Костюк А.Д. – мл. науч. сотрудник, Научная станция РАН, Бишкек
ДЕФОРМАЦИОННЫЕ ИЗМЕНЕНИЯ ЗЕМНОЙ КОРЫ СЕВЕРНОГО ТЯНЬ-ШАНЯ ПО ДАННЫМ КОСМИЧЕСКОЙ ГЕОДЕЗИИ
High density of Central Asia GPS network in the Northern Tien Shan and long period of observations have allowed to estimate a velocity vector field of movement crust and strain field. Results shows that strain rate axes have north-northwest directions; strain field is heterogeneous and have high compression zones.
Түйүндүү сөздөр орус тилинде:High density of Central Asia GPS network in the Northern Tien Shan and long period of observations have allowed to estimate a velocity vector field of movement crust and strain field. Results shows that strain rate axes have north-northwest directions; strain field is heterogeneous and have high compression zones.
ДЕФОРМАЦИОННЫЕ ИЗМЕНЕНИЯ ЗЕМНОЙ КОРЫ СЕВЕРНОГО ТЯНЬ-ШАНЯ ПО ДАННЫМ КОСМИЧЕСКОЙ ГЕОДЕЗИИ
High density of Central Asia GPS network in the Northern Tien Shan and long period of observations have allowed to estimate a velocity vector field of movement crust and strain field. Results shows that strain rate axes have north-northwest directions; strain field is heterogeneous and have high compression zones.
Түйүндүү сөздөр кыргыз тилинде:High density of Central Asia GPS network in the Northern Tien Shan and long period of observations have allowed to estimate a velocity vector field of movement crust and strain field. Results shows that strain rate axes have north-northwest directions; strain field is heterogeneous and have high compression zones.
ДЕФОРМАЦИОННЫЕ ИЗМЕНЕНИЯ ЗЕМНОЙ КОРЫ СЕВЕРНОГО ТЯНЬ-ШАНЯ ПО ДАННЫМ КОСМИЧЕСКОЙ ГЕОДЕЗИИ
High density of Central Asia GPS network in the Northern Tien Shan and long period of observations have allowed to estimate a velocity vector field of movement crust and strain field. Results shows that strain rate axes have north-northwest directions; strain field is heterogeneous and have high compression zones.
Түйүндүү сөздөр англис тилинде:High density of Central Asia GPS network in the Northern Tien Shan and long period of observations have allowed to estimate a velocity vector field of movement crust and strain field. Results shows that strain rate axes have north-northwest directions; strain field is heterogeneous and have high compression zones.