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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Main Authors: Баяраа Г, А В Ключевский, Дэмбэрэл С
Format: Article
Language:English
Published: Mongolian Academy of Sciences 2017-06-01
Series:Proceedings of the Mongolian Academy of Sciences
Online Access:https://www.mongoliajol.info/index.php/PMAS/article/view/796
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spelling 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
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