| 1. Identity statement | ||||
| Reference Type | Journal Article | |||
| Site | mtc-m21b.sid.inpe.br | |||
| Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S | |||
| Identifier | 8JMKD3MGP3W34P/3LF2S5H | |||
| Repository | sid.inpe.br/mtc-m21b/2016/04.05.13.19 (restricted access) | |||
| Last Update | 2016:04.05.13.20.04 (UTC) simone | |||
| Metadata Repository | sid.inpe.br/mtc-m21b/2016/04.05.13.19.29 | |||
| Metadata Last Update | 2018:06.04.02.40.38 (UTC) administrator | |||
| DOI | 10.1016/j.precamres.2015.12.012 | |||
| ISSN | 0301-9268 | |||
| Citation Key | PadilhaVitoPáduFuck:2016:DeMaSi | |||
| Title | Deep magnetotelluric signatures of the early Neoproterozoic Cariris Velhos tectonic event within the Transversal sub-province of the Borborema Province, NE Brazil  | |||
| Year | 2016 | |||
| Month | Apr. | |||
| Access Date | 2024, May 23 | |||
| Type of Work | journal article | |||
| Secondary Type | PRE PI | |||
| Number of Files | 1 | |||
| Size | 4760 KiB | |||
| 2. Context | ||||
| Author | 1 Padilha, Antonio Lopes 2 Vitorello, Ícaro 3 Pádua, Marcelo Banik de 4 Fuck, Reinhardt Adolfo | |||
| Resume Identifier | 1 8JMKD3MGP5W/3C9JGJG 2 8JMKD3MGP5W/3C9JHD6 3 8JMKD3MGP5W/3C9JHNR | |||
| Group | 1 DGE-CEA-INPE-MCTI-GOV-BR 2 DGE-CEA-INPE-MCTI-GOV-BR 3 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 Universidade de Brasília (UnB) | |||
| Author e-Mail Address | 1 antonio.padilha@inpe.br 2 icaro@dge.inpe.br 3 marcelo.banik@inpe.br 4 reinhardt@unb.br | |||
| Journal | Precambrian Research | |||
| Volume | 275 | |||
| Pages | 70-83 | |||
| Secondary Mark | A1_INTERDISCIPLINAR A1_GEOCIÊNCIAS A1_CIÊNCIAS_AMBIENTAIS A2_QUÍMICA A2_ENGENHARIAS_II A2_ENGENHARIAS_I A2_CIÊNCIAS_BIOLÓGICAS_I A2_BIODIVERSIDADE B1_MATERIAIS | |||
| History (UTC) | 2016-04-05 13:19:29 :: simone -> administrator :: 2016-07-04 12:29:58 :: administrator -> simone :: 2016 2016-12-21 12:24:36 :: simone -> administrator :: 2016 2018-06-04 02:40:38 :: administrator -> simone :: 2016 | |||
| 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 | Northeast Brazil Borborema Province Magnetotellurics Subduction zone Neoproterozoic Cariris Velhos Orogeny | |||
| Abstract | The Borborema structural province, in northeast Brazil, consists of a complex set of crustal blocks of different ages, origin and evolution, with final amalgamation during the late Neoproterozoic Brasiliano Orogeny. In the central part of the province, its Transversal sub-province is characterized by elongate NE-SW terranes largely affected by the Brasiliano metamorphic overprinting and by a suite of early Neoproterozoic metavolcanic and metaplutonic rocks, reflecting a distinct tectonic event (Cariris Velhos). Magnetotelluric (MT) data were collected at 64 stations along four profiles across this central region of the province to assess its deep electrical resistivity structure. Dimensionality analysis shows that the subsurface is electrically dominated by 3D structure, and 3D inversions of the full impedance tensor and vertical magnetic transfer function (tipper) were carried out. Data fit is relatively good with an acceptable distribution of the misfit between the sites and the dominant features in the final model are north-dipping crustal conductors, which can be tentatively correlated between the different MT profiles and cross contrasting terranes at the surface of the province. Considering the geometry and distribution of the conductors, it is proposed that they might reflect remnants of a north-directed subduction zone with enhanced conductivity associated with graphitized biogenic material in metasedimentary rocks originally deposited in a restricted oceanic environment and subsequently metamorphosed and introduced into the deep crust by the subduction of the oceanic lithosphere. Constrained by isolated outcrops of early Neoproterozoic rocks with oceanic affinity, the proposed subduction event may have taken place during the Cariris Velhos Orogeny with the crustal remobilization by the Brasiliano Orogeny being restricted to the brittle upper crust. This interpretation gives support for an accretionary model to the Neoproterozoic geodynamic evolution of the Borborema Province. | |||
| Area | CEA | |||
| Arrangement | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDGE > Deep magnetotelluric signatures... | |||
| doc Directory Content | access | |||
| source Directory Content | there are no files | |||
| agreement Directory Content |
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| 4. Conditions of access and use | ||||
| Language | en | |||
| Target File | Padilha_deep.pdf | |||
| User Group | simone | |||
| Reader Group | administrator simone | |||
| Visibility | shown | |||
| Archiving Policy | denypublisher denyfinaldraft24 | |||
| Read Permission | deny from all and allow from 150.163 | |||
| Update Permission | not transferred | |||
| 5. Allied materials | ||||
| Mirror Repository | urlib.net/www/2011/03.29.20.55 | |||
| Next Higher Units | 8JMKD3MGPCW/3EU29DP | |||
| Citing Item List | sid.inpe.br/bibdigital/2013/10.01.22.11 4 sid.inpe.br/mtc-m21/2012/07.13.14.50.10 2 sid.inpe.br/mtc-m21/2012/07.13.14.54.32 1 | |||
| Dissemination | WEBSCI; PORTALCAPES; MGA; COMPENDEX; SCOPUS. | |||
| Host Collection | sid.inpe.br/mtc-m21b/2013/09.26.14.25.20 | |||
| 6. Notes | ||||
| Empty Fields | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url | |||
| 7. Description control | ||||
| e-Mail (login) | simone | |||
| update | ||||