Publication | Closed Access
Attenuation of intensity with epicentral distance in the Philippines
71
Citations
2
References
1980
Year
GeophysicsApplied GeophysicsTectonicsPhilippine RegionEngineeringSeismologyEarthquake SourceGeographySeismic ImagingSan Andreas RegionIntensity Attenuation EquationEarthquake HazardsEarthquake RuptureGeophysical Signal ProcessingEpicentral DistanceSeismic HazardEarth ScienceGeodesy
abstract With data from 83 earthquakes in the Philippine region, an intensity attenuation equation is derived in the form: I(R) − Io = 4.01 − 0.015 R − 2.40 log R. This compares very favorably with results for a tectonically similar region, the San Andreas region, derived by Howell and Schultz (1975).
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