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Minnes Group

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Journal Article

Tectonostratigraphy of Jurassic and Cretaceous sediments of the east-central British Columbia Foothills near Kinuseo Creek Available to Purchase

S.T. Johnston
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 215.
DOI: https://doi.org/10.35767/gscpgbull.39.2.215c
...S.T. Johnston Jurassic and Cretaceous strata in the Foothills near Kinuseo Creek are divisible into three tectonostratigraphic packages. The lower package consists of Fernie Group strata and the lower part of the Minnes Group. Strata are characteristically folded and thickened by numerous thrust...
View PDF for article title, Tectonostratigraphy of Jurassic and Cretaceous sediments of the east-central British Columbia Foothills near Kinuseo Creek
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Journal Article

Jurassic strata of northwestern (and west-central) Alberta and northeastern British Columbia Available to Purchase

T.P. Poulton, J. Tittemore, G. Dolby
Published: 01 December 1990
Bulletin of Canadian Petroleum Geology (1990) 38A (1): 159–175.
DOI: https://doi.org/10.35767/gscpgbull.38a.1.159
... formation Nikanassin et le groupe Minnes, est un dépôt orogénique clastique qui se termine en biseau en direction est et remplit l’avant-fosse à l’ouest, et qui se retrouve en minces dépôts de schiste argileux et de grès équivalents déposés sur une plate-forme à l’est. L’absence ou la quasi-absence de...
View PDF for article title, Jurassic strata of northwestern (and west-central) Alberta and northeastern British Columbia
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Journal Article

LOWER CRETACEOUS LUSCAR GROUP (REVISED) OF THE NORTHERN AND NORTH-CENTRAL FOOTHILLS OF ALBERTA Available to Purchase

C. Willem Langenberg, Margaret E. McMechan
Published: 01 March 1985
Bulletin of Canadian Petroleum Geology (1985) 33 (1): 1–11.
DOI: https://doi.org/10.35767/gscpgbull.33.1.001
...C. Willem Langenberg; Margaret E. McMechan RÉSUMÉ Le Groupe Luscar (revisé) forme la séquence carbonifère du Crétacé Inférieur qui recouvre disconformément les strates marines et non-marines de la Formation Nikanassin du Groupe Minnes et qui est disconformément sous-jacent aux argiles marines...
View PDF for article title, LOWER CRETACEOUS LUSCAR <span class="search-highlight">GROUP</span> (REVISED) OF THE NORTHERN AND NORTH-CENTRAL FOOTHILLS OF ALBERTA
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Journal Article

RANK AND PETROGRAPHIC COMPOSITION OF SELECTED JURASSIC - LOWER CRETACEOUS COALS OF BRITISH COLUMBIA, CANADA Available to Purchase

W. D. Kalkreuth
Published: 01 June 1982
Bulletin of Canadian Petroleum Geology (1982) 30 (2): 112–139.
DOI: https://doi.org/10.35767/gscpgbull.30.2.112
... of the Kootenay Group, whereas coals of the Peace River Coalfield were obtained from the Gorman Creek and Bickford Formations of the Minnes Group and from the Gething Formation of the Bullhead Group. Rank, determined by vitrinite reflectance measurements, ranges from subbituminous C in the Crowsnest Coalfield...
View PDF for article title, RANK AND PETROGRAPHIC COMPOSITION OF SELECTED JURASSIC - LOWER CRETACEOUS COALS OF BRITISH COLUMBIA, CANADA
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Journal Article

Sediment dispersal in an evolving foreland: Detrital zircon geochronology from Upper Jurassic and lowermost Cretaceous strata, Alberta Basin, Canada Available to Purchase

M. Keegan Raines, Stephen M. Hubbard, Ross B. Kukulski, Andrew L. Leier, George E. Gehrels
Journal: GSA Bulletin
Published: 01 May 2013
GSA Bulletin (2013) 125 (5-6): 741–755.
DOI: https://doi.org/10.1130/B30671.1
.... Accordingly, sandstones of the Jurassic foreland, associated with the Minnes Group and equivalent Kootenay and Nikanassin formations, are divided into two informal groups, type 1 and type 2. Type 1 sandstones are mature quartz arenites, present along the entire north-south length of the Alberta Basin...
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View PDF for article title, Sediment dispersal in an evolving foreland: Detrital zircon geochronology from Upper Jurassic and lowermost Cretaceous strata, Alberta Basin, Canada
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Journal Article

Tight gas sandstone reservoir delineation through channel-belt analysis, Late Jurassic Monteith Formation, Alberta Deep Basin Available to Purchase

Ross B. Kukulski, Thomas F. Moslow, Stephen M. Hubbard
Published: 01 June 2013
Bulletin of Canadian Petroleum Geology (2013) 61 (2): 133–156.
DOI: https://doi.org/10.2113/gscpgbull.61.2.133
...Ross B. Kukulski; Thomas F. Moslow; Stephen M. Hubbard Abstract The Late Jurassic–Early Cretaceous Monteith Formation (Minnes Group) records incipient foredeep deposition in the Deep Basin of northwestern Alberta and British Columbia. The uppermost lithostratigraphic unit of the Monteith Formation...
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View PDF for article title, Tight gas sandstone reservoir delineation through channel-belt analysis, Late Jurassic Monteith Formation, Alberta Deep Basin
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Journal Article

A stratigraphic framework for Late Jurassic–Early Cretaceous gas-bearing strata (Monteith Formation) in the subsurface of northwest Alberta Available to Purchase

Brett D. Miles, Ross B. Kukulski, M. Keegan Raines, John-Paul Zonneveld, Andrew L. Leier, Stephen M. Hubbard
Published: 01 March 2012
Bulletin of Canadian Petroleum Geology (2012) 60 (1): 3–36.
DOI: https://doi.org/10.2113/gscpgbull.60.1.3
..., is assigned to the Monteith Formation (Minnes Group). Three mappable units are present, informally termed Monteith A, B and C, from youngest to oldest. The Monteith C was deposited in a marginal marine–deltaic depositional setting. Upward, the transition to coastal plain (Monteith B) and fluvial (Monteith...
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View PDF for article title, A stratigraphic framework for Late Jurassic–Early Cretaceous gas-bearing strata (Monteith Formation) in the subsurface of northwest Alberta
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Journal Article

Structural geometry in the Carbon Creek area of the Rocky Mountain Fold and Thrust Belt, northeastern British Columbia Available to Purchase

M.E. McMechan
Published: 01 September 2002
Bulletin of Canadian Petroleum Geology (2002) 50 (3): 407–418.
DOI: https://doi.org/10.2113/50.3.407
... in excess shortening of Fernie Formation and Jurassic–Cretaceous Minnes Group strata relative to overlying strata that is most reasonably balanced by two local triangle zones or tectonic wedges rather than one more regional zone. A thick sequence (up to 6 km) of pre-Windermere Proterozoic sediments...
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View PDF for article title, Structural geometry in the Carbon Creek area of the Rocky Mountain Fold and Thrust Belt, northeastern British Columbia
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Journal Article

Source Rock Potential and Thermal Maturity of Lower Cretaceous Strata: Monkman Pass Area, British Columbia Available to Purchase

D. A. Leckie, W. D. Kalkreuth, L. R. Snowdon
Journal: AAPG Bulletin
Published: 01 July 1988
AAPG Bulletin (1988) 72 (7): 820–838.
DOI: https://doi.org/10.1306/703C8F38-1707-11D7-8645000102C1865D
... gas will be, or has been, generated. The nonmarine Minnes Group and Gething and Gates Formations average 2.7, 6.3, and 5.2% total organic carbon (TOC), respectively, with fair to very good gas source potential. The nonmarine Boulder Creek Formation contains 1.1% TOC and has poor source rock potential...
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View PDF for article title, Source Rock Potential and Thermal Maturity of Lower Cretaceous Strata: Monkman Pass Area, British Columbia
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—Crossplots of oxygen index vs. hydrogen index for each formation. Maturation pathways from Espitalié et al (1977). Results of analyses of individual samples are plotted with an X. Minnes Group and Gething, Gates, and Boulder Creek Formations are nonmarine; Moosebar, Hulcross, and Shaftesbury Formations are marine.

—Crossplots of oxygen index vs. hydrogen index for each formation. Maturati... Available to Purchase

Published: 01 July 1988
Figure 5 —Crossplots of oxygen index vs. hydrogen index for each formation. Maturation pathways from Espitalié et al (1977) . Results of analyses of individual samples are plotted with an X. Minnes Group and Gething, Gates, and Boulder Creek Formations are nonmarine; Moosebar, Hulcross
Image
—Crossplots of Tmax vs. HI for each formation. Organic matter types and oil-gas limits based on Espitalié et al (1984). Results of analyses of individual samples are plotted with an X. Dashed line represents threshold of hydrocarbon generation for different types of organic matter. Minnes Group and Gething, Gates, and Boulder Creek Formations are nonmarine; Moosebar, Hulcross, and Shaftesbury Formations are marine.

—Crossplots of T max vs. HI for each formation. Organic matter types and o... Available to Purchase

Published: 01 July 1988
. Minnes Group and Gething, Gates, and Boulder Creek Formations are nonmarine; Moosebar, Hulcross, and Shaftesbury Formations are marine.
Image
—(a) Reflectance data for Lower Cretaceous Cadomin Formation, Upper Jurassic-Lower Cretaceous Minnes Group and Jurassic Fernie Formation. (A), (B), and (C) denote locations where vitrinite reflectances were found to be depressed (Kalkreuth, 1982). See Figure 2 for location identification. (b) Reflectance data for Triassic, Carboniferous, and Devonian samples. Rrandom reflectances can be converted to Rmax using the equation: Rmax% = 1.12 Rrandom% – 0.05 (Weiss, 1985).

—(a) Reflectance data for Lower Cretaceous Cadomin Formation, Upper Jurassi... Available to Purchase

Published: 01 November 1988
Figure 6 —(a) Reflectance data for Lower Cretaceous Cadomin Formation, Upper Jurassic-Lower Cretaceous Minnes Group and Jurassic Fernie Formation. (A), (B), and (C) denote locations where vitrinite reflectances were found to be depressed ( Kalkreuth, 1982 ). See Figure 2 for location
Image
Overview of study area and regional stratigraphic nomenclature context. (A) Regional map of subsurface Late Jurassic–Early Cretaceous well penetrations, subsurface deformation front, and Minnes Group zero edge. Spatial extent of lithostratigraphic units defined by Stott (1998) and corresponding type sections in the foothills are shown. Inset map of Canada with study area location included. (B) Detailed study area map with wells used for mapping; locations of core and subcrop edges of the three Monteith Formation units are indicated.

Overview of study area and regional stratigraphic nomenclature context. (A)... Available to Purchase

Published: 01 March 2012
Figure 2 Overview of study area and regional stratigraphic nomenclature context. (A) Regional map of subsurface Late Jurassic–Early Cretaceous well penetrations, subsurface deformation front, and Minnes Group zero edge. Spatial extent of lithostratigraphic units defined by Stott (1998
Image
Regional dip oriented gamma radiation log cross-section (B–B′) featuring the stratigraphic correlation scheme adapted in this study indicated by solid lines, as well as previous stratigraphic picks from Stott (1998) and Legun (1988), indicated by bars adjacent to gamma radiation curves. Progressive downcutting and erosion of the Minnes Group associated with the sub-Cadomin unconformity in northeast British Columbia was substantial. The differential application of stratigraphic picks by Stott (1998) in 07-12-077-25W6 in part, caused miscorrelation of units into the Alberta subsurface; note the very limited spatial extent of the Bickford, Monach and Beattie Peaks formations. The section location is shown in Figure 2A.

Regional dip oriented gamma radiation log cross-section (B–B′) featuring th... Available to Purchase

Published: 01 March 2012
curves. Progressive downcutting and erosion of the Minnes Group associated with the sub-Cadomin unconformity in northeast British Columbia was substantial. The differential application of stratigraphic picks by Stott (1998) in 07-12-077-25W6 in part, caused miscorrelation of units into the Alberta
Journal Article

Ultra high pulse power acoustic logging with low frequency multipole transmitters and receivers — a discussion of interpretive techniques Available to Purchase

P. Husten, D. Patterson, S. Gill, W. Volk
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 215.
DOI: https://doi.org/10.35767/gscpgbull.39.2.215
... lower package consists of Fernie Group strata and the lower part of the Minnes Group. Strata are characteristically folded an thickened by numerous thrust faults. Open anti- clines and synclines are thought to overlie and be related to ramps in underly- ing thrust faults affecting Triassic and older...
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Journal Article

Horizontal drilling of a pinnacle reef: a geologist’s perspective Available to Purchase

G.S. Jones
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 215.
DOI: https://doi.org/10.35767/gscpgbull.39.2.215e
... into three tectonostratigraphic packages. Th lower package consists of Fernie Group strata and the lower part of the Minnes Group. Strata are characteristically folded an thickened by numerous thrust faults. Open anti- clines and synclines are thought to overlie and be related to ramps in underly- ing thrust...
View PDF for article title, Horizontal drilling of a pinnacle reef: a geologist’s perspective
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Journal Article

Stratigraphic architecture of the Cardium Formation in the Pembina Field, west–central Alberta Available to Purchase

S.D. Joiner, F.F. Krause
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 215.
DOI: https://doi.org/10.35767/gscpgbull.39.2.215d
... and Cretaceous ediments of the east- central British Columbia Foothills near Kinuseo Creek Jurassic and Cretaceous strata in the Foothills near Kinuseo Creek are divisible into three tectonostratigraphic packages. Th lower package consists of Fernie Group strata and the lower part of the Minnes Group. Strata...
View PDF for article title, Stratigraphic architecture of the Cardium Formation in the Pembina Field, west–central Alberta
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Journal Article

Coalbed methane in Southeast British Columbia Available to Purchase

D.G.S. Johnson, L.A. Smith
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 215.
DOI: https://doi.org/10.35767/gscpgbull.39.2.215b
... and Cretaceous ediments of the east- central British Columbia Foothills near Kinuseo Creek Jurassic and Cretaceous strata in the Foothills near Kinuseo Creek are divisible into three tectonostratigraphic packages. Th lower package consists of Fernie Group strata and the lower part of the Minnes Group. Strata...
View PDF for article title, Coalbed methane in Southeast British Columbia
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Journal Article

Geometry of the structural front in the Kakwa area, northern Foothills of Alberta Available to Purchase

M.E. McMechan
Published: 01 March 1999
Bulletin of Canadian Petroleum Geology (1999) 47 (1): 31–42.
DOI: https://doi.org/10.35767/gscpgbull.47.1.031
... the top of the Minnes Group, in the Kaskapau Formation and in the mid- dle part of the Brazeau Formation. Four main, tectonically thickened wedges are interpreted (Fig. 5a). Only in the western third of the cross-section, in the 'lower inner' wedge, are Triassic and Paleozoic strata involved...
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—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.