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Stettler

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Journal Article
Published: 01 December 2018
Bulletin of Canadian Petroleum Geology (2018) 66 (4): 773–802.
... minerals. The evidence for density-driven reflux from the Stettler brines for the formation of the pervasive fine-crystalline matrix dolomite include: 1) dolomitization occurs in sediments that were relatively uncompacted, and the degree of preservation of the original fabrics, such as fenestrae...
FIGURES | View All (15)
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 558.
...J. R. Century In October 1977, a significant extension to the 50,000,000 bbl Stettler D-3 and D-2 reef oil field was made 28 years after the initial 1949 discovery and 17 years after the field was considered fully delineated by exploratory and development drilling. The Stettler field is among...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1958
AAPG Bulletin (1958) 42 (1): 1–93.
... controlled in part by ocean currents in later Leduc time. In the Stettler area, late Cooking Lake sedimentation produced shallow-water limestones, now dolomitized, along three main trends termed Fenn-Big Valley, Stettler-Erskine, and Gadsby shoals. The Gadsby shoal was characterized by widespread biostromal...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1954
AAPG Bulletin (1954) 38 (12): 2500–2536.
...J. M. Andrichuk; J. S. Wonfor ABSTRACT Late Devonian history in the Stettler area is divisible into four sequences of deposition comprising a major evaporite cycle. Unconformities mark the base and top of this cycle. The sequences in increasing age are: (1) final normal marine, (2) biostromal...
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Series: AAPG Special Publication, AAPG Special Publication
Published: 01 January 1954
DOI: 10.1306/SV15347C26
EISBN: 9781629812465
... Abstract The Stettler field is in the central plains of Alberta, Canada, approximately 100 miles northeast of Calgary. The field was found by detailed seismograph and structural core drilling. The producing reservoir was found in May, 1949, in two reefoid zones of Upper Devonian age...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1951
AAPG Bulletin (1951) 35 (4): 865–884.
...R. P. Lockwood; O. A. Erdman ABSTRACT The Stettler field is in the central plains of Alberta, Canada, approximately 100 miles northeast of Calgary. The field was found by detailed seismograph and structural core drilling. The producing reservoir was found in May, 1949, in two reefoid zones of Upper...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1950
AAPG Bulletin (1950) 34 (11): 2253.
...R. P. Lockwood; O. A. Erdman ABSTRACT The Stettler field is located in the central plains of Alberta, Canada, approximately 100 miles northeast of Calgary. The field was found by detailed seismograph and structural core drilling. Production was found in two reefoid horizons of Upper Devonian age...
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1960
AAPG Bulletin (1960) 44 (10): 1651–1681.
...John M. Andrichuk ABSTRACT The Wabamun group, consisting mainly of carbonate rocks and anhydrite, increases in thickness westward from less than 500 feet in the Leduc and Stettler areas to approximately 1,800 feet in part of the Rocky Mountains of Alberta. East of Leduc and north of Stettler...
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Journal Article
Published: 01 December 1969
Bulletin of Canadian Petroleum Geology (1969) 17 (4): 444–459.
...R. G. Metherell; L. E. Workman ABSTRACT The Crossfield Member is a gas-producing zone in the middle of the Stettler Formation of Upper Devonian age. It averages about 100 ft in thickness and is recognized in a north - south belt, about 2to 12 mi wide, along the line of the Fifth Principle Meridian...
Journal Article
Published: 01 December 1998
Bulletin of Canadian Petroleum Geology (1998) 46 (4): 487–514.
.... The platform experienced widely fluctuating subsidence rates superimposed on slowly varying eustatic sea-level, and paleoceanographic changes which altered depositional environments and caused large variability of strata. Intertidal evaporites of the Upper Famennian Stettler Formation are separated from...
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Depositional model for the Upper <b>Stettler</b> Formation and Crossfield Member w...
Published: 01 December 2018
Figure 4. Depositional model for the Upper Stettler Formation and Crossfield Member with division of facies into supratida l /intertidaf/shailow subtidal/open marine realms (Modified from Martindale, 2005 (personal communication), and Raymus, 2006 ).
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Diagenetic model for the Upper <b>Stettler</b> Formation and Crossfield Member. Du...
Published: 01 December 2018
Figure 15. Diagenetic model for the Upper Stettler Formation and Crossfield Member. During stages 1 and 2, which include deposition and early marine diagenesis processes such as micritization, primary evaporite precipitation and early calcite cementation become important. During stage 3: shallow
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Generalized lithofacies succession for the <b>Stettler</b>, Big Valley and Exshaw ...
Published: 01 June 2015
Figure 6 Generalized lithofacies succession for the Stettler, Big Valley and Exshaw formations in the study area.
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Core photographs of upper <b>Stettler</b> Formation. A. Characteristic textures of...
Published: 01 June 2015
Figure 7 Core photographs of upper Stettler Formation. A. Characteristic textures of sabkha-salina environments. Enterolithic (en) anhydrite layers separated by laminoid dark organic-rich microbial mats (06-13-009-25W4M, 2453.0 m). B. Laminated to disrupted dololaminite (dol.micr) with nodular
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Isopach maps of the Big Valley Formation (left) and <b>Stettler</b> Formation (rig...
Published: 01 June 2015
Figure 20 Isopach maps of the Big Valley Formation (left) and Stettler Formation (right) A. This map highlights the irregular over thickened localized areas, as well as the thickness trend oriented NNW-SSE. B. This map illustrates, to some degree, that where the Big Valley Formation is thickest
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Cored interval of upper <b>Stettler</b> to lower Exshaw formations from Husky et a...
Published: 01 December 2010
Fig. 11. Cored interval of upper Stettler to lower Exshaw formations from Husky et al. Coaldale 6-34-7-20W4 well (Well C2 in Fig. 2 , Table 1 ) showing interpreted depositional environments, stratigraphic ranges of selected conodonts, and interpreted conodont zones. In this figure and Figs. 12
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Cored interval of upper <b>Stettler</b> to upper Exshaw formations from Husky et a...
Published: 01 December 2010
Fig. 13. Cored interval of upper Stettler to upper Exshaw formations from Husky et al. Leopard 12-1-9-20W4 well (Well C9 in Fig. 2 , Table 1 ) showing interpreted depositional environments, stratigraphic ranges of selected conodonts, and interpreted conodont zones. Gamma curve for well shown
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Cored interval of upper <b>Stettler</b> to lower Banff formations from Husky et al...
Published: 01 December 2010
Fig. 14. Cored interval of upper Stettler to lower Banff formations from Husky et al. Keho 16-27-11-22W4 well (Well C12 in Fig. 2 , Table 1 ) showing interpreted depositional environments, stratigraphic ranges of selected conodonts, and interpreted conodont zones. Gamma curve for well shown
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Cored interval of upper part of <b>Stettler</b> Formation to the lower part of the...
Published: 01 December 2010
Fig. 20. Cored interval of upper part of Stettler Formation to the lower part of the Banff Formation in the Gulf Mohawk Blood 11-36-7-23W4 well (Well C11 in Fig. 2 , Table 1 ) showing interpreted depositional environments, stratigraphic ranges of selected conodonts, and interpreted conodont
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Cored interval of upper part of <b>Stettler</b> Formation to lower part of Banff F...
Published: 01 December 2010
Fig. 24. Cored interval of upper part of Stettler Formation to lower part of Banff Formation in the Chevron et al. 1-2-6-26W4 well (Well C7 in Fig. 2 , Table 1 ) showing interpreted depositional environments, stratigraphic ranges of selected conodonts, and interpreted conodont zones. Arrow