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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/44EDBU2
Repositorysid.inpe.br/mtc-m21c/2021/04.02.14.51   (restricted access)
Last Update2021:04.02.14.55.58 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2021/04.02.14.51.01
Metadata Last Update2022:04.03.22.28.28 (UTC) administrator
DOI10.1016/j.quaint.2020.10.051
ISSN1040-6182
Citation KeyAndradesFoRossBeze:2021:UnPoSt
TitleThe unsteady post-rift stage of the South American passive margin based on the tectono-sedimentary evolution of the onshore Paraíba Basin, NE Brazil
Year2021
MonthApr.
Access Date2024, May 19
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size49550 KiB
2. Context
Author1 Andrades Filho, Clódis de Oliveira
2 Rossetti, Dilce de Fátima
3 Bezerra, Francisco Hilário Rego
Resume Identifier1
2 8JMKD3MGP5W/3C9JGTQ
Group1
2 DIOTG-CGCT-INPE-MCTI-GOV-BR
Affiliation1 Universidade de São Paulo (USP)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Universidade Federal do Rio Grande do Norte (UFRN)
Author e-Mail Address1
2 dilce.rossetti@inpe.br
JournalQuaternary International
Volume580
Pages100-119
Secondary MarkA1_GEOGRAFIA A1_ANTROPOLOGIA_/_ARQUEOLOGIA A2_INTERDISCIPLINAR A2_GEOCIÊNCIAS B1_SAÚDE_COLETIVA B1_ODONTOLOGIA B1_MEDICINA_II B1_HISTÓRIA B1_ENGENHARIAS_II B1_BIODIVERSIDADE B2_CIÊNCIAS_BIOLÓGICAS_III B2_CIÊNCIAS_BIOLÓGICAS_I C_CIÊNCIAS_AGRÁRIAS_I
History (UTC)2021-04-02 14:55:59 :: simone -> administrator :: 2021
2022-04-03 22:28:28 :: administrator -> simone :: 2021
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsBrittle and ductile deformation
Tectono–sedimentary analysis
Neogene-late Pleistocene
Neotectonics
AbstractThe post-rift tectono-sedimentary history of passive margins has been an issue of increased interest after the perception of their unsteady nature during the Neogene and Quaternary. The evolution of the eastern South America margin might be benefited from investigations of the sedimentary record in a number of marginal basins. The Paraíba Basin is of particular interest to discuss the post-rift evolution of the South American passive margin, because it represents the last bridge with the African plate. This work aims to analyze the post-rift sedimentary record of the onshore Paraíba Basin as a contribution to discuss the neotectonic history of the South American passive margin. Surface and subsurface data were integrated from outcrops, deep stratigraphic profiles, airborne geophysical maps and remote sensing products. The depositional and denudational processes in this basin were a result of tectonic subsidence and uplifting. Tectonics after the main rifting phase are indicated by abundant structures, including normal, reverse, and strikeslip faults, as well as folds that affected the Neogene and Late Pleistocene sedimentary deposits. The ductile and brittle deformation resulted mainly from multiple reactivations of EW, NESW and NWSE trending basement shear zones. The deformation mechanism included distension and compression under a strikeslip regime. Tectonic reactivations even during the late Pleistocene support an unsteady South Atlantic passive continental margin throughout the postrifting stage.
AreaSRE
ArrangementThe unsteady post-rift...
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4. Conditions of access and use
Languageen
Target Fileandrades_unstead.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/46KUATE
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
sid.inpe.br/bibdigital/2022/04.03.22.23 1
DisseminationWEBSCI; PORTALCAPES; SCOPUS.
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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