8th International Congress of the Brazilian Geophysical Society 2003
DOI: 10.3997/2214-4609-pdb.168.arq_341
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Magnetômetro tipo Fluxgate para aplicações em Sondagens Geomagnéticas Profundas (GDS) no Brasil

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Cited by 5 publications
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“…A two‐dimensional conductivity‐depth model for the area between the two selected TLs is shown in Figure 3 [ Bologna et al , 2001]. The measurements of geomagnetic field variations under the two selected TLs were started in August 2004 by installing three‐component fluxgate magnetometers constructed at INPE [ Kabata et al , 2004; Trivedi et al , 1995]. The selected transmission lines Itumbiara–São Simão and Pimenta‐Barreiro, situated in the western region of the state of Minas Gerais, are about 700 and 300 km, respectively, from the magnetic observatory of Vassouras (Rio de Janeiro (RJ)), our reference station for GIC investigation.…”
Section: Selection Of the Site For Gic Measurementsmentioning
confidence: 99%
“…A two‐dimensional conductivity‐depth model for the area between the two selected TLs is shown in Figure 3 [ Bologna et al , 2001]. The measurements of geomagnetic field variations under the two selected TLs were started in August 2004 by installing three‐component fluxgate magnetometers constructed at INPE [ Kabata et al , 2004; Trivedi et al , 1995]. The selected transmission lines Itumbiara–São Simão and Pimenta‐Barreiro, situated in the western region of the state of Minas Gerais, are about 700 and 300 km, respectively, from the magnetic observatory of Vassouras (Rio de Janeiro (RJ)), our reference station for GIC investigation.…”
Section: Selection Of the Site For Gic Measurementsmentioning
confidence: 99%