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Zama Lake

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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1968
AAPG Bulletin (1968) 52 (10): 1899–1924.
... elsewhere in the Zama area. The Basal Red beds of the Zama area form a diachronous clastic unit overlying the Precambrian. A thin arkosic basal sandstone unit grades vertically into a red, anhydritic, dolomitic shale. A part of this shale may be equivalent to the Ernestina Lake Formation which...
FIGURES | View All (26)
Journal Article
Published: 01 June 2013
Bulletin of Canadian Petroleum Geology (2013) 61 (2): 187–210.
...Naomi S. Wiebe; Nancy Chow; Lavern D. Stasiuk Abstract Organic-rich carbonate facies in the Middle Devonian Keg River Formation in the Rainbow and Zama sub-basins are widely recognized as source rocks but have received considerably less attention than the oil-producing reef facies in the formation...
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Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2404(13)
... established at eight locations in Spring Mill State Park. Six of the monitoring sites were at springs that feed the streams entering Spring Mill Lake (Fig. 2) . The springs were chosen for sampling in order to isolate water sources for the six subwatersheds and to assess their impact on water quality. Two...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1968
AAPG Bulletin (1968) 52 (6): 1059–1067.
... of activity were Peejay-Wildmint (Triassic oil) and Clarke Lake (Devonian gas). Geophysical .—Seismic work was at its highest since 1958, while gravity operations reached an all-time high ( Table V ). In Alberta, seismic crew-months increased 15% from 1966 to 628; 87% of this was in the Rainbow-Zama...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1970
AAPG Bulletin (1970) 54 (12): 2260–2281.
... billion bbl of oil and 1.5 trillion cu ft of gas. The productive Rainbow-Zama trend extends 110 mi in a general north-south direction and is 20 mi wide at its widest part. Additional discoveries have been made in the Slave Point Formation, Sulphur Point Formation, and Zama Member, all of which overlie...
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Image
—Rainbow-<b>Zama</b> area, Alberta (6-fold CDP dynamite data, section datumed on C...
Published: 01 May 1978
Fig. 10 —Rainbow-Zama area, Alberta (6-fold CDP dynamite data, section datumed on Cold Lake salt reflection—a near-basement horizon). Presence of two small pinnacle reefs is indicated by small amount of drape in reflectors above reefs and by one cycle of onlap (?). Buildups indicated on section
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1986
AAPG Bulletin (1986) 70 (10): 1231–1242.
... of oil and gas from the uphole Tertiary section. Gas and condensate discoveries were also made in the Lower Cambrian section of the Tweed Lake area. The first commercial oil production project in the north, at Norman Wells, was connected to southern markets with the completion of the Zama pipeline...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 March 2014
GSA Bulletin (2014) 126 (3-4): 289–306.
... Society of America 2014 Marshall et al. (1981) first reported a basalt flow above the Bajo Barreal Formation (Chubut Group), but below the unconformable contact with the Salamanca Formation, in the area along the Río Chico, just east of its outflow from Lake Colhué Huapi ( Fig. 1 ). Whole rock...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2012
GSA Bulletin (2012) 124 (7-8): 1071–1086.
... so far. The most similar δ 13 C foraminifera record is based on planktonic foraminifera from the Wilson Lake section (the mixed layer dweller Acarinina ; Zachos et al., 2006 ), which shows an ∼4‰ excursion. Low δ 13 C values recorded in the large miliolids/alveolinids (up to –7.18‰) might...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1989
AAPG Bulletin (1989) 73 (10B): 159–169.
... for the last month of 1988. In the Zama Lake area, Co-enerco drilled the 6-5-118-5 W6M new-pool wildcat. It flowed 10,838 m 3 of oil at an average rate of 67 m 3 /day. The well encountered 56 m of Keg River pay on an isolated pinnacle reef. Momentum generated in oil and gas activity in the last...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1969
AAPG Bulletin (1969) 53 (6): 1308–1317.
.... Of the 1,512 exploratory wells, 29% were successful. Exploration activity in Alberta occurred primarily in central and southern Alberta, and in the Rainbow-Zama area of northwestern Alberta. However, 6 very significant gas discoveries were made in the foothills or deep plains area of Alberta. Saskatchewan had...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1969
AAPG Bulletin (1969) 53 (6): 1308–1317.
... combined current estimates suggest it could be Canada’s largest gas field. Three wells have been credited with discovering the Clark Lake trend—Chevron Clark Lake 11-33-59-18W.5, Fina et al . Fox Creek 10-7-60-18W.5, and Triad et al . Fox Creek 6-24-60-19W.5. In the Rainbow-Zama area of northwest...
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Journal Article
Published: 01 September 1995
Journal of the Geological Society (1995) 152 (5): 849–860.
..., A transfer Zone in Central Lake Baikal EOS, Transactions American Geophysical Union 1991 72 468 Artyushkov E.V. Letnikov F.A. Ruzhich V.V. The mechanism of formation of the Baikal basin Journal of Geodynamics 1990 11 277 291 Badley M.E. Price J.D. Rambech Dahl C...
Journal Article
Published: 01 June 2004
Bulletin of Canadian Petroleum Geology (2004) 52 (2): 156–176.
... Formation of Saskatchewan : Saskatchewan Department of Mineral Resources Report , v. 98 , 101 p. Jordan , S.P. 1967 . Saskatchewan reef trend looks big . Oilweek , v. 17 , p. 10 – 12 . Jordan , S.P. 1968 . Will Zama be duplicated at Quill Lake, Saskatchewan? Oilweek , v. 19...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1968
AAPG Bulletin (1968) 52 (10): 1925–1955.
... of the Rainbow-Zama Island reef trend is indicated on this map; the Rainbow Lake reefs are shown diagrammatically in an isometric block diagram ( Fig. 7 ). These reefs were established in an area that was to become one of the deepest parts of the Muskeg evaporite basin. Deposition during the time of Muskeg...
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Journal Article
Published: 01 September 2009
Bulletin of Canadian Petroleum Geology (2009) 57 (3): 209–250.
... in the July Lake area of extreme northeastern British Columbia, based on the description and investigation of 18 cores from vertical wells drilled in the early 1990s. The Jean Marie in these wells varies from 11.7 to 21.2 m thick and consists of the upper portion of one Transgressive-Regressive (T-R) cycle...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1984
AAPG Bulletin (1984) 68 (10): 1273–1280.
... of oil/day from the overlying Boundary Lake member of the Charlie Lake formation (Triassic), and succeeded in extending westward the limits of the nearby Upper Cretaceous Doe Creek oil field. The Middle Devonian Keg River pinnacle reefs of the Amigo-Shekilie-Zama area (D, Figure 2 ) of northwestern...
FIGURES
Series: SEPM Special Publication
Published: 01 January 2016
DOI: 10.2110/sepmsp.106.11
EISBN: 9781565763432
... basin systems dominated by shallow standing bodies of water. In these nonmarine systems, fluvial channels penetrate all or most of thecontemporary lake. Lakes may be perennial or seasonal and may occur in arid or humid climates. The Hay-Zama Lake system, Alberta, Canada, provides a modern example...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1964
AAPG Bulletin (1964) 48 (6): 1009–1021.
... Point reef gas play in the far northeastern part of the province at Western Natural Gas, Cabin 6-40-A and Standard Oil of British Columbia, Helmet b-49-G, and 50 mi. west of 2 Slave Point gas discoveries just across the Alberta border, Central Del Rio, Zama Lake 10-8, and British American, North Bistcho...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1997
AAPG Bulletin (1997) 81 (5): 712–733.
... and aquifer systems separated by intervening aquitards is at steady state and is driven by the present-day topography both on a regional and a local scale. The flow is generally from a recharge area in the southwest at the fold belt and Bovie Lake fault, to discharge in the northeast at the Great Slave Lake...
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