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REP 35

Coals of Alberta, Their Occurrence, Analysis and Utilization

Coals of Alberta, Their Occurrence, Analysis and Utilization Coal-bearing beds in Alberta occur in three different geological horizons namely, the Edmonton, the Belly River, and the Blairmore-Kootenay. The first two horizons are in the Upper ... Show Abstract

Stansfield, E.  Lang, W.A.  1943-01-01

REP 54

Twenty-Ninth Annual Report of the Research Council of Alberta: 1948

Twenty-Ninth Annual Report of the Research Council of Alberta: 1948 The annual report lists the Research Council of Alberta's projects for 1948, including bituminous sand, gasoline, clay, water, soil and natural gas. Place Keywords 72e 72l 72m 73d ... Show Abstract

Research Council of Alberta  1949-03-01

REP 47

Annual Report of the Research Council of Alberta: 1945

Annual Report of the Research Council of Alberta: 1945 The annual report lists the Research Council of Alberta's projects for 1945, including bituminous sand, fuels, clay, soil and natural gas. Place Keywords 72e 72l 72m 73d 73e 73l 73m 74d 74e ... Show Abstract

Research Council of Alberta  1946-03-01

REP 46

Alberta Coals and Automatic Domestic Stokers

Laboratory investigation and questionnaire as sources of information. -- In 1942 the Research Council of Alberta decided to carry out an investigation on the suitability of Alberta coals for use in automatic domestic stokers; and funds for this ... Show Abstract

Stansfield, E.  Genge, C.A.  1945-03-01

REP 44

Annual Report of the Research Council of Alberta: 1943

Annual Report of the Research Council of Alberta: 1943 The annual report lists the Research Council of Alberta's projects for 1943, including bituminous sand, natural resources, fuels and coal ash. Place Keywords 72e 72l 72m 73d 73e 73l 73m 74d ... Show Abstract

Research Council of Alberta  1945-02-01

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 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 063

The Diamond Potential of Alberta

Diamonds have been discovered in surficial sediments west of Edmonton at locations near Evansburg and Hinton, in southern Alberta in the Sweetgrass Hills area, and in Cretaceous-Tertiary sediments southeast of Red Deer. There are numerous diamond ... Show Abstract

Dufresne, M.B.  Eccles, D.R.  McKinstry, B.  Schmitt, D.R.  Fenton, M.M.  Pawlowicz, J.G.  Edwards, W.A.D.  1996-01-01

BUL 065

Northern Alberta Kimberlite Province: The First 20 Years

Northern Alberta Kimberlite Province: The First 20 Years The report comprehensively summarizes the events that led to the discovery of kimberlitic rocks in Alberta, the geological setting in which they were discovered, geochronology, physical and ... Show Abstract

Eccles, D.R.  2011-11-01

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

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