Следы сильных землетрясений прошлого в рельефе Горного Алтая
Аннотация
Paleoseismogeological field researches in the south-eastern part of Altai Mts. took place in the 1996- and 1997. Seismodislocations of earlier unknown earthquakes was found in this region; their mapping and investigation ill the mine-workings were fulfilled. Primary seismodislocations may be-seen in recent landforms as low cliffs of large extent and as thrusts in cross-sections. Landfalls, landslides and stone avalanches represent secondary seismodislocations. Their C14 dating lies in the range 8000-200 b.p. The data obtained allow considering the south-east part, of Altai Mts. region to be apparently high seismic.
Об авторах
Е. А. РогожинРоссия
Б. М. Богачкин
Россия
Ю. В. Нечаев
Россия
С. Г. Платонова
Россия
В. П. Чичагов
Россия
А. О. Чичагова
Россия
Рецензия
Для цитирования:
Рогожин Е.А., Богачкин Б.М., Нечаев Ю.В., Платонова С.Г., Чичагов В.П., Чичагова А.О. Следы сильных землетрясений прошлого в рельефе Горного Алтая. Геоморфология и палеогеография. 1999;(1):82-95.
For citation:
Rogozhin E.A., Bogachkin B.M., Nechayev Yu.V., Platonova S.G., Chichagov V.P., Chichagova O.A. Traces of ancient earthquakes in the Altai mountains. Geomorfologiya i Paleogeografiya. 1999;(1):82-95.
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