сотрудник
НИТУ МИСиС (Горный институт, старший преподаватель)
сотрудник
г. Москва и Московская область, Россия
сотрудник
сотрудник
сотрудник
Институт физики Земли им. О.Ю. Шмидта (лаборатория геоинформатики, младший научный сотрудник)
сотрудник
сотрудник
сотрудник
Институт физики Земли им. О.Ю. Шмидта (лаборатория геоинформатики, ведущий научный сотрудник)
докторант
ВАК 1.6.20 Геоинформатика, картография
ВАК 1.6.21 Геоэкология
ВАК 1.6 Науки о Земле и окружающей среде
УДК 551.242 Тектонические движения, колебания и т. п. Тектонические структуры земной коры и их элементы
УДК 550.34.016 Экспериментальные исследования: измерения, опыты, полевые эксперименты
УДК 55 Геология. Геологические и геофизические науки
УДК 550.34 Сейсмология
УДК 550.383 Главное магнитное поле Земли
ГРНТИ 37.31 Физика Земли
ГРНТИ 37.01 Общие вопросы геофизики
ГРНТИ 37.15 Геомагнетизм и высокие слои атмосферы
ГРНТИ 37.25 Океанология
ГРНТИ 38.01 Общие вопросы геологии
ГРНТИ 36.00 ГЕОДЕЗИЯ. КАРТОГРАФИЯ
ГРНТИ 37.00 ГЕОФИЗИКА
ГРНТИ 38.00 ГЕОЛОГИЯ
ГРНТИ 39.00 ГЕОГРАФИЯ
ГРНТИ 52.00 ГОРНОЕ ДЕЛО
ОКСО 05.06.01 Науки о Земле
ББК 26 Науки о Земле
ТБК 63 Науки о Земле. Экология
BISAC SCI SCIENCE
There are numerous methods for modeling velocity fields of the Earth’s crust. However, only a few of them are capable of modeling data beyond the contour of the geodetic network (extrapolating). Spatial modeling based on a neural network approach allows for the adequate modeling of the field of recent crustal movements and deformations of the Earth’s crust beyond the geodetic network contour. The study extensively examines the hyperparameter settings and justifies the applicability of the neural network model for predicting crustal movement fields using the Ossetian geodynamic polygon as an example. The presented results, when compared to classical modeling methods, demonstrate that the neural network approach confidently yields results no worse than classical methods. The results of modeling for the Ossetian polygon can be used for geodynamic zoning, identification zones of extension and compression, computing the tectonic component of stresses, and identifying areas of high-gradient displacements.
velocity fields, resent crustal movements, spatial modeling, regular grid, extrapolation, interpolation, artificial neural networks
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