H. Sargsyan, G. Abgaryan, E. Mughnetsyan, A. Gevorgyan
{"title":"亚美尼亚","authors":"H. Sargsyan, G. Abgaryan, E. Mughnetsyan, A. Gevorgyan","doi":"10.18356/7025206b-en","DOIUrl":null,"url":null,"abstract":"The analysis of the earthquakes on the territory of Armenia and adjacent regions is presented. The highest level of seismic activity in the Republic is registered in the Northern part of the territory, within the source zones of the Spitak (1988), Van (2011) and two Akharin (2012) earthquakes. The significant earthquakes felt on the territory of Armenia are described.","PeriodicalId":118110,"journal":{"name":"Rome and the Near Eastern Kingdoms and Principalities, 44-31 BC","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2002-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Armenia\",\"authors\":\"H. Sargsyan, G. Abgaryan, E. Mughnetsyan, A. Gevorgyan\",\"doi\":\"10.18356/7025206b-en\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The analysis of the earthquakes on the territory of Armenia and adjacent regions is presented. The highest level of seismic activity in the Republic is registered in the Northern part of the territory, within the source zones of the Spitak (1988), Van (2011) and two Akharin (2012) earthquakes. The significant earthquakes felt on the territory of Armenia are described.\",\"PeriodicalId\":118110,\"journal\":{\"name\":\"Rome and the Near Eastern Kingdoms and Principalities, 44-31 BC\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2002-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Rome and the Near Eastern Kingdoms and Principalities, 44-31 BC\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.18356/7025206b-en\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Rome and the Near Eastern Kingdoms and Principalities, 44-31 BC","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18356/7025206b-en","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The analysis of the earthquakes on the territory of Armenia and adjacent regions is presented. The highest level of seismic activity in the Republic is registered in the Northern part of the territory, within the source zones of the Spitak (1988), Van (2011) and two Akharin (2012) earthquakes. The significant earthquakes felt on the territory of Armenia are described.
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