The Osmussaar earthquake on October 25, 1976: Macroseismic analysis, seismotectonics, and focal mechanism

The paper presents additional evidence on macroseismic features (mostly in the near-field zone), morphostructure, and tectonics in the source area of the strongest (M = 4.7-4.8), instrumentally recorded earthquake on the western East European platform. Its macroseismic field is described more accurately and is compared with seismotectonics based on