А. Ovsyuchenko, А.Н. Овсюченко, R. Vakarchuk, Р Н Вакарчук, A. Korzhenkov, А.М. Корженков, A. S. Larkov, А.С. Ларьков, А. I. Sysolin, А. И. Сысолин, E. Rogozhin, Е. А. Рогожин, A. V. Marahanov, А.В. Мараханов
{"title":"Active faults of the Kerch’s Peninsula: new results","authors":"А. Ovsyuchenko, А.Н. Овсюченко, R. Vakarchuk, Р Н Вакарчук, A. Korzhenkov, А.М. Корженков, A. S. Larkov, А.С. Ларьков, А. I. Sysolin, А. И. Сысолин, E. Rogozhin, Е. А. Рогожин, A. V. Marahanov, А.В. Мараханов","doi":"10.31857/s0869-56524884408-412","DOIUrl":null,"url":null,"abstract":"In the paper there are results of a recent study of the active faults in the Kerch Peninsula. There was compiled a Map of Active Faults - sources of the strong earthquakes occurred in Late Holocene. The map is a regional seismotectonic model of strong earthquake sources - detailed basis for a spatial prognosis of the seismic hazard. Results of the study show that the Kerch Peninsula demonstrates signs of the classical morphostructures, and a morphology of the modern peninsula contours is caused by the large active fault zones.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":"64 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2019-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Доклады Академии наук","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31857/s0869-56524884408-412","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
In the paper there are results of a recent study of the active faults in the Kerch Peninsula. There was compiled a Map of Active Faults - sources of the strong earthquakes occurred in Late Holocene. The map is a regional seismotectonic model of strong earthquake sources - detailed basis for a spatial prognosis of the seismic hazard. Results of the study show that the Kerch Peninsula demonstrates signs of the classical morphostructures, and a morphology of the modern peninsula contours is caused by the large active fault zones.