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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21d.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34T/499PHPP
Repositorysid.inpe.br/mtc-m21d/2023/06.13.13.38   (restricted access)
Last Update2023:06.13.13.38.12 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21d/2023/06.13.13.38.12
Metadata Last Update2024:01.02.17.16.43 (UTC) administrator
DOI10.1016/j.jsames.2023.104356
ISSN0895-9811
Citation KeyBezerraMVRTMCNFM:2023:AnMeTi
TitleReview of tectonic inversion of sedimentary basins in NE and N Brazil: Analysis of mechanisms, timing and effects on structures and relief
Year2023
MonthJune
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size48219 KiB
2. Context
Author 1 Bezerra, Francisco H.
 2 Marques, Fernando O.
 3 Vasconcelos, David L.
 4 Rossetti, Dilce de Fátima
 5 Tavares, Aline C.
 6 Maia, Rubson P.
 7 Castro, David L. de
 8 Nogueira, Francisco C. C.
 9 Fuck, Reinhardt A.
10 Medeiros, Walter E.
Resume Identifier 1
 2
 3
 4 8JMKD3MGP5W/3C9JGTQ
Group 1
 2
 3
 4 DIOTG-CGCT-INPE-MCTI-GOV-BR
Affiliation 1 Universidade Federal do Rio Grande do Norte (UFRN)
 2 Universidade de Lisboa
 3 Instituto Nacional de Ciência e Tecnologia em Estudos Tectônicos
 4 Instituto Nacional de Pesquisas Espaciais (INPE)
 5 Universidade Federal do Rio Grande do Norte (UFRN)
 6 Instituto Nacional de Ciência e Tecnologia em Estudos Tectônicos
 7 Universidade Federal do Rio Grande do Norte (UFRN)
 8 Instituto Nacional de Ciência e Tecnologia em Estudos Tectônicos
 9 Instituto Nacional de Ciência e Tecnologia em Estudos Tectônicos
10 Universidade Federal do Rio Grande do Norte (UFRN)
Author e-Mail Address 1 hilario.bezerra@ufrn.br
 2
 3
 4 rossettidilce@gmail.com
JournalJournal of South American Earth Sciences
Volume126
Pagese104356
Secondary MarkA1_INTERDISCIPLINAR A1_GEOGRAFIA A2_GEOCIÊNCIAS A2_ENGENHARIAS_III A2_CIÊNCIAS_AGRÁRIAS_I B1_ODONTOLOGIA B1_MEDICINA_II B1_CIÊNCIAS_AMBIENTAIS B1_BIODIVERSIDADE B1_ANTROPOLOGIA_/_ARQUEOLOGIA B2_QUÍMICA B2_MATERIAIS B2_CIÊNCIAS_BIOLÓGICAS_I B3_ASTRONOMIA_/_FÍSICA C_ENGENHARIAS_II
History (UTC)2023-06-13 13:38:12 :: simone -> administrator ::
2023-06-13 13:38:13 :: administrator -> simone :: 2023
2023-06-13 13:39:24 :: simone -> administrator :: 2023
2024-01-02 17:16:43 :: administrator -> simone :: 2023
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsBasin inversion
Stress field
Fault reactivation
Uplift
Strike-slip stress regime
AbstractMost intraplate areas worldwide are under compression characterized by thrust and strike-slip deformations. The sources of the stresses in these regions are a combination of far-field (regional) stresses (e.g., ridge push, slab pull, lithospheric drag) and near-field (local) stresses (e.g., topography, lateral and vertical anisotropy of strength or elastic properties, erosion, flexural bending, overloading, buoyancy of low-density regions). These intraplate regions are sites favorable for the tectonic inversion of sedimentary basins. Here, we review the tectonic inversions of the sedimentary basins in NE and N Brazil, which comprise a significant part of the South American intraplate (the South American Platform). These regions have been under compression since the Late Cretaceous. Reports of post-rift basin inversions derived from seismic profiles, fault-slip data, and topography have been described in the Sergipe-Alagoas, Paraiba, Potiguar, Cear ' a, Rio do Peixe, Araripe (NE Brazil), and Solimo similar to es (N Brazil) basins. Reports of inversions in the rift phase have also been described in the Araripe Basin. The presentday stress field indicates that inversions in NE Brazil can mainly be characterized as strike-slip and thrust fault regimes, whereas in N Brazil, inversions have occurred under reverse stress regimes. The most frequent inversion structures are reactivated faults, folds, and dome structures affecting the topography and the consequent uplift of rift and post-rift sedimentary units. Inversions have led to the reactivation of continental-scale structures, such as the strike-slip dextral shearing of the Transbrasiliano lineament, which affected rift and post-rift units in the Equatorial Margin of Brazil. The small crustal thickness of these areas favors inversion, as indicated by the most recent Moho depth map of South America. The interplay between far-field and near-field stresses explains the stress pattern in NE and N Brazil, where inversions have been observed.
AreaSRE
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4. Conditions of access and use
Languageen
Target File1-s2.0-S0895981123001670-main.pdf
User Groupsimone
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Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
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5. Allied materials
Next Higher Units8JMKD3MGPCW/46KUATE
Citing Item Listsid.inpe.br/bibdigital/2022/04.03.22.23 2
sid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
DisseminationWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Host Collectionurlib.net/www/2021/06.04.03.40
6. Notes
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