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A Miniature “Dyke” Echelon

Published online by Cambridge University Press:  01 May 2009

William N. Gilliland
William N. Gilliland
Affiliation:
Department of Geology, University of Nebraska, Lincoln, Nebraska, U.S.A.
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Abstract

A specimen of shale containing an echelon of quartz-filled vertical tension fractures which merge “at depth” with a single filled fissure dipping 65 degrees confirms, in general, E. M. Anderson's interpretation of dyke echelons. Also illustrated are a change in manner of stress relief and an upward diminution of strain.

Type
Articles
Information
Geological Magazine , Volume 100 , Issue 5 , October 1963 , pp. 424 - 427
Copyright
Copyright © Cambridge University Press 1963

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References

REFERENCES

Anderson, E. M., 1951. The Dynamics of Faulting. London.Google Scholar
Chamberlin, R. T., 1919. A peculiar belt of oblique faulting. J. Geol., 27, 602–613.Google Scholar
Chamberlin, R. T., 1940. Disatraphic behaviour around the Bighorn Basin. J. Geol., 48, 673–716.CrossRefGoogle Scholar
De Sitter, L. U., 1956. Structural Geology. New York.Google Scholar
Eaton, J. E., 1933. Long Beach, California, earthquake of 10th March, 1933. Bull. Amer. Ass. Petrol. Geol., 17, 732–738.Google Scholar
Fath, A. E., 1920. The origin of the faults, anticlines, and buried “Granite Ridge” of the northern part of the Mid-Continent Oil and Gas Field. Prof. Pap. U.S. geol. Surv., 128-c, p. 75–84.Google Scholar
Russell, W. L., 1955. Structural Geology for Petroleum Geologists. New York.Google Scholar