Bespalova H. Dynamics of Landslide Formation for the Middle Part of Dnieper River Valley, as Applied to Trypillya-Kaniv Site

Українська версія

Thesis for the degree of Candidate of Sciences (CSc)

State registration number

0404U000668

Thesis Registration Form

0404U000668.pdf

Applicant for

Specialization

  • 04.00.07 - Інженерна геологія

03-02-2004

Specialized Academic Board

Д 26.162.05

Essay

Based on statistically processed regime observations, long-term temporal changes of landslide formation were estimated as well as space-time regularities determined. Besides, landslide formation was forecasted for two types of geological environment. The first type involves landslides of Kyiv type, develope in Paleogene, Neogene and Quaternary flat-bedded deposits (Kyiv sub-region). The second one involves Jurassic, Cretaceous, Paleogene and Quaternary dislocated folded strucctures within the Kaniv dislocated region. For Kyiv sub-region landslide systems of two types were distihguished. according to geological and geomorphological features as well as mechanism and dynamics of their development. For Kaniv sub-region landslide formation was forecasted using landslide potential method. Clay soil microstructures were studied, and mechanism of landslide formation determined in accordance with specific clay horizon composing its base.

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Дисертація.doc

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