Монгол орны нутал дэвсгэрт бүртгэгдсэн газар хөдлөлтийн төвүүдийн нягтаршил
Map of earthquake epicenter density of Mongolia for the instrumental period (1964 - 2000) is presented. Seismic active zones are studied using information provided by the location of earthquake epicenters density. The results suggest that Mongolian territory could be divided into five seismic active...
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doaj-d31a44d83bc7475d9814994064d839d22020-11-24T22:19:45ZengMongolian Academy of SciencesProceedings of the Mongolian Academy of Sciences2310-47162312-29942017-06-015119631310.5564/pmas.v57i196.796759Монгол орны нутал дэвсгэрт бүртгэгдсэн газар хөдлөлтийн төвүүдийн нягтаршилБаяраа Г0А В Ключевский1Дэмбэрэл С2ШУА, Одон Орон, Геофизикийн Судалгааны Төв,Институттут Земной Коры СО РАНШУА, Одон Орон, Геофизикийн Судалгааны Төв,Map of earthquake epicenter density of Mongolia for the instrumental period (1964 - 2000) is presented. Seismic active zones are studied using information provided by the location of earthquake epicenters density. The results suggest that Mongolian territory could be divided into five seismic active and homogeneous sub- zones originated by the distribution of seismic active Cenozoic faults and epicenter density. Earthquake epicenter density and its spatial distribution are given a possibility to define and localize seismic active zones, current seismic pattern and its future dynamics of seismic activity in these zones. Most of earthquakes with the larger magnitude in the seismic active zones occurred in proximity to the statistically identified potential faults. Results of this study would be input parameters of seismic hazard assessment study of urban areas.https://www.mongoliajol.info/index.php/PMAS/article/view/796 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Баяраа Г А В Ключевский Дэмбэрэл С |
spellingShingle |
Баяраа Г А В Ключевский Дэмбэрэл С Монгол орны нутал дэвсгэрт бүртгэгдсэн газар хөдлөлтийн төвүүдийн нягтаршил Proceedings of the Mongolian Academy of Sciences |
author_facet |
Баяраа Г А В Ключевский Дэмбэрэл С |
author_sort |
Баяраа Г |
title |
Монгол орны нутал дэвсгэрт бүртгэгдсэн газар хөдлөлтийн төвүүдийн нягтаршил |
title_short |
Монгол орны нутал дэвсгэрт бүртгэгдсэн газар хөдлөлтийн төвүүдийн нягтаршил |
title_full |
Монгол орны нутал дэвсгэрт бүртгэгдсэн газар хөдлөлтийн төвүүдийн нягтаршил |
title_fullStr |
Монгол орны нутал дэвсгэрт бүртгэгдсэн газар хөдлөлтийн төвүүдийн нягтаршил |
title_full_unstemmed |
Монгол орны нутал дэвсгэрт бүртгэгдсэн газар хөдлөлтийн төвүүдийн нягтаршил |
title_sort |
монгол орны нутал дэвсгэрт бүртгэгдсэн газар хөдлөлтийн төвүүдийн нягтаршил |
publisher |
Mongolian Academy of Sciences |
series |
Proceedings of the Mongolian Academy of Sciences |
issn |
2310-4716 2312-2994 |
publishDate |
2017-06-01 |
description |
Map of earthquake epicenter density of Mongolia for the instrumental period (1964 - 2000) is presented. Seismic active zones are studied using information provided by the location of earthquake epicenters density. The results suggest that Mongolian territory could be divided into five seismic active and homogeneous sub- zones originated by the distribution of seismic active Cenozoic faults and epicenter density. Earthquake epicenter density and its spatial distribution are given a possibility to define and localize seismic active zones, current seismic pattern and its future dynamics of seismic activity in these zones. Most of earthquakes with the larger magnitude in the seismic active zones occurred in proximity to the statistically identified potential faults. Results of this study would be input parameters of seismic hazard assessment study of urban areas. |
url |
https://www.mongoliajol.info/index.php/PMAS/article/view/796 |
work_keys_str_mv |
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