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Prediction equations for macroseismic intensity are the backbone of seis- mic hazard assessment, of source parameter estimation, and of shake map generation in cases where an output in terms of intensity is desired. This is especially required when a direct relation to the damage associated with ground shaking is of interest or if ground shaking estimates will be used for informing nonseismologists such as emer- gency response teams or the general public. In the current study we derive ground- motion prediction equations for macroseismic intensity valid for the Marmara Sea region, northwest Turkey. The relations have a physical basis and are easy to imple- ment for the user. In one relation, the finite extent of the fault rupture is accounted for by defining distance as the Joyner-Boore distance leading to the relation

Attenuation of Macroseismic Intensity: A New Relation for the Marmara Sea Region, Northwest Turkey