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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP5W34M/3GD3H4P
Repositorysid.inpe.br/mtc-m21b/2014/05.30.02.28.51   (restricted access)
Last Update2014:07.28.17.53.45 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2014/05.30.02.28.52
Metadata Last Update2018:06.04.03.04.17 (UTC) administrator
DOI10.1016/j.tecto.2013.12.021
ISSN0040-1951
Labelisi 2014-05 BezerraROMBBNDAG:2014:NeReSh
Citation KeyBezerraROMBBNDAG:2014:NeReSh
TitleNeotectonic reactivation of shear zones and implications for faulting style and geometry in the continental margin of NE Brazil
ProjectBrazilian National Research Council (CNPq) INCTET Project no. 573713/2008-1, CNPq Project no. 471950/2012-2, and FAPESP Projects 2006/04687-7 and 2012/06010-5.
Year2014
MonthFeb.
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size4717 KiB
2. Context
Author 1 Bezerra, F. H. R.
 2 Rossetti, Dilce de Fátima
 3 Oliveira, R. G.
 4 Medeiros, W. E.
 5 Brito Neves, B. B.
 6 Balsamo, F.
 7 Nogueira, F. C. C.
 8 Dantas, E. L.
 9 Andrades Filho, C.
10 Goes, A. M.
Resume Identifier 1
 2 8JMKD3MGP5W/3C9JGTQ
Group 1
 2 DSR-OBT-INPE-MCTI-GOV-BR
Affiliation 1 Univ Fed Rio Grande do Norte, BR-59072970 Natal, RN, Brazil.; CNPq, INCT ET, Inst Nacl Ciencia & Tecnol Estudos Tecton, Brasilia, DF, Brazil.
 2 Instituto Nacional de Pesquisas Espaciais (INPE)
 3 Serv Geol Brasil CPRM, Rio De Janeiro, Brazil.
 4 Univ Fed Rio Grande do Norte, BR-59072970 Natal, RN, Brazil.; Inst Nacl Ciencia & Tecnol Geofis Petr CNPq, INCT GP, Brasilia, DF, Brazil.
 5 Univ Sao Paulo, Inst Geociencias, BR-05508 Sao Paulo, Brazil.
 6 Univ Parma, I-43100 Parma, Italy.
 7 CNPq, INCT ET, Inst Nacl Ciencia & Tecnol Estudos Tecton, Brasilia, DF, Brazil.; Univ Fed Campina Grande, Campina Grande, Paraiba, Brazil.
 8 CNPq, INCT ET, Inst Nacl Ciencia & Tecnol Estudos Tecton, Brasilia, DF, Brazil.; Univ Brasilia, BR-70910900 Brasilia, DF, Brazil.
 9 Univ Estadual Rio Grande do Sul, Porto Alegre, RS, Brazil.
10 Univ Sao Paulo, Inst Geociencias, BR-05508 Sao Paulo, Brazil.
Author e-Mail Address 1 bezerrafh@geologia.ufrn.br
 2 rossetti@dsr.inpe.br
e-Mail Addressmarcelo.pazos@inpe.br
JournalTectonophysics
Volume614
Pages78-90
Secondary MarkA1_ENGENHARIAS_III A1_GEOGRAFIA A2_GEOCIÊNCIAS A2_ENGENHARIAS_II
History (UTC)2018-06-04 03:04:17 :: administrator -> marcelo.pazos@inpe.br :: 2014
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordscontinental margin
neotectonics
fault reactivation
post-rift sediments
AbstractThe eastern continental margin of South America comprises a series of rift basins developed during the breakup of Pangea in the Jurassic-Cretaceous. We integrated high resolution aeromagnetic, structural and stratigraphic data in order to evaluate the role of reactivation of ductile, Neoproterozoic shear zones in the deposition and deformation of post-rift sedimentary deposits in one of these basins, the Paraiba Basin in northeastern Brazil. This basin corresponds to the last part of the South American continent to be separated from Africa during the Pangea breakup. Sediment deposition in this basin occurred in the Albian-Maastrichtian, Eocene-Miocene, and in the late Quaternary. However, our investigation concentrates on the Miocene-Quaternary, which we consider the neotectonic period because it encompasses the last stress field. This consisted of an E-W-oriented compression and a N-S-oriented extension. The basement of the basin forms a slightly seaward-tilted ramp capped by a late Cretaceous to Quaternary sedimentary cover similar to 100-400 m thick. Aeromagnetic lineaments mark the major steeply-dipping, ductile E-W- to NE-striking shear zones in this basement. The ductile shear zones mainly reactivated as strike-slip, normal and oblique-slip faults, resulting in a series of Miocene-Quaternary depocenters controlled by NE-, E-W-, and a few NW-striking faults. Faulting produced subsidence and uplift that are largely responsible for the present-day morphology of the valleys and tablelands in this margin. We conclude that Precambrian shear zone reactivation controlled geometry and orientation, as well as deformation of sedimentary deposits, until the Neogene-Quaternary. (C) 2014 Elsevier B.V. All rights reserved.
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Languageen
Target File1-s2.0-S0040195114000055-main.pdf
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5. Allied materials
Mirror Repositoryiconet.com.br/banon/2006/11.26.21.31
Next Higher Units8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
URL (untrusted data)http://dx.doi.org/10.1016/j.tecto.2013.12.021
DisseminationWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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