Abstract

"It is generally accepted that there is lack of parallelism between surface and subsurface beds and between the productive sands in the Beggs District, a condition similar to that which obtains in the Cushing Field. The explanation of this condition as given on page 31, Bulletin 658, U.S. Geological Survey, is: 1) The difference in resistance to compression of the hard and soft beds of which the formations of the Cushing Field are composed; 2) The lenticular form of the Bartlesville sand (the equivalent of the Glen; Gas of Morris pool); 3) One or more unconformities between surface beds and the Bartlesville sand; 4) Folding during deposition; 5) Cross folding"--Pages 14-15.

Department(s)

Mining Engineering

Degree Name

Professional Degree in Mining Engineering

Comments

Illustrated by author.

Publisher

Missouri School of Mines and Metallurgy

Publication Date

1921

Pagination

33 pages, 3 plates

Geographic Coverage

Oklahoma

Rights

© 1921 J. Chas. Miller, All rights reserved.

Document Type

Thesis - Open Access

File Type

text

Language

English

Subject Headings

Geology -- OklahomaBeds (Stratigraphy)Oil fields -- OklahomaGas fields -- Oklahoma

Thesis Number

T 430

Print OCLC #

5953607

Electronic OCLC #

849899598

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