1. Identity statement | |
Reference Type | Journal Article |
Site | mtc-m21b.sid.inpe.br |
Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identifier | 8JMKD3MGP3W34P/3KBEF7H |
Repository | sid.inpe.br/mtc-m21b/2015/09.30.12.25 |
Last Update | 2016:01.05.18.22.39 (UTC) administrator |
Metadata Repository | sid.inpe.br/mtc-m21b/2015/09.30.12.25.57 |
Metadata Last Update | 2022:03.18.22.11.46 (UTC) administrator |
DOI | 10.1002/2014JB011657 |
ISSN | 0148-0227 2156-2202 |
Citation Key | PadilhaVitoAntuPádu:2015:ImThCr |
Title | Imaging three-dimensional crustal conductivity structures reflecting continental flood basalt effects hidden beneath thick intracratonic sedimentary basin |
Year | 2015 |
Month | July |
Access Date | 2024, May 22 |
Type of Work | journal article |
Secondary Type | PRE PI |
Number of Files | 1 |
Size | 5630 KiB |
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2. Context | |
Author | 1 Padilha, Antonio Lopes 2 Vitorello, Ícaro 3 Antunes, Cássio Espíndola 4 Pádua, Marcelo Banik de |
Resume Identifier | 1 8JMKD3MGP5W/3C9JGJG 2 8JMKD3MGP5W/3C9JHD6 3 4 8JMKD3MGP5W/3C9JHNR |
Group | 1 DGE-CEA-INPE-MCTI-GOV-BR 2 DGE-CEA-INPE-MCTI-GOV-BR 3 GESAST-CEA-SPG-INPE-MCTI-GOV-BR 4 DGE-CEA-INPE-MCTI-GOV-BR |
Affiliation | 1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Instituto Nacional de Pesquisas Espaciais (INPE) 4 Instituto Nacional de Pesquisas Espaciais (INPE) |
Author e-Mail Address | 1 antonio.padilha@inpe.br 2 icaro.vitorello@inpe.br 3 cassio.antunes@inpe.br 4 marcelo.banik@inpe.br |
Journal | Journal of Geophysical Research |
Volume | 120 |
Number | 7 |
Pages | 4702-4719 |
Secondary Mark | A1_INTERDISCIPLINAR A1_GEOGRAFIA A1_GEOCIÊNCIAS A1_ENGENHARIAS_III A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_QUÍMICA A2_ENGENHARIAS_IV A2_ENGENHARIAS_II A2_ENGENHARIAS_I A2_BIODIVERSIDADE B1_MATERIAIS B1_MATEMÁTICA_/_PROBABILIDADE_E_ESTATÍSTICA B1_CIÊNCIAS_BIOLÓGICAS_I B1_CIÊNCIA_DA_COMPUTAÇÃO B1_ASTRONOMIA_/_FÍSICA B2_PLANEJAMENTO_URBANO_E_REGIONAL_/_DEMOGRAFIA |
History (UTC) | 2015-09-30 12:25:57 :: simone -> administrator :: 2022-03-18 22:11:46 :: administrator -> simone :: 2015 |
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3. Content and structure | |
Is the master or a copy? | is the master |
Content Stage | completed |
Transferable | 1 |
Content Type | External Contribution |
Version Type | publisher |
Keywords | continental flood basalts electromagnetic induction large igneous provinces Paraná Basin three-dimensional conductivity structure |
Abstract | A large-scale array of long-period magnetic data and a deep-probing magnetotelluric profile were recorded in the intracratonic Paraná sedimentary basin in central eastern South America, which presents a thick and extensive sedimentary-magmatic sequence that allows its basement to be investigated only by indirect methods. Integration of the results from both methods showed that the crust beneath the basin presents several quasi-linear highly conductive channeled zones with limited lateral extent, in coincidence with some of the main tectonic structures recognized at the surface, and a moderate but pervasive lithosphere conductivity enhancement beneath its central part. Upward movement of CO2-bearing volatiles and magmas precipitating highly conducting mineral phases along discrete subvertical fault zones that served as feeder conduits for Early Cretaceous voluminous continental flood basalts was a likely process responsible for the localized conductivity enhancements. Correlation between some of the linear conductive zones and elongated magnetic anomalies and between the maximum depth occurrence of most of these conductive anomalies and the Curie depth at which crustal rocks lose their magnetism gives strong support to interconnected iron oxides (especially magnetite) and iron sulfides (such as pyrrhotite) as the main conductive sources. The moderate bulk conductivity increase in the crust and upper mantle beneath the central part of the basin is unexpected for a postulated cratonic basement and is tentatively associated with impregnation of the lithosphere by conducting minerals related either to widespread tectonic events in the Ordovician or Late Precambrian or to dispersed magmatic residues of an Early Cretaceous magma differentiation contaminating the entire lithosphere. |
Area | CEA |
Arrangement 1 | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDGE > Imaging three-dimensional crustal... |
Arrangement 2 | urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > GES > Imaging three-dimensional crustal... |
doc Directory Content | access |
source Directory Content | there are no files |
agreement Directory Content | |
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4. Conditions of access and use | |
data URL | http://urlib.net/ibi/8JMKD3MGP3W34P/3KBEF7H |
zipped data URL | http://urlib.net/zip/8JMKD3MGP3W34P/3KBEF7H |
Language | en |
User Group | marciana simone |
Reader Group | administrator marciana simone |
Visibility | shown |
Archiving Policy | denypublisher6 allowfinaldraft |
Read Permission | allow from all |
Update Permission | not transferred |
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5. Allied materials | |
Mirror Repository | urlib.net/www/2011/03.29.20.55 |
Next Higher Units | 8JMKD3MGPCW/3EU29DP 8JMKD3MGPCW/3F2PBEE |
Citing Item List | sid.inpe.br/bibdigital/2013/10.12.21.02 2 sid.inpe.br/mtc-m21/2012/07.13.14.40.26 2 sid.inpe.br/bibdigital/2013/10.01.22.11 1 |
Dissemination | WEBSCI; AGU; COMPENDEX; SCOPUS. |
Host Collection | sid.inpe.br/mtc-m21b/2013/09.26.14.25.20 |
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6. Notes | |
Empty Fields | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject targetfile tertiarymark tertiarytype url |
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7. Description control | |
e-Mail (login) | simone |
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