{"title":"超宽带大地噪声产生机制:“电地震信号”(SES)的可能信号源","authors":"V. Pham, D. Boyer, F. Perrier, J. L. Mouël","doi":"10.1016/S1251-8050(01)01639-1","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":10613,"journal":{"name":"Comptes rendus hebdomadaires des seances de l'Academie des sciences","volume":"96 1","pages":"255-262"},"PeriodicalIF":0.0000,"publicationDate":"2001-09-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":"{\"title\":\"Mécanismes de génération de bruits telluriques dans la bande ultrabasse fréquence (UBF) : sources possibles des signaux dits «signaux électro-sismiques » (SES)\",\"authors\":\"V. Pham, D. Boyer, F. Perrier, J. L. Mouël\",\"doi\":\"10.1016/S1251-8050(01)01639-1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":10613,\"journal\":{\"name\":\"Comptes rendus hebdomadaires des seances de l'Academie des sciences\",\"volume\":\"96 1\",\"pages\":\"255-262\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2001-09-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"4\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Comptes rendus hebdomadaires des seances de l'Academie des sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1016/S1251-8050(01)01639-1\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Comptes rendus hebdomadaires des seances de l'Academie des sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1016/S1251-8050(01)01639-1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Mécanismes de génération de bruits telluriques dans la bande ultrabasse fréquence (UBF) : sources possibles des signaux dits «signaux électro-sismiques » (SES)