{"title":"地震起爆中的非线性特征值问题","authors":"I. Ionescu, Vicentiu D. Rădulescu","doi":"10.57262/ade/1355926811","DOIUrl":null,"url":null,"abstract":"We study a symmetric, nonlinear eigenvalue problem arising in earthquake initiation, and we establish the existence of inflnitely many solutions. Under the efiect of an arbitrary perturbation, we prove that the number of solutions becomes greater and greater if the perturbation tends to zero with respect to a prescribed topology. Our approach is based on nonsmooth critical-point theories in the sense of De Giorgi and Degiovanni.","PeriodicalId":353809,"journal":{"name":"GeologyRN: Computational Methods in Geology (Topic)","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2003-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"8","resultStr":"{\"title\":\"Nonlinear Eigenvalue Problems Arising in Earthquake Initiation\",\"authors\":\"I. Ionescu, Vicentiu D. Rădulescu\",\"doi\":\"10.57262/ade/1355926811\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"We study a symmetric, nonlinear eigenvalue problem arising in earthquake initiation, and we establish the existence of inflnitely many solutions. Under the efiect of an arbitrary perturbation, we prove that the number of solutions becomes greater and greater if the perturbation tends to zero with respect to a prescribed topology. Our approach is based on nonsmooth critical-point theories in the sense of De Giorgi and Degiovanni.\",\"PeriodicalId\":353809,\"journal\":{\"name\":\"GeologyRN: Computational Methods in Geology (Topic)\",\"volume\":\"1 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2003-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"8\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"GeologyRN: Computational Methods in Geology (Topic)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.57262/ade/1355926811\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"GeologyRN: Computational Methods in Geology (Topic)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.57262/ade/1355926811","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Nonlinear Eigenvalue Problems Arising in Earthquake Initiation
We study a symmetric, nonlinear eigenvalue problem arising in earthquake initiation, and we establish the existence of inflnitely many solutions. Under the efiect of an arbitrary perturbation, we prove that the number of solutions becomes greater and greater if the perturbation tends to zero with respect to a prescribed topology. Our approach is based on nonsmooth critical-point theories in the sense of De Giorgi and Degiovanni.