Forecasting of possible seismogenic zones in the Dnieper-Donetsk paleorift
As a result of complex geologic-geophysical investigations data analysis in the territory of the Dnieper-Donets paleorift (DDP) along DSS-profiles stretched across this structure, four possible seismogenic zones were distinguished. By preliminary data the junction region of DDP with the Ukrainian Sh...
Збережено в:
Видавець: | Subbotin Institute of Geophysics of the NAS of Ukraine |
---|---|
Дата: | 2012 |
Автори: | , , |
Формат: | Стаття |
Мова: | rus |
Опубліковано: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2012
|
Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/116590 |
Теги: |
Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|
Репозиторії
Geofizicheskiy Zhurnalid |
journalsuranua-geofizicheskiy-article-116590 |
---|---|
record_format |
ojs |
spelling |
journalsuranua-geofizicheskiy-article-1165902020-10-07T12:02:45Z Forecasting of possible seismogenic zones in the Dnieper-Donetsk paleorift Trypol'skii, A. A. Kalyuzhnaya, A. T. Tripolskaya, E. A. As a result of complex geologic-geophysical investigations data analysis in the territory of the Dnieper-Donets paleorift (DDP) along DSS-profiles stretched across this structure, four possible seismogenic zones were distinguished. By preliminary data the junction region of DDP with the Ukrainian Shield and the Voronezh massif, the central part of paleorift (DSS-profile Piryatin - Talalaevka) and the junction region of DDP with folded Donbass are the most seismically active. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116590 10.24028/gzh.0203-3100.v34i1.2012.116590 Geofizicheskiy Zhurnal; Vol. 34 No. 1 (2012); 95-104 Геофизический журнал; Том 34 № 1 (2012); 95-104 Геофізичний журнал; Том 34 № 1 (2012); 95-104 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116590/110616 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
institution |
Geofizicheskiy Zhurnal |
collection |
OJS |
language |
rus |
format |
Article |
author |
Trypol'skii, A. A. Kalyuzhnaya, A. T. Tripolskaya, E. A. |
spellingShingle |
Trypol'skii, A. A. Kalyuzhnaya, A. T. Tripolskaya, E. A. Forecasting of possible seismogenic zones in the Dnieper-Donetsk paleorift |
author_facet |
Trypol'skii, A. A. Kalyuzhnaya, A. T. Tripolskaya, E. A. |
author_sort |
Trypol'skii, A. A. |
title |
Forecasting of possible seismogenic zones in the Dnieper-Donetsk paleorift |
title_short |
Forecasting of possible seismogenic zones in the Dnieper-Donetsk paleorift |
title_full |
Forecasting of possible seismogenic zones in the Dnieper-Donetsk paleorift |
title_fullStr |
Forecasting of possible seismogenic zones in the Dnieper-Donetsk paleorift |
title_full_unstemmed |
Forecasting of possible seismogenic zones in the Dnieper-Donetsk paleorift |
title_sort |
forecasting of possible seismogenic zones in the dnieper-donetsk paleorift |
description |
As a result of complex geologic-geophysical investigations data analysis in the territory of the Dnieper-Donets paleorift (DDP) along DSS-profiles stretched across this structure, four possible seismogenic zones were distinguished. By preliminary data the junction region of DDP with the Ukrainian Shield and the Voronezh massif, the central part of paleorift (DSS-profile Piryatin - Talalaevka) and the junction region of DDP with folded Donbass are the most seismically active. |
publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
publishDate |
2012 |
url |
https://journals.uran.ua/geofizicheskiy/article/view/116590 |
work_keys_str_mv |
AT trypolskiiaa forecastingofpossibleseismogeniczonesinthednieperdonetskpaleorift AT kalyuzhnayaat forecastingofpossibleseismogeniczonesinthednieperdonetskpaleorift AT tripolskayaea forecastingofpossibleseismogeniczonesinthednieperdonetskpaleorift |
first_indexed |
2024-04-21T19:40:56Z |
last_indexed |
2024-04-21T19:40:56Z |
_version_ |
1796974530343731200 |