PlanetPhysics/Geiger's Method
Geiger's method [1] is an iterative procedure using Gauss-Newton optimization to determine the location of an earthquake, or seismic event. Originally his method was developed to obtain the origin time and [[../Epicentre/|Epicentre]] but it is easily extended to include the [[../FocalDepth/|Focal Depth]] for [[../Hypocenter/|Hypocentre]] determination.
Given a set of arrival times find the origin time and the hypocentre in cartesian coordinatios which minimize
the objective [[../Bijective/|function]]
Here, is the difference between observed and calculated arrival times
and the unknown [[../Parameter/|parameter]] [[../Vectors/|vector]] is
In [[../Matrix/|matrix]] form (1) becomes
The Gauss--Newton procedure requires an initial guess of the sought parameters, denoted here as
which are then used to calculate the adjustment vector
in
The Jacobian matrix is defined as
The partial derivatives are evaluated at the initial guess, or trial vector, . Equation (45) can be rewritten as
Using (46) and an initial guess an adjustment vector can be calculated. The initial guess can then be updated and used as the inital guess in the next run of the [[../RecursiveFunction/|algorithm]]. In this manner the sought parameters can be determined to some tolerance.
All Sources
References
- β 1.0 1.1 Geiger, L., Probability method for the determination of earthquake epicenters from the arrival time only. {\it Bull. St. Louis Univ.} vol. 8, pp. 60-71.
- β Lee, W. H. K. and Stewart, S. W. {\it Principles and Applications of Microearthquake Networks,} Academic Press, New York. 1981
- β Gibowicz, S. J. and Kijko, A. {\it An Introduction to Mining Seismology,} Academic Press, New York. 1994.