Признаки сильных землетрясений в карстовых областях (на примере Горного Крыма)
Аннотация
Mountain karst massifs have some special features which determine passing of seismic waves. Paleoseismic information may be obtained from a number of karst features, such as breaks and displacements of the cave passages, distorted limestone blocks, corrosion-gravitation landforms, debaris resulting from collapse and chemogenic sediments precipitates from water solutions in the karst cavities.
Рецензия
Для цитирования:
Дублянский В.Н. Признаки сильных землетрясений в карстовых областях (на примере Горного Крыма). Геоморфология и палеогеография. 1995;(1):38-46.
For citation:
Dublyansky V.N. Signs of intense earthquakes in karst areas (with special reference to the Mountain Crimea). Geomorfologiya i Paleogeografiya. 1995;(1):38-46.