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1. Identity statement
Reference TypeJournal Article
Sitemarte3.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZ3r59YCT/GUdnh
Repositorysid.inpe.br/iris@1905/2005/07.28.22.11   (restricted access)
Last Update2011:01.20.16.01.00 (UTC) administrator
Metadata Repositorysid.inpe.br/iris@1905/2005/07.28.22.11.06
Metadata Last Update2018:06.06.04.02.42 (UTC) administrator
Secondary KeyINPE-5955-PRE/2093
ISSN0269-7491
Label6043
Citation KeyPadilha:1999:BeMaSo
TitleBehaviour of magnetotelluric source fields within the equatorial zone
Year1999
MonthMay
Access Date2024, Apr. 28
Secondary TypePRE PI
Number of Files1
Size745 KiB
2. Context
AuthorPadilha, Antonio Lopes
GroupDGE-INPE-MCT-BR
AffiliationInstituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Addresspadilha@dge.inpe.br
JournalEnvironmental Pollution
Volume51
Number10
Pages1119-1125
History (UTC)2008-06-09 16:40:53 :: administrator -> banon ::
2010-05-11 15:34:57 :: banon -> jefferson ::
2011-01-20 16:01:00 :: jefferson -> banon :: 1999
2012-09-27 18:10:43 :: banon -> administrator :: 1999
2018-06-06 04:02:42 :: administrator -> marciana :: 1999
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordsgeofísica espacial
Brasil
eletrojatos equatorial
pesquisa magnética (perfis magnetoteluricos)
Brazil
equatorial electrojet
magnetic surveys (magnetotelluric profiling)
AbstractIt is well known that equatorial electrojet (EEJ) currents can significantly affect the geomagnetic variations. However, in a recent study (Padilha et al, 1997) it was observed that magnetotelluric (MT) soundings carried out across the dip equator in the Brazilian equatorial zone were not affected significantly due to EEJ currents. By using new results from geomagnetic variation signals, measured simultaneously to the MT experiment at a chain of equatorial and mid-latitude stations, an attempt is made here to explain the MT results in terms of the behaviour of the primary inducing field during the survey. Most of the analysis is performed by considering a single frequency (0.885 mHz), representative of the MT frequency interval. It is observed that the amplitude of the geomagnetic variations appears horizontally homogeneous within the study area (from -3 degrees to +3 degrees of geomagnetic latitude), indicating that the primary field in the analysed frequency range may be considered sufficiently uniform in the horizontal direction thus satisfying the Tikhonov-Cagniard plane-wave criterion. The same geomagnetic data also show that, if any EEJ source effect exists, it would be restricted to the transition zone (between 3 degrees and 5 degrees, at both sides of the dip equator). Dmitriev-Berdichevsky's constraints calculated at two different frequencies and a modelling exercise using EEJ parameters derived from a magnetometer array were able to explain the MT observations and have shown that source effects would just appear in frequencies lower than 1 mHz (resistive regions) and 0.1 mHz (conductive regions). Considering the characteristics of propagation and amplification of geomagnetic variations at the equatorial zone it is concluded that EEJ currents could be used as a source for lithospheric MT studies in these regions.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDGE > Behaviour of magnetotelluric...
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4. Conditions of access and use
Languageen
Target Filepublicacao.pdf
User Groupadministrator
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jefferson
Visibilityshown
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5. Allied materials
Next Higher Units8JMKD3MGPCW/3EU29DP
DisseminationWEBSCI; PORTALCAPES.
Host Collectionsid.inpe.br/banon/2001/04.03.15.36
6. Notes
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