{"title":"震源与区域参数反演策略","authors":"Z. Tao, A. Cui, Xiwei Wang, X. Tao","doi":"10.1109/ICNC.2012.6234628","DOIUrl":null,"url":null,"abstract":"To obtain source and regional parameters, which are adopted to describe the earthquake source and crustal medium in a region to estimate ground motion, an inversion strategy is presented in this paper. Since these parameters are inversed from seismographic records by micro-genetic algorithm to establish strong ground motion attenuation relations, it is important to choose parameters not related with the sizes of earthquakes. One source parameter, stress drop Δσ, and four regional ones, Q0, η, R1 and R2, are selected as the inversed parameters.","PeriodicalId":404981,"journal":{"name":"2012 8th International Conference on Natural Computation","volume":"298 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2012-05-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Inversion strategy for seismic source and regional parameters\",\"authors\":\"Z. Tao, A. Cui, Xiwei Wang, X. Tao\",\"doi\":\"10.1109/ICNC.2012.6234628\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"To obtain source and regional parameters, which are adopted to describe the earthquake source and crustal medium in a region to estimate ground motion, an inversion strategy is presented in this paper. Since these parameters are inversed from seismographic records by micro-genetic algorithm to establish strong ground motion attenuation relations, it is important to choose parameters not related with the sizes of earthquakes. One source parameter, stress drop Δσ, and four regional ones, Q0, η, R1 and R2, are selected as the inversed parameters.\",\"PeriodicalId\":404981,\"journal\":{\"name\":\"2012 8th International Conference on Natural Computation\",\"volume\":\"298 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2012-05-29\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"2012 8th International Conference on Natural Computation\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/ICNC.2012.6234628\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"2012 8th International Conference on Natural Computation","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ICNC.2012.6234628","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Inversion strategy for seismic source and regional parameters
To obtain source and regional parameters, which are adopted to describe the earthquake source and crustal medium in a region to estimate ground motion, an inversion strategy is presented in this paper. Since these parameters are inversed from seismographic records by micro-genetic algorithm to establish strong ground motion attenuation relations, it is important to choose parameters not related with the sizes of earthquakes. One source parameter, stress drop Δσ, and four regional ones, Q0, η, R1 and R2, are selected as the inversed parameters.