paleoground surface. Datum line is top of Bluesky-Gething Formation (stippled areas). Also shown are estimated positions of 1.3% Rmax (end of oil generation), 2.2% Rmax (upper limit of wet-gas preservation), and 4.8% Rmax (upper limit of dry-gas preservation). Upper limit of light-oil (API 50°) preservation (~2.0% Rmax) occurs approximately 200 m (656 ft) above the 2.2% Rmax isoreflectance line. Arrows indicate control points for reflectance values. Numbers in brackets refer to localities shown on Figure 2. Locations of oil pools (o) and gas fields (g) indicated by horizontal bars (from Wallace-Dudley, 1982a, b). For example see position of Blueberry field near eastern limit of section AA’. Palinspastic restoration of section AA’ after Thompson (1986). Unrestored lines of section are shown in Figure 2. uKW = Wapiti Formation, uKS = Smoky Group (Kaskapau to Puskwaskau Formations), KS-uKD = Shaftesbury and Dunvegan Formations, KB-uKD = Buckinghorse to Dunvegan Formations, KM-KBC = Moosebar to Boulder Creek Formations, KS-KPC = Spirit River and Peace River Formations, stippled pattern = Cadomin and Bluesky-Gething Formations, JF-KG = Femie to Bluesky-Gething Formations, JFJKM = Fernie Formation and Minnes Group, T = Triassic undivided, uCP == Stoddart Group and Belloy Formation, CD = Debolt Formation, CDP = Debolt Formation to Belloy Formation, CRP = Rundle Group, Mowich and/or Belloy Formations.

—Palinspastically-restored section AA′, BB′, and CC′ extending from Paleozo... Available to Purchase

Published: 01 November 1988
= Fernie Formation and Minnes Group, T = Triassic undivided, uCP == Stoddart Group and Belloy Formation, CD = Debolt Formation, CDP = Debolt Formation to Belloy Formation, CRP = Rundle Group, Mowich and/or Belloy Formations.
Image

Fig. 9. Residual (upper) and offset pattern (lower) maps derived from the... Available to Purchase

Published: 13 March 2009
Fig. 9. Residual (upper) and offset pattern (lower) maps derived from the top of the Permian Belloy Formation.
Image
Early to Middle Triassic regional schematic stratigraphy oriented parallel to depositional dip. Datum is the top of the Belloy Formation. Stratigraphic location of the D1 and D2 horizons have been identified. Modified from Moslow and Davies, 1997; Davies and Hume, 2016.

Early to Middle Triassic regional schematic stratigraphy oriented parallel ... Available to Purchase

Published: 01 March 2018
Figure 2. Early to Middle Triassic regional schematic stratigraphy oriented parallel to depositional dip. Datum is the top of the Belloy Formation. Stratigraphic location of the D1 and D2 horizons have been identified. Modified from Moslow and Davies, 1997 ; Davies and Hume, 2016 .
Journal Article

New insights on faults in the Peace River Arch region, northwest Alberta, based on existing well-log data and refined trend surface analysis Available to Purchase

Shilong Mei
Published: 13 March 2009
Canadian Journal of Earth Sciences (2009) 46 (1): 41–65.
DOI: https://doi.org/10.1139/E09-006
...Fig. 9. Residual (upper) and offset pattern (lower) maps derived from the top of the Permian Belloy Formation. ...
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View PDF for article title, New insights on faults in the Peace River Arch region, northwest Alberta, based on existing well-log data and refined trend surface analysis
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Lithological log of core from well (Canadian Oxy Belloy, 6-19-78-25W5) showing precise level of specimen of Discamphiceras cf. silberlingi Guex (and coccoliths 2 cm below) in lowermost part of Fernie Formation (Lower Jurassic) overlying dolomitized coquinas of Montney Formation (Lower Triassic).

Lithological log of core from well (Canadian Oxy Belloy, 6-19-78-25W5) show... Available to Purchase

Published: 21 September 2000
Fig. 2. Lithological log of core from well (Canadian Oxy Belloy, 6-19-78-25W5) showing precise level of specimen of Discamphiceras cf. silberlingi Guex (and coccoliths 2 cm below) in lowermost part of Fernie Formation (Lower Jurassic) overlying dolomitized coquinas of Montney Formation (Lower
Journal Article

Structural inversion of the Middle Triassic Halfway Formation, Monias Field, northeast British Columbia Available to Purchase

George T. Norgard
Published: 01 December 1997
Bulletin of Canadian Petroleum Geology (1997) 45 (4): 614–623.
DOI: https://doi.org/10.35767/gscpgbull.45.4.614
... MISSISSIPPIAN STRUCTURAL MOVEMENT During the Carboniferous, the Monias area was part of the Fort St. John Graben where continuous deposition from Mississippian to Permian time produced an overthickened sec- tion from the Mississippian Debolt Formation to the Belloy Formation in response to extensional tectonism...
View PDF for article title, Structural inversion of the Middle Triassic Halfway <span class="search-highlight">Formation</span>, Monias Field, northeast British Columbia
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Laterally flattened specimen of Discamphiceras cf. silberlingi Guex, 25 cm above the base of dark brown, silty shales of the Fernie Formation (Lower Jurassic; Hettangian), from core in Canadian Oxy Belloy, 6-19-78-25W5. Natural size.

Laterally flattened specimen of Discamphiceras cf. silberlingi Guex, 25... Available to Purchase

Published: 21 September 2000
Fig. 3. Laterally flattened specimen of Discamphiceras cf. silberlingi Guex, 25 cm above the base of dark brown, silty shales of the Fernie Formation (Lower Jurassic; Hettangian), from core in Canadian Oxy Belloy, 6-19-78-25W5. Natural size.
Image

Fig. 15. Formation-top offset lines digitized from the offset pattern ima... Available to Purchase

Published: 02 July 2009
Fig. 15. Formation-top offset lines digitized from the offset pattern image in Fig. 9 , overlying the local subsidence map associated with deposition of the interval from the top of the Peace River Formation to the Basal Fish Scale Zone (BFSZ). Major faults: 1, Farmington; 2, Gordondale; 3
Journal Article

The role of differential chemical compaction in the formation of the Gold Creek Collapse Structure, West Central Alberta Available to Purchase

K. Barrett
Published: 01 September 2014
Bulletin of Canadian Petroleum Geology (2014) 62 (3): 132–156.
DOI: https://doi.org/10.2113/gscpgbull.62.3.132
... the approximate area of the Gold Creek Collapse Structure based on the Wabamun Time Structure Map. The reef outline is defined as the approximate midpoint between outer reef crest margin and the reef toe, based on the seismic interpretation. Structure maps of the Wabamun and Belloy Formations helped determine...
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View PDF for article title, The role of differential chemical compaction in the <span class="search-highlight">formation</span> of the Gold Creek Collapse Structure, West Central Alberta
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Fig. 17. Clear River Graben and interpreted faults superimposed on the re... Available to Purchase

Published: 13 March 2009
Fig. 17. Clear River Graben and interpreted faults superimposed on the residual map for the top of the Montney Formation. Major faults: 1, Bear Canyon; 2, Josephine Creek; 4, Gordondale; 5, Saddle Hills; 6, Rycroft; 8, Belloy (Dunvegan); 9, Fairview; 11, Bluesky; 13, Normandville (Tangent); 14
Image

Fig. 11. Formation-top offset lines digitized from the offset pattern ima... Available to Purchase

Published: 02 July 2009
Fig. 11. Formation-top offset lines digitized from the offset pattern image in Fig. 9 , overlying the residual surface of the Basal Fish Scale Zone (BFSZ; Fig. 7 ). Major faults: 1, Farmington; 2, Gordondale; 3, George; 4, Hines Creek; 5, Whitemud; 6, Belloy (Dunvegan); 7, Normandville (Tangent
Image

Fig. 16. Refined interpretation of the Dawson Creek Graben Complex (DCGC)... Available to Purchase

Published: 13 March 2009
Fig. 16. Refined interpretation of the Dawson Creek Graben Complex (DCGC) superimposed on the residual map for the top of the Debolt Formation. Major faults: 1, Bear Canyon; 2, Josephine Creek; 3, Farmington; 4, Gordondale; 5, Saddle Hills; 6, Rycroft; 7, George; 8, Belloy (Dunvegan); 9, Fairview
Image

Fig. 18. Faults and other structures interpreted from Cretaceous formatio... Available to Purchase

Published: 13 March 2009
Fig. 18. Faults and other structures interpreted from Cretaceous formation tops superimposed on the residual map for the Basal Fish Scale Zone (BFSZ). Major faults: 1, Bear Canyon; 2, Josephine Creek; 3, Farmington; 4, Gordondale; 7, George; 8, Belloy (Dunvegan); 9, Fairview; 10, Whitemud; 11