SEISMOLOGICAL MONITORING OF THE DEFORMATION PROCESS

dc.contributor.authorBormotov V.A.
dc.contributor.authorBykov V.G.
dc.date.accessioned2021-02-14T10:37:02Z
dc.date.available2021-02-14T10:37:02Z
dc.date.issued2001
dc.description.abstractA technique for determining volume deformation variations is suggested and substantiated theoretically on the basis of the multiple-reflection longitudinal waves specified in the seismograms from distant earthquakes. Results of seismological monitoring carried out in the south of Priamurye testify to the qualitative and quantitative difference of the deformation process at different depth levels. Variations of volume deformation are estimated down to a depth of 50 km.
dc.identifierhttps://elibrary.ru/item.asp?id=13363854
dc.identifier.citationGeology of the Pacific Ocean, 2001, 16, 6, 981-994
dc.identifier.issn8755-755X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/24932
dc.titleSEISMOLOGICAL MONITORING OF THE DEFORMATION PROCESS
dc.typeСтатья

Файлы

Оригинальный пакет

Показано 1 - 1 из 1
Загрузка...
Изображение-миниатюра
Имя:
Borm_01.pdf
Размер:
371.81 KB
Формат:
Adobe Portable Document Format

Коллекции