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; February 1984; v. 74; no. 1; p. 255-265
© 1984 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
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
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by LIU, Z.-R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Earthquake frequency and prediction

ZHENG-RONG LIU

SEISMOLOGICAL BUREAU OF YUNNAN PROVINCE, KUNMING, Peoples Republic of China

Abstract

The coefficient p in n(t) = n1t–p, where n(t) is the daily count of earthquakes and n1 is the number of earthquakes on the first day following a larger earthquake, is less double equals1 for foreshock sequences, {gtrsim}1 for double-main shock sequences, and »1 for aftershock sequences with a single largest earthquake. For p »1, the magnitude of the largest aftershock and the cutoff time of the aftershocks can be estimated. These observations are the basis for an earthquake prediction technique successfully used in the Peoples Republic of China (PRC).




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
G. Zhang, L. Zhu, X. Song, Z. Li, M. Yang, N. Su, and X. Chen
Predictions of the 1997 strong earthquakes in Jiashi, Xinjiang, China
Bulletin of the Seismological Society of America, October 1, 1999; 89(5): 1171 - 1183.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
P. Nyffenegger and C. Frohlich
Recommendations for determining p values for aftershock sequences and catalogs
Bulletin of the Seismological Society of America, October 1, 1998; 88(5): 1144 - 1154.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
H. K. GUPTA
Are ris events of M greater double equals 5 preceded by a couple of foreshocks of M greater double equals 4?
Bulletin of the Seismological Society of America, February 1, 1992; 82(1): 517 - 520.
[PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
S. K. SINGH and G. SUAREZ
Regional variation in the number of aftershocks (mb greater double equals 5) of large, subduction-zone earthquakes (Mw greater double equals 7.0)
Bulletin of the Seismological Society of America, February 1, 1988; 78(1): 230 - 242.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
R. A. PAGE
Comments on "Earthquake frequency and prediction" by Liu Z.-R.
Bulletin of the Seismological Society of America, October 1, 1986; 76(5): 1491 - 1496.
[PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
Z.-R. LIU
Reply to R. A. Page's "Comments on 'Earthquake frequency and prediction'"
Bulletin of the Seismological Society of America, October 1, 1986; 76(5): 1497 - 1499.
[PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
H. K. GUPTA and H. M. IYER
Are reservoir-induced earthquakes of magnitude greater double equals 5.0 at Koyna, India, preceded by pairs of earthquakes of magnitude greater double equals 4.0?
Bulletin of the Seismological Society of America, June 1, 1984; 74(3): 863 - 873.
[Abstract] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1984 by the Seismological Society of America.