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SPE 014

Quaternary Geology and Dispersal Patterns, Winagami Region, Alberta

Surficial deposits are associated with ice advance and stagnation, deglaciation and post-glacial processes. [...]glaciolacustrine silt, clay and diamict blanket the majority of the region. Sediments of the glaciofluvial, aeolian, colluvial, ... Show Abstract

Balzer, S.A.  2000-04-01

ESR 2001-04

Petrographic, Mineralogical and Lithogeochemical Study of Core from Three Drillholes into the Steen River Structure, Northern Alberta

In general, the similarity of its structural geometry, stratigraphy and breccia unit to other known meteorite impact features has supported an extraterrestrial (astrobleme) origin. [...]some prior workers have suggested, based on geophysical ... Show Abstract

Molak, B.  Balzer, S.A.  Olson, R.A.  Waters, E.J.  2002-05-01

OFR 1994-20

Quaternary Stratigraphy and Surficial Geology Peace River-Winagami Region Year One Report For The End Fiscal Year 1993-94

A reconnaissance survey of the southern half of the Peace River map area (84C/w 1/2) revealed the presence of predominantly two types of surficial glacial deposit they are: morainal and glaciolacustrine. Indicator minerals were picked from thick ... Show Abstract

Balzer, S.A.  Leslie, L.E.  Fenton, M.M.  1994-10-01

OFR 1995-09

Quaternary Stratigraphy and Surficial Geology Peace River-Winagami Region, Alberta; Year Two Report For The End Fiscal Year 1994-95

The surficial morainal deposits, flutes, and morainal ridges which are generally situated in the uplands of the Clear and Whitemud Hills, are evidence of an unobstructed southerly flowing Laurentide Ice Sheet. Deglaciation is marked in the uplands ... Show Abstract

Balzer, S.A.  Leslie, L.E.  Fenton, M.M.  1995-04-01