The Structural–Formational Zoning of the Laptev Sea Shelf (Eastern Arctic)Geotectonics - Tập 56 - Trang 453-470 - 2022
A. D. Dzyublo, O. V. Grushevskaya, A. N. Obukhov, A. Yu. Makarova
In our research, the structural-formational zoning of the Laptev Sea shelf (Eastern Arctic) was performed, and description of the Taymyr (northwestern part of the Laptev Sea), Laptev (central part of the Laptev Sea), Gakkel (northern part of the Laptev Sea), Omoloy (eastern part of the Laptev Sea) and transitional Khatanga (southwestern part of the Laptev Sea) structural-formational zones, and the...... hiện toàn bộ
Paleoearthquakes in the Baikal region: Methods and results of timingGeotectonics - Tập 44 - Trang 158-175 - 2010
O. P. Smekalin, A. V. Chipizubov, V. S. Imaev
Over the half-century history of seismological studies in the Baikal region, more than 70 seismotectonic or inferred seismic dislocations related to displacements along active faults have been established. Some of them have been studied in detail by trenching and methods of absolute and relative timing. The current work discusses the age of paleoearthquakes in the Baikal region and gives an overvi...... hiện toàn bộ
Neotectonics and the Upper Mantle Structure of Central AsiaGeotectonics - Tập 55 - Trang 334-360 - 2021
V. G. Trifonov, S. Yu. Sokolov, D. M. Bachmanov, S. A. Sokolov, Ya. I. Trikhunkov
Studies carried out by the authors show that the uplift of Central Asia situated between the eastern Alpine–Himalayan and western Altai–Stanovoy orogenic belts formed in the neotectonic epoch. Major elements of the neotectonic structure and compiled upper mantle sections showing the difference in P-wave velocities from the standard values for the corresponding depths are analyzed. It is found that...... hiện toàn bộ
Morpho-Structural Study of the Korek Anticline, Zagros Fold-Thrust Belt, Kurdistan of IraqGeotectonics - Tập 52 - Trang 382-400 - 2019
A. A. Omar, A. T. Othman
The present study is an attempt to construct a morpho-structural model for the Korek anticline that is located within the High folded zone of the Zagros Fold and Thrust Belt in the Northern Iraq-Kurdistan region. A detail geological map constructed for this structure, the stratigraphic succession that is exposed in the area was deposited from the middle Jurassic up to upper Cretaceous, and consist...... hiện toàn bộ