Earthquake-induced deformation at archaeological sites in southeastern Gorny Altai (Siberia, Russia)

Deev, E.; Borodovskiy, A.; Entin, A.

Статья опубликована в высокорейтинговом журнале

Информация о цитировании статьи получена из Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 31 июля 2024 г.

Авторы: Deev E., Borodovskiy A., Entin A.
Журнал: Archaeological Research in Asia
Том: 34
Номер: 2
Год издания: 2023
Издательство: Elsevier B.V.
Местоположение издательства: Netherlands
Первая страница: 1
Последняя страница: 13
Номер статьи: 100431
DOI: 10.1016/j.ara.2023.100431
Аннотация: Archaeoseismic studies in the Kurai Fault Zone in southeastern Gorny Altai (Siberia, Russia) reveal signatures of deformation caused by paleoearthquakes to burial and memorial sites (mound, khereksur, stone heap, stone enclosures), megaliths (steles), and irrigation ditch (suvak), which were located at the front of fault scarps or in their vicinity. The seismic motions left numerous traces of deformation: displaced of cairns of mound and khereksur; bending, displacement and rotation of parts of the khereksur's walls; bending stone structures at scarp crests; tilted and rotated enclosure's stone slabs; offset irrigation ditch; the displacement is most often directed. Dating of the archaeological site provides lower age bounds to the earthquakes. They all occurred for the past 3000 years, while the youngest events, ∼1.2 ka BP and no older than 1000 CE, were located in the northern Kurai and Kokorya basins, respectively. The deformation features in the mounds have bearing on the coseismic slip geometry.
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Earthquake-induced deformation at archaeological sites in southeastern Gorny Altai (Siberia, Russia)статья

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