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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/3RPNLJH
Repositorysid.inpe.br/mtc-m21c/2018/09.06.15.34   (restricted access)
Last Update2018:09.06.15.34.19 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2018/09.06.15.34.19
Metadata Last Update2019:01.14.17.06.34 (UTC) administrator
DOI10.1029/2017GC007314
ISSN1525-2027
Citation KeyMauryaMeFoPaLaMi:2018:DeReSt
TitleDeep Resistivity Structure of Basalt-Covered Central Part of Paraná Basin, Brazil, From Joint 3-D MT and GDS Data Imaging
Year2018
MonthJuly
Access Date2024, May 22
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size3171 KiB
2. Context
Author1 Maurya, Ved P.
2 Meju, Maxwell A.
3 Fontes, Sergio L.
4 Padilha, Antônio Lopes
5 La Terra, Emanuele F.
6 Miquelutti, Leonardo G.
Resume Identifier1
2
3
4 8JMKD3MGP5W/3C9JGJG
ORCID1 0000-0002-3626-5399
2 0000-0002-0485-0198
3 0000-0002-5765-5409
4
5 0000-0002-8606-2311
6 0000-0002-1665-5525
Group1
2
3
4 DIDGE-CGCEA-INPE-MCTIC-GOV-BR
Affiliation1 Observatório Nacional
2 Petronas Upstream Exploration, Kuala Lumpu
3 Observatório Nacional
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Observatório Nacional
6 Observatório Nacional
Author e-Mail Address1
2 maxwell_meju@petronas.com
3
4 antonio.padilha@inpe.br
JournalGeochemistry, Geophysics, Geosystems
Volume19
Number7
Pages1994-2013
Secondary MarkA1_GEOCIÊNCIAS
History (UTC)2018-09-06 15:35:03 :: simone -> administrator :: 2018
2019-01-04 16:57:10 :: administrator -> simone :: 2018
2019-01-07 12:36:54 :: simone -> administrator :: 2018
2019-01-14 17:06:34 :: administrator -> simone :: 2018
3. Content and structure
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Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractThe deep structure beneath the basalt-covered sediments of Paraná basin is not well understood. Magnetotelluric (MT) broadband (1,000 to 0.001 Hz) data recorded at 296 selected stations along three new survey lines were first inverted in three dimensions to reveal the local scale resistivity structure of the central part of the basin where there are three deep exploration wells with resistivity logs for model validation. The 3-D MT inversion model correctly identified the resistive (>100 Ωm) flood basalts and postvolcanic cover layer, the underlying electrically conductive (~10 Ωm) sediments, and the highly resistive (>1,000 Ωm) crystalline basement at the well locations and provides a reliable average crustal resistivity structure consisting of ~2024 km thick highly resistive upper crust and ~20 km thick conductive lower crust above a resistive mantle. Subsequent basin-scale joint inversion of highest quality MT data sets (261 stations) and geomagnetic depth sounding array data imaged two prominent subparallel belts of N-S and NNE-SSW trending steep conductors in the deep crust and upper mantle, one located directly beneath the present-day axis of thickest sedimentary deposits in the basin and another near the coastal location where dolerite dyke swarms intrude the outcropping Precambrian basement. Other roughly orthogonal bands (E-W to NW-SE) of linear crustal conductors radiate from these two main belts. The resulting networks of steep conductors at upper to midcrustal level seem to mark the fossil plumbing system of Paraná magmatic province and are interpreted as preexisting shear zones exploited by the voluminous Early Cretaceous magmatism in the region.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDGE > Deep Resistivity Structure...
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4. Conditions of access and use
Languageen
Target Filemaurya_deep.pdf
User Groupsimone
Reader Groupadministrator
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Visibilityshown
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EU29DP
Citing Item Listsid.inpe.br/bibdigital/2013/10.01.22.11 2
sid.inpe.br/mtc-m21/2012/07.13.14.40.26 2
DisseminationWEBSCI
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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