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Osnovnyye cherty tektoniki Kaspiyskogo morya po dannym morskikh geofizicheskikh issledovaniy

Osnovnyye cherty tektoniki Kaspiyskogo morya po dannym morskikh geofizicheskikh issledovaniy

International Geology Review 12: 80-99

An analysis of the main tectonic features of the Caspian sea, USSR, on the basis of marine geophysical data, shows that the sea is located within the Precambrian Russian and epi-Hercynian Scythian platform regions and the Alpine geosynclinal province. Marine geophysical methods have added many details about the structure and salt tectonics of the basin. The ancient age of the Caspian central massif is supported by relationships between the Karabogaz arch and the meganticline of Turkey. Basically the south Caspian represents a remnant of the ancient Tethys trough; the middle and north Caspian are epiplatforms. The western part is associated with a post-Alpine platform and its foredeeps, with the middle Caspian only recently involved in its subsidence.

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