Hailinskiy earthquake (8 march 1991) tectonic phenomenon of south-western part of Koryak highlandsv
Goal. The paper reveals geostructural conditions of foreshocks and aftershocks swarm location for the strong (M=6.6) Khailinsky earthquake on the south margin of the Koryak Late Mesozoic micro-continent on the northeast of Asia. The margin is an active junction of the continent and the Olyutor Paleogene tectonic zone and is manifested at the surface in the Koryak seismic belt. A swarm of earthquakes is located within the north margin of the Olyutor Paleogene tectonic zone. Methods.