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@Article{KlausnerAlMeKhPiMuFa:2017:FiReSe,
               author = "Klausner, V. and Almeida, T. and Meneses J{\'u}nior, Francisco 
                         Carlos de and Kherani, Esfhan Alam and Pillat, V. G. and Muella, 
                         Marcio Tadeu A. H. and Fagundes, P. R.",
          affiliation = "{Universidade do Vale do Para{\'{\i}}ba (UNIVAP)} and 
                         {Universidade do Vale do Para{\'{\i}}ba (UNIVAP)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de 
                         Pesquisas Espaciais (INPE)} and {Universidade do Vale do 
                         Para{\'{\i}}ba (UNIVAP)} and {Universidade do Vale do 
                         Para{\'{\i}}ba (UNIVAP)} and {Universidade do Vale do 
                         Para{\'{\i}}ba (UNIVAP)}",
                title = "First report on seismogenic magnetic disturbances over brazilian 
                         sector",
              journal = "Pure and Applied Geophysics",
                 year = "2017",
               volume = "174",
               number = "3",
                pages = "737--745",
                month = "Mar.",
             keywords = "Brazil, H-component, Illapel earthquake 2015, LAI coupling, 
                         seismogenic magnetic disturbances.",
             abstract = "In this work, we present a first report on magnetic disturbances 
                         over the Brazilian sector that occurred on September 1617, 2015. 
                         These disturbances are associated with the Illapel earthquake. 
                         Using seven magnetometers installed across Brazil, and distributed 
                         within 4500 km from the epicenter, the presence of magnetic 
                         disturbances is noted ~15 min after the time of earthquake. The 
                         seismometers registered the arrival of the first seismic waves ~10 
                         min prior to the observed signatures on magnetic disturbances, 
                         suggesting that such waves are possibly from seismogenic origin, 
                         which involves the lithosphereatmosphereionosphere coupling.",
                  doi = "10.1007/s00024-016-1455-0",
                  url = "http://dx.doi.org/10.1007/s00024-016-1455-0",
                 issn = "0033-4553",
             language = "en",
           targetfile = "klausner_first.pdf",
        urlaccessdate = "28 nov. 2020"
}


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