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The structure of zone of subduction in region of joint of the Black Sea crust and of the Crimea crust is obtained in the result of reinterpretation of data of Deep Seismic Sounding profiles with usage of new computer technologies. Rift zone and zones anomalously of low velocities in district of the Andrusov ridge are distinguished. These structures are traced and interpreted on the seismic cross sections and map-slices.
№ | Имя | Описание | Имя файла | Размер | Добавлен |
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1. | Полный текст | Piip_Ermakov_EAGE_65th_Conference__Exhibition_2003.pdf | 719,4 КБ | 21 февраля 2019 [ERMAKOV] |