
В работе рассмотрены современная сейсмичность и возможные геодинамические модели сжатия осадочной толщи Южно-Каспийской впадины, которые позволяют объяснить феномен резкого изменения уровня Каспия The article considers the seismic geodynamic model of compression sedimentary strata of the South Caspian depression, which allows to explain the phenomenon of abrupt changes in sea level as a result of dilatancy expansion of the sedimentary cover.
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