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BUL 045

Polyphase Deformation in the Canadian Shield of Northeastern Alberta

Two generations of structures can be distinguished in the granite gneisses and intercalated high-grade metasediments of the basement neiss complex, which has been shown to be Archean by radiometry dating. In some areas, D2 folds form parts of domes ... Show Abstract

Langenberg, C.W.  1983-01-01

BUL 051

Petrology and geochemistry of the Canadian Shield of northeastern Alberta

The remnant, central belt of granodioritic to quartz-monzonitic gneiss, of I-type granitoid composition, is flanked on its western argin by fairly homogeneous protons of biotite quartz monzonite to granite (Slave and Arch Lake Granitoids), and on ... Show Abstract

Goff, S.P.  Godfrey, J.D.  Holland, J.G.  1986-01-01

BUL 062

Industrial Mineral Potential of Alberta Formation Waters

Nearly 130 000 analyses of formation waters from Alberta and adjacent areas were searched for contents of Ca, Mg, K, Br, I and Li exceeding specified regional exploration thresholds. The 5280 analyses meeting these criteria comprise the formation ... Show Abstract

Hitchon, B.  Bachu, S.  Underschultz, J.R.  Yuan, L.P.  1995-01-01

BUL 003

Precambrian Basement Features in Northern Alberta

The Precambrian basement rocks and their overlying arenaceous deposits have been discussed by Baillie (1956), Goodman (1956), Greenwalt (1956), Guthrie (1956), and Sproule (1956), and the Peace River region has been the subject of a symposium of the ... Show Abstract

Green, R.  1958-01-01

BUL 052

Geophysical expression of the Canadian Shield of northeastern Alberta

The Canadian Shield of northeastern Alberta has a geophysical expression controlled by lithology and complex structural- metamorphic features. The magnetic field of the Alberta Shield (the exposed part of the Canadian Shield in Alberta) shows a ... Show Abstract

Sprenke, K.F.  Wavra, C.S.  Godfrey, J.D.  1986-01-01

BUL 055

Geology of the basement beneath the Athabasca Basin in Alberta

The basement beneath the unconformity can be subdivided into four granitoid rock types recognized as part of the Wylie Lake pluton, and two mylonitic rock types derived partly from the granitoids and partly from a metasedimentary or metavolcanic ... Show Abstract

Wilson, J.A.  1986-01-01

BUL 058

Hydrogeology of the Swan Hills Area, Alberta: Evaluation for deep waste injection

A detailed hydrogeological study was carried out in a region defined as Tp 62-74 R 1-13 W5M, comprising 15 760 square km effectively centered on the Special Waste Injection Site of the Alberta Special Waste Management Corporation. The objective was ... Show Abstract

Hitchon, B.  Sauveplane, C.M.  Bachu, S.  Koster, E.H.  Lytviak, A.T.  1989-01-01

BUL 038

The Hydrogeology of the Athabasca Oil Sands Area, Alberta

West of the fault, three hydrostratigraphic units are defined: 1.The K-O hydrostratigraphic unit, consisting of Holocene and Cretaceous sediments, is characterized by alternating vertical and horizontal groundwater flow controlled by zones of low ... Show Abstract

Hackbarth, D.A.  Nastasa, N.  1979-01-01

ESR 2002-02

Precambrian Basement of the Western Canada Sedimentary Basin in Northern Alberta

The Early Proterozoic Athabasca Group covers a limited portion of the basement south of Lake Athabasca; north of Lake Athabasca, the crystalline basement is exposed in the northeastern corner of the province. The aeromagnetic domains are routinely ... Show Abstract

Pana, D.I.  2003-03-01

ESR 1962-02

Geology of the Colin Lake District, Alberta

The geology of a 75 square mile area in the Precambrian Shield of northeastern Alberta is shown on a colored map of a scale of 2 inches to 1 mile. The predominant feature of this map area is the Colin Lake synclinorium whose folded axis plunges ... Show Abstract

Godfrey, J.D.  Peikert, E.W.  1964-01-01