The bases of seismic microzoning of the territories with difficult engineering-geological conditions (on the example of the Black Sea coast of North-West Caucasus)
The paper considers the territory of the Black Sea coast of North-West Caucasus, to determine the complexity and the degree of variability of the engineering-geological conditions as factors of the degree of a local seismic hazard changing. A complex studying of the territory has been executed, the major engineering-geological factors defining the specifics of microseismic zoning, have been defined. The engineering-geological and seismic properties of the main stratigraphic-genetic complexes and engineering-geological elements have been analyzed. An influence of the soil conditions on seismic intensity has been specified, a calculation of the sizes of an increment of the seismic intensity for the typical conditions by means of a method of seismic rigidities has been executed. An assessment of the spatial variability of the possible sizes of an increment of seismic intensity at the sites with standard geological sections by geostatistical methods has been made. A model of a total size of the increment of the seismic intensity in the explored territory has been developed. It has been established that elements of a rank of engineering-geological subdistricts and sites, which are an analog of seismic microdistricts, are the most uniform in engineering-geological and seismic properties.