Value Of Ceramic Tests In Subsurface Correlation Of Cretaceous Shales In Central Wyoming

The American Institute of Mining, Metallurgical, and Petroleum Engineers
C. E. Dobbin
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
12
File Size:
1206 KB
Publication Date:
Jan 1, 1931

Abstract

THE identification of rock formations by a study of certain physical characteristics of burned samples was introduced in Wyoming in 1,926, when W. G. Buckles, superintendent. of the brick department of the Parco Development Co., reported to officials of the Producers & Refiners Corpn. that shales from the Cretaceous and older formations exposed between Parco and Rawlins exhibited distinctive coloration and textural features when burned in a standard brick kiln at temperatures ranging between 1000° and 3000° F. In collaboration with Elfred Beck, chief geologist of the Producers & Refiners Corpn., Buckles later burned cuttings and cores from several Wyoming wildcat wells in a standard kiln and successfully identified certain subsurface formations which had not been satisfactorily identified by other means. The results of their investigations were outlined in papers presented by Beck before the American Association of Petroleum Geologists at San Francisco in March, 1928, and by Buckles at. a joint meeting of the Rocky Mountain Oil and Gas Association and the Production Division of the American Petroleum Institute at Casper in November, 1928. These papers have not been published. The investigations set forth in this paper were carried out for. the purpose of determining the value of certain ceramic tests in assisting the petroleum engineers of the U. S. Geological Survey to identify well cuttings that represent Cretaceous shales penetrated beneath unconformable Tertiary formations in central, and eastern Wyoming, but that yield neither lithologic nor paleontologic criteria for satisfactory correlations with distinctive weathered outcrops. The investigations were made in the chemical laboratories of the Geological Survey at- Midwest, Wyo., and consisted of studying certain physical characteristics of burned bricks from representative outcrop samples of unweathered Cretaceous shales and of similarly burned cuttings of the same shales collected from wells in the Salt Creek oil field.
Citation

APA: C. E. Dobbin  (1931)  Value Of Ceramic Tests In Subsurface Correlation Of Cretaceous Shales In Central Wyoming

MLA: C. E. Dobbin Value Of Ceramic Tests In Subsurface Correlation Of Cretaceous Shales In Central Wyoming. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1931.

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