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Bulletin of the Seismological Society of America; February 1966; v. 56; no. 1; p. 35-42
© 1966 Seismological Society of America
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Deduction of earth strains from survey data

F. C. FRANK

UNIVERSITY OF BRISTOL, BRISTOL, England

Abstract

In deducing earth strains from repeated triangulation surveys, it is advantageous to extract the shear components of strain Formula separately. Unlike the dilation and rotation components of strain, Formula, these shear components can be determined locally, each triangle giving one measurement for {gamma}1 and {gamma}2, without requiring knowledge from adjoining areas. It follows that it should be possible to extract much more and better information about the shear strains from existing survey data than has been extracted hitherto.




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