Complex structural-geomorphological, structural-morphological and fractal analysis of vertical newest movements of the Kerch Peninsula
https://doi.org/10.33623/0579-9406-2019-5-19-29
Abstract
A comprehensive analysis was carried out for the Kerch Peninsula using morphostructural, structural and geomorphological methods as well as determining the fractal dimension D of the driangle system. It has been discovered that increased values of the field of fractal dimension D correlate well with the total uplift amplitude during the Pleistocene and Holocene, and worse with the latest structures formed during the conerosion stage of development. It can be concluded that the fractal approach for the quantitative analysis of the driangle system pattern gives good results in identifying the latest movements, and is less effective in identifying the latest structures. The further development of the fractal analysis method is promising, with the inclusion of other driangle system parameters widely used in structural-geomorphological analysis.
About the Authors
D. A. SimonovRussian Federation
Faculty of Geology, 119991, Moscow, GSP-1, Leninskiye Gory, 1
V. S. Zakharov
Russian Federation
Faculty of Geology, 119991, Moscow, GSP-1, Leninskiye Gory, 1;
141980, MO, Dubna, University st., 19
G. V. Bryantseva
Russian Federation
Faculty of Geology, 119991, Moscow, GSP-1, Leninskiye Gory, 1;
141980, MO, Dubna, University st., 19
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Review
For citations:
Simonov D.A., Zakharov V.S., Bryantseva G.V. Complex structural-geomorphological, structural-morphological and fractal analysis of vertical newest movements of the Kerch Peninsula. Moscow University Bulletin. Series 4. Geology. 2019;(5):19-29. (In Russ.) https://doi.org/10.33623/0579-9406-2019-5-19-29