Moscow, Russian Federation
Russian Federation
Schmidt Institute of the Physics of the Earth Russian Academy of Sciencies
UDC 55
UDC 550.34
UDC 550.383
CSCSTI 37.01
CSCSTI 37.15
CSCSTI 37.25
CSCSTI 37.31
CSCSTI 38.01
CSCSTI 36.00
CSCSTI 37.00
CSCSTI 38.00
CSCSTI 39.00
CSCSTI 52.00
Russian Classification of Professions by Education 05.00.00
Russian Library and Bibliographic Classification 26
Russian Trade and Bibliographic Classification 63
BISAC SCI SCIENCE
Using the Baltic Shield as an example, various methods for calculating the integral morphometric parameter (𝐹) based on a set of geomorphological data processed using fuzzy logic tools were tested. Comparison of the spatial distribution patterns of this parameter with the localization of epicenters of modern crustal earthquakes shows that it reflects the degree of seismotectonic activity to a certain extent. The best agreement was achieved when the initial morphometric parameters and the 𝐹 calculation algorithm were selected separately for each megablock – Kola-Karelian, Svecofennian, and Sveco-Norwegian. This can be explained by the significant influence of the geological structure on the relief. A similar result was achieved when calculating 𝐹 within blocks characterized by a certain type of recent stress state. However, the relationship between seismicity and the integral morphometric parameter 𝐹 is statistically significant when determining the latter by processing data on average heights, relief slopes and the difference in base surfaces of 3–4 orders using a fuzzy sum for the entire territory of the Baltic Shield.
morphometric analysis of relief, fuzzy logic, seismicity, Baltic Shield
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