| 1. Identity statement | |
| Reference Type | Journal Article |
| Site | plutao.sid.inpe.br |
| Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
| Identifier | 8JMKD3MGP3W/3P5U6P2 |
| Repository | sid.inpe.br/plutao/2017/06.22.00.45 (restricted access) |
| Last Update | 2017:06.23.17.10.09 (UTC) administrator |
| Metadata Repository | sid.inpe.br/plutao/2017/06.22.00.45.19 |
| Metadata Last Update | 2018:06.04.23.26.36 (UTC) administrator |
| DOI | 10.1016/j.quaint.2016.03.026 |
| ISSN | 1040-6182 |
| Label | lattes: 0307721738107549 2 LimaRoBeBaMeCaVa:2017:NeFaRe |
| Citation Key | LimaRoBaMeCaVa:2017:NeFaRe |
| Title | Neogene-quaternary fault reactivation influences coastal basin sedimentation and landform in the continental margin of NE Brazil  |
| Year | 2017 |
| Access Date | 2024, Apr. 23 |
| Type of Work | journal article |
| Secondary Type | PRE PI |
| Number of Files | 1 |
| Size | 12665 KiB |
| 2. Context | |
| Author | 1 Lima, Jean C. F. 2 Rossetti, Dilce de Fátima 3 Barbosa, José A. 4 Medeiros, Walter Eugênio de 5 Castro, David L. de 6 Vasconcelos, David L. |
| Resume Identifier | 1 2 8JMKD3MGP5W/3C9JGTQ |
| Group | 1 2 DIDSR-CGOBT-INPE-MCTIC-GOV-BR |
| Affiliation | 1 Universidade Federal do Rio Grande do Norte (UFRN) 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Universidade Federal de Pernambuco (UFPE) 4 Universidade Federal do Rio Grande do Norte (UFRN) 5 Universidade Federal do Rio Grande do Norte (UFRN) 6 Universidade Federal do Rio Grande do Norte (UFRN) |
| Author e-Mail Address | 1 2 dilce.rossetti@inpe.br |
| Journal | Quaternary International |
| Volume | 438 |
| Pages | 92-107 |
| Secondary Mark | A1_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) | 2017-06-23 17:10:09 :: lattes -> administrator :: 2017 2017-07-03 05:06:45 :: administrator -> lattes :: 2017 2017-12-05 15:40:20 :: lattes -> administrator :: 2017 2017-12-06 05:17:25 :: administrator -> lattes :: 2017 2017-12-11 14:28:04 :: lattes -> administrator :: 2017 2018-06-04 23:26:36 :: administrator -> simone :: 2017 |
| 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 | Post-rift reactivation neotectonic landform neogene-quaternary sedimentation |
| Abstract | We investigate the role of reactivation of Precambrian basement fabric in the tectono-sedimentary and geomorphological evolution of the Paraíba Basin, continental margin of northeastern Brazil, during the Cretaceous, Neogene, and Quaternary. This basin represents part of the last bridge between South America and Africa before the last breakup stage of the South Atlantic rifting in the early Cretaceous. The Paraíba Basin infill is composed of siliciclastic and carbonate Cretaceous units, as well as aeolian, fluvial and marine Quaternary units. We used shuttle radar imagery, aeromagnetic, wellbore and field data. The reduced-to-the-pole magnetic map (RTP) indicates the continuity of the steeply dipping Precambrian basement shear zones beneath the Paraíba Basin. The combined analysis of surface and subsurface data shows that NE-SW and E-W-striking shear zones were subjected to brittle reactivation in the Aptian-Middle Albian during the basin opening and again in the Neogene-Quaternary, forming a system of horsts and grabens along the basin; some of these structures such as the E-W-oriented Pernambuco shear zone present modern-day seismicity. N-S- and mainly NW-SE-striking transfer faults cut across Aptian-Middle Albian to Neogene-Quaternary strata. These four main fault directions control main river channels and alluvial valleys up to 2 km wide. Topographic breaks up to 50 m were created by late reactivation of rift faults, which mark the boundary between horsts and grabens along the basin. In addition, structural data evidence syn-tectonic faulting with vertical offsets up to 80 m in the Cretaceous and up to 70 m in the Neogene-Quaternary. We conclude that shear zones across the study area are long-lived structures that have behaved as weakness zones. Their neotectonic brittle reactivation has controlled sediment deposition and landform development, which continued through the Neogene-Quaternary. |
| Area | SRE |
| Arrangement | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Neogene-quaternary fault reactivation... |
| doc Directory Content | access |
| source Directory Content | there are no files |
| agreement Directory Content | there are no files |
| 4. Conditions of access and use | |
| Language | en |
| Target File | lima_neogene.pdf |
| Reader Group | administrator lattes |
| Visibility | shown |
| Read Permission | deny from all and allow from 150.163 |
| Update Permission | not transferred |
| 5. Allied materials | |
| Next Higher Units | 8JMKD3MGPCW/3ER446E |
| Citing Item List | sid.inpe.br/bibdigital/2013/09.13.21.11 4 sid.inpe.br/mtc-m21/2012/07.13.14.44.37 1 |
| Dissemination | WEBSCI; PORTALCAPES; SCOPUS. |
| Host Collection | dpi.inpe.br/plutao@80/2008/08.19.15.01 |
| 6. Notes | |
| Empty Fields | alternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn lineage mark mirrorrepository month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url usergroup |
| 7. Description control | |
| e-Mail (login) | simone |
| update | |