Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Natural Gas in Alberta

View through CrossRef
Abstract Alberta is the only western Canadian province in which a production of natural gas and oil has been developed. Natural gas was discovered in 1885, and at present there are seven producing fields and 330 miles of main pipe lines. Alberta is divided into eight structural provinces; four of these are gas-producing regions, one is prospective, and the others are of no interest as gas areas. The stratigraphic column has three persistent features, namely, the Palaeozoic limestone section, the profound unconformity superimposed on it, and the succeeding Mesozoic section of transgressive-regressive deposits. The Turner Valley field is the only developed field producing from formations of Palaeozoic age, though there have been significant discoveries suggesting that other fields are present. A theory is advanced in this paper to explain a Palaeozoic origin for the heavy oil and bitumen in the basal sandstones of the Mesozoic. The gas accumulations in the basal sands were later derived from the bitumen and heavy oil. The reserves of gas in Palaeozoic rocks and the basal sands of Mesozoic age are large. During Mesozoic time there were at least five marine transgressions of the seas, and there is a marked relation between the marine shales and the gas-bearing horizons in rocks of Mesozoic age. Gas is generally found in the sandstones immediately overlying, within, or immediately underlying the marine shales. Gas is found in rocks of Jurassic age in the Southern Plains and the Southern Foothills. The reserves are estimated to be about 80 billion cubic feet. Only small amounts of gas are now produced from Jurassic horizons. Gas is found in marine formations of Comanche age in northern Alberta, but there are no developed fields, and the reserves are unknown. There are three gas-bearing horizons in the Colorado (Gulf series), with several fields, including the Foremost, Viking, and Medicine Hat fields. The possible reserves are large and are probably in excess of 600 billion cubic feet. The Lower Montana and Upper Montana rocks (Gulf series) produce gas over large areas, but the yields are small and the horizons are of minor importance. There are no marine rocks of post-Mesozoic age, and the only gas occurrences are small flows from lacustrine deposits. The analyses of natural gases in Alberta when arranged according to geologic horizons and localities appear to show an increase in the proportion of higher hydrocarbons to methane in a westerly direction for a given gas-bearing horizon. This may be due to the effect on the source material of increasing metamorphism westward.
American Association of Petroleum Geologists
Title: Natural Gas in Alberta
Description:
Abstract Alberta is the only western Canadian province in which a production of natural gas and oil has been developed.
Natural gas was discovered in 1885, and at present there are seven producing fields and 330 miles of main pipe lines.
Alberta is divided into eight structural provinces; four of these are gas-producing regions, one is prospective, and the others are of no interest as gas areas.
The stratigraphic column has three persistent features, namely, the Palaeozoic limestone section, the profound unconformity superimposed on it, and the succeeding Mesozoic section of transgressive-regressive deposits.
The Turner Valley field is the only developed field producing from formations of Palaeozoic age, though there have been significant discoveries suggesting that other fields are present.
A theory is advanced in this paper to explain a Palaeozoic origin for the heavy oil and bitumen in the basal sandstones of the Mesozoic.
The gas accumulations in the basal sands were later derived from the bitumen and heavy oil.
The reserves of gas in Palaeozoic rocks and the basal sands of Mesozoic age are large.
During Mesozoic time there were at least five marine transgressions of the seas, and there is a marked relation between the marine shales and the gas-bearing horizons in rocks of Mesozoic age.
Gas is generally found in the sandstones immediately overlying, within, or immediately underlying the marine shales.
Gas is found in rocks of Jurassic age in the Southern Plains and the Southern Foothills.
The reserves are estimated to be about 80 billion cubic feet.
Only small amounts of gas are now produced from Jurassic horizons.
Gas is found in marine formations of Comanche age in northern Alberta, but there are no developed fields, and the reserves are unknown.
There are three gas-bearing horizons in the Colorado (Gulf series), with several fields, including the Foremost, Viking, and Medicine Hat fields.
The possible reserves are large and are probably in excess of 600 billion cubic feet.
The Lower Montana and Upper Montana rocks (Gulf series) produce gas over large areas, but the yields are small and the horizons are of minor importance.
There are no marine rocks of post-Mesozoic age, and the only gas occurrences are small flows from lacustrine deposits.
The analyses of natural gases in Alberta when arranged according to geologic horizons and localities appear to show an increase in the proportion of higher hydrocarbons to methane in a westerly direction for a given gas-bearing horizon.
This may be due to the effect on the source material of increasing metamorphism westward.

Related Results

Economics Of Solar Heating In Alberta
Economics Of Solar Heating In Alberta
Abstract Natural gas prices in Alberta are anticipated, after having reached Btu equivalence with crude oil prices, to inflate at rates very close to overall infl...
The Relative Economics of Recovering And Upgrading Alberta's Hydrocarbon Resources
The Relative Economics of Recovering And Upgrading Alberta's Hydrocarbon Resources
Summary In an attempt to provide a current appreciation of the comparative economics of the various Alberta hydrocarbon feedstocks in the petrochemical, electric ...
Comparisons of Pore Structure for Unconventional Tight Gas, Coalbed Methane and Shale Gas Reservoirs
Comparisons of Pore Structure for Unconventional Tight Gas, Coalbed Methane and Shale Gas Reservoirs
Extended abstract Tight sands gas, coalbed methane and shale gas are three kinds of typical unconventional natural gas. With the decrease of conventional oil and gas...
Gas Water Deliverability Considerations
Gas Water Deliverability Considerations
Abstract When natural gas from high pressure and temperature reservoir is produced, due to cooling of gas in wellbore tubing and in gas gathering pipelines, the a...
Maximizing Value In Gas Marketing
Maximizing Value In Gas Marketing
Abstract Discuss the evolution of gas marketing from deregulation in late 1985 to the present, identifying the key changes that have taken place from the perspect...
Critical Gas Saturation During Depressurisation and its Importance in the Brent Field
Critical Gas Saturation During Depressurisation and its Importance in the Brent Field
Critical Gas Saturation During Depressurisation and its Importance in the Brent Field. Abstract After some 20 years of pressure ...
Unconventional Reservoirs: Basic Petrophysical Concepts for Shale Gas
Unconventional Reservoirs: Basic Petrophysical Concepts for Shale Gas
Abstract Unconventional reservoirs have burst with considerable force in oil and gas production worldwide. Shale Gas is one of them, with intense activity taking pla...
Understanding Unconventional Gas Reservoir Damages
Understanding Unconventional Gas Reservoir Damages
Abstract It is estimated that there are large reserves of unconventional gas located throughout the world, including coalbed methane, shale gas and tight gas sand...

Back to Top