Figure 16. The distribution of the different types of the paleoseismic dislocations in time: (1-2) results of 14C dating at the Radiocarbon Laboratory of the Institute of Geography and Geological Institute (GIN), Russian Academy of Sciences: (1) lower age boundary of seismic event; (2) age of earthquake dislocations; (3) upper age limit of seismic event; (4) modern soil sample (the size of the rectangle agrees with the size of the error); (5) numbers of samples used in radiocarbon analysis; (16) age of volcanic eruption; (17) age of seismic event.