SEISMICITY PATTERNS AND THE CHARACTERISTIC EARTHQUAKE IN THE CENTRAL MISSISSIPPI VALLEY, USA

Authors
Citation
Dh. Speidel, SEISMICITY PATTERNS AND THE CHARACTERISTIC EARTHQUAKE IN THE CENTRAL MISSISSIPPI VALLEY, USA, Engineering geology, 50(1-2), 1998, pp. 1-8
Citations number
25
Categorie Soggetti
Engineering, Geological","Geosciences, Interdisciplinary
Journal title
ISSN journal
00137952
Volume
50
Issue
1-2
Year of publication
1998
Pages
1 - 8
Database
ISI
SICI code
0013-7952(1998)50:1-2<1:SPATCE>2.0.ZU;2-A
Abstract
The magnitude-frequency distribution of the Armbruster-Seeber (1992) c atalog of the Central Mississippi valley earthquakes from 1811 to 1985 can be well described as a linear combination of three earthquakes po pulations each of which fits a normal distribution with respect to mag nitude. The mean magnitudes of the lower magnitude populations are con sistent with previous work based on a 1974-1991 catalog of the same ar ea. The presence of the high magnitude population, mean M=7.2, account s for the development of a characteristic earthquake pattern. This pat tern is very dependent on the assumed activity of the 7.2 population. The operating basis earthquake (144 years) of interest to structural e ngineers occurs in the region of greatest sensitivity to those assumpt ions about activity, thus complicating matters for design. (C) 1998 El sevier Science B.V. All rights reserved.