{"title":"An Evaluation on the Behaviors of Aftershock Sequence of November 26th, 2019 Earthquake, ML=6.3, North of Durrës, Albania","authors":"S. Öztürk, R. Ormeni","doi":"10.18586/MSUFBD.899411","DOIUrl":null,"url":null,"abstract":"(Kabul): 03.05.2021 ABSTRACT A comprehensive assessment of aftershocks occurrence for the November 26 th , 2019 earthquake, M L =6.3, 16 km north of Durrës, Albania was achieved. b -value was estimated as 0.88 ±0.07. b -value is close to 1.0 and relatively small b -value may be resulted from the plenty of larger aftershocks with M L 4.0. p -value was calculated as 1.23±0.08 with Mmin =3.1 and Tstart =0.0034 days. This high p -value may be a result of the relative fast decay rate of aftershock activity. Dc -value was calculated as 1.74±0.09 and it means that aftershocks are homogeneously distributed at larger scales. The smallest b -values and the largest p -values were observed in the north, northwest and northeast parts of the mainshock. The smaller b -values correlate with the larger stress variations, whereas the larger p -values are related to the maximum slip after mainshock. Consequently, region-time-magnitude analyses of the aftershocks occurrence may supply important clues for the fast evaluations of real","PeriodicalId":437889,"journal":{"name":"Muş Alparslan Üniversitesi Fen Bilimleri Dergisi","volume":"21 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-05-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Muş Alparslan Üniversitesi Fen Bilimleri Dergisi","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18586/MSUFBD.899411","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
(Kabul): 03.05.2021 ABSTRACT A comprehensive assessment of aftershocks occurrence for the November 26 th , 2019 earthquake, M L =6.3, 16 km north of Durrës, Albania was achieved. b -value was estimated as 0.88 ±0.07. b -value is close to 1.0 and relatively small b -value may be resulted from the plenty of larger aftershocks with M L 4.0. p -value was calculated as 1.23±0.08 with Mmin =3.1 and Tstart =0.0034 days. This high p -value may be a result of the relative fast decay rate of aftershock activity. Dc -value was calculated as 1.74±0.09 and it means that aftershocks are homogeneously distributed at larger scales. The smallest b -values and the largest p -values were observed in the north, northwest and northeast parts of the mainshock. The smaller b -values correlate with the larger stress variations, whereas the larger p -values are related to the maximum slip after mainshock. Consequently, region-time-magnitude analyses of the aftershocks occurrence may supply important clues for the fast evaluations of real