Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Bulletin of the Seismological Society of America Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Bulletin of the Seismological Society of America; February 1967; v. 57; no. 1; p. 99-112
© 1967 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
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
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by STEVENS, A. E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

S-wave earthquake mechanism equations

ANNE E. STEVENS

DIVISION OF SEISMOLOGY DEPARTMENT OF MINES AND TECHNICAL SURVEYS, OTTAWA 3, ONTARIO Canada

Abstract

The orientation of force axes at the focus of an earthquake can be calculated using S polarization angles in a set of S-wave mechanism equations (Stevens, 1964). These equations are rederived in this paper in a more direct manner and each equation is shown to represent the plane of polarization of S at a point on the focal sphere. Two special cases of the general mechanism equations, the single-couple and the double-dipole focal mechanism, have been used to study a number of earthquakes.

Mechanism solutions for seven Kamchatka-Kuril earthquakes and one Alaskan earthquake discussed previously (Stevens, 1964) are reconsidered. The former single couple solutions for the earthquakes of 1949 Nov 3, 1951 Nov 6, 1952 Nov 5 and 1957 Dec 17 are rejected. No meaningful solution of either type is considered possible with the limited data available. The single couple solution for the earthquake of 1955 April 17 is changed to a double dipole solution; the single couple solution for the earthquake of 1958 July 10 and the double dipole solution for 1953 Nov 10 are altered slightly; the single couple solution of 1960 July 25 is changed significantly.

Mechanism solutions are presented for five Aleutian earthquakes using S polarization angles published by Stauder and Udias (1963). All five earthquakes are the double dipole type. The principal compressive stress axes are nearly horizontal and perpendicular to the trend of the Aleutian arc, the intermediate stress axes are horizontal and trend along the arc and the principal tensile stress axes dip steeply under the continent.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
A. UDIAS and D. BAUMANN
A computer program for focal mechanism determination combining P and S wave data
Bulletin of the Seismological Society of America, April 1, 1969; 59(2): 503 - 519.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
A. E. STEVENS and J. H. HODGSON
A study of P nodal solutions (1922-1962) in the Wickens-Hodgson Catalogue
Bulletin of the Seismological Society of America, June 1, 1968; 58(3): 1071 - 1082.
[Abstract] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Seismological Society of America