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1. Identity statement
Reference TypeJournal Article
Sitemarte3.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZ3r59YCT/GUiPe
Repositorysid.inpe.br/iris@1905/2005/07.29.02.28   (restricted access)
Last Update2013:02.06.16.34.01 (UTC) administrator
Metadata Repositorysid.inpe.br/iris@1905/2005/07.29.02.28.32
Metadata Last Update2018:06.06.04.14.30 (UTC) administrator
Secondary KeyINPE-5847-PRE/1991
ISSN0236-5758
Label7235
Citation KeyPadilhaCostTriv:1992:UpCrHi
TitleUpper crustal high conductivity layer in the intraplate seismic province of NE-Brazil revealed by magnetotellurics
Year1992
Secondary Date19960402
Access Date2024, May 02
Secondary TypePRE PI
Number of Files1
Size2454 KiB
2. Context
Author1 Padilha, Antonio Lopes
2 Costa, I. V. J. M. da
3 Trivedi, Nalin Babulal
Group1 DGE-INPE-MCT-BR
2 DGE-INPE-MCT-BR
3 DGE-INPE-MCT-BR
JournalActa Geodaetica, Geophysica et Montanistica Hungarica
Volume27
Number1
Pages111-119
History (UTC)2008-06-09 16:17:45 :: administrator -> jefferson ::
2010-05-11 15:05:09 :: jefferson -> administrator ::
2012-11-21 14:10:43 :: administrator -> jefferson :: 1992
2013-02-06 17:32:27 :: jefferson -> banon :: 1992
2013-02-18 18:47:53 :: banon -> administrator :: 1992
2018-06-06 04:14:30 :: administrator -> marciana :: 1992
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsGEOFISICA ESPACIAL
AbstractA magnetotelluric survey consisting of fifteen high-frequency AMT and six low frequency MT soundings was carried out in the intraplate seismic province of northeast Brazil. A NW-SE profile with nine AMT and four MT stations was positioned to cross the seismic zone of Joao Camara (5.5 degrees S, 35.7 degrees W) which is the easternmost swarm of the NE province. Two conductive layers were derived from 2D modelling of the TM-mode of electromagnetic wave propagation: 1. a shallower one (depth of 10 km) in the NW-end of the profile with conductance of 60 S, and 2, a deeper one (at 30 km) in the SE-end. Preliminary interpretation of these results suggests that the crustal conductivity structure of the region could be controlled by unexpected temperature differences between conterminous crustal blocks. In the western block are concentrated the principal upper crust geophysical and geological inhomogeneities and the most important recent shallow-depth seismic activity. The 10 km deep conductive layer in this block could be possible associated with a ductile layer which limits the maximum depht of the earthquakes.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDGE > Upper crustal high...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target Filepadilha92b.pdf
User Groupadministrator
banon
jefferson
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher allowfinaldraft
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EU29DP
DisseminationCOMPENDEX
Host Collectionsid.inpe.br/banon/2001/04.03.15.36
6. Notes
NotesGeneral Assembly IUGG, 20
IAGA, 91, Aug., 1991, Viena, AU.
Empty Fieldsaffiliation alternatejournal archivist callnumber copyright creatorhistory descriptionlevel doi e-mailaddress electronicmailaddress format isbn lineage mark mirrorrepository month nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Description control
e-Mail (login)marciana
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