THE DESIGN OF OPTIMUM NETWORKS FOR AFTERSHOCK RECORDINGS

Citation
M. Hardt et F. Scherbaum, THE DESIGN OF OPTIMUM NETWORKS FOR AFTERSHOCK RECORDINGS, Geophysical journal international, 117(3), 1994, pp. 716-726
Citations number
31
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
0956540X
Volume
117
Issue
3
Year of publication
1994
Pages
716 - 726
Database
ISI
SICI code
0956-540X(1994)117:3<716:TDOONF>2.0.ZU;2-N
Abstract
The analysis of aftershocks is more and more recognized by the seismol ogical community as being an essential tool to improve the understandi ng of the earthquake faulting process, as well as of the various facto rs contributing to the generation of earthquake damage. In this contex t, the success or failure of aftershock monitoring programs depends to a large degree on the performance of the mobile seismic network deplo yed. In comparison with pure location networks, for aftershock monitor ing networks the situation is complicated by the fact that they have t o perform well for additional tasks such as determination of focal mec hanisms, source-parameter estimation, tomographic experiments etc. We have developed a method to design optimum networks for aftershock reco rdings based on the technique of simulated annealing. If aftershock da ta are not yet available for the design of a mobile network, they are simulated for the optimization process from the mainshock-source param eters. Different objective functions to quantify network performance f or each intended task are used. For the location problem it is based o n the average confidence volume of hypocentral locations while for the focal mechanism determination it is derived from the distribution of rays on the focal sphere. For the tomography problem, the resolution m atrix of the inverse problem is used. Furthermore, for each station in dividual noise levels can be assumed. Optimization for multiple tasks is performed in a sequential way with highest priority given to the lo cation problem. The method has been applied to the Roermond earthquake of 1992 April 13. Optimum subsets of the existing ad hoc multinationa l temporary network for aftershock recordings of this event have been evaluated.