ABSTRACT

Discovered in 1954, Wimborne oil and gas field lies in southwestern Alberta, fifty miles northeast of the city of Calgary. The main oil and gas accumulation occurs in a dolomitized reef of Devonian Leduc age, with a secondary accumulation occurring at a higher elevation in the biostromal development in the Nisku formation of the Devonian Winterburn group. Nineteen wells have been drilled to the Leduc reef in the field area, of which thirteen are on steady production. No production is presently being taken from the Nisku.

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