A catastrophic holocene event in the lake bottom sediments of the Kola region (northeastern Fennoscandian shield)     

S. B. Nikolaeva  N. B. Lavrova  D. B. Denisov 《Doklady Earth Sciences》2017,473(1):308-312

Horizons with seismogenic sediments are revealed in the bottom sediments of the lake basins in the southwestern Kola Peninsula. In the borehole cores, they are represented by material that sharply differs from the overlying and underlying sediments: fragments of gyttia, siltstone, wood, sand, and peat that are embedded in the sapropelic matrix and look like breccia. These sediments reflect a strong catastrophic event from the Holocene that occurred 6000–5400 ¹⁴C yr BP. The seismic events that happened in the middle Holocene in the northeastern Fennoscandian shield indicate a significant role of the tectonic component in the damping process of relaxation of the Earth’s crust in the unloading of the recent glacier cover.  相似文献   

The Use of Mini-Drifters in Coastal Current Measurements Conducted Concurrently with Satellite Imaging     

Lavrova  O. Yu.  Soloviev  D. M.  Strochkov  A. Ya.  Nazirova  K. R.  Krayushkin  E. V.  Zhuk  E. V. 《Izvestiya Atmospheric and Oceanic Physics》2020,56(9):1022-1033

Izvestiya, Atmospheric and Oceanic Physics - The results of field measurements of coastal currents using Lagrangian mini-drifters are presented. The drifter experiments were conducted concurrently...  相似文献