Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; August 1975; v. 65; no. 4; p. 845-854
© 1975 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by SINGH, S. K.
Right arrow Articles by SABINA, F. J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Epicentral deformation based on the dilatancy-fluid diffusion model

SHRI KRISHNA SINGH and FEDERICO J. SABINA

INSTITUTO DE GEOFISICA UNIVERSIDAD NAL. AUTONOMA DE MEXICO, C.U., MEXICO 20, D.F.
INSTITUTO DE INGENIERIA UNIVERSIDAD NAL. AUTONOMA DE MEXICO, C.U., MEXICO 20, D.F.

Abstract

The dilatancy-fluid diffusion model of the earthquake mechanism implies deformation of the epicentral area. Based on a result in the theory of thermoelasticity, we present a method for computing such deformation. Details are given for a dilating sphere and a dilating infinite cylinder buried in an elastic half-space. Given the volumetric strain of the dilatant region, the deformation measurements could be used to estimate the magnitude of the impending earthquake. Alternatively, a constraint on the volumetric strain can be obtained from deformation measurements before earthquakes that are preceded by dilatancy.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1975 by the Seismological Society of America.