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1. Identity statement
Reference TypeJournal Article
Sitemtc-m12.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZ3ukuKE/Fbgam
Repositorysid.inpe.br/sergio/2005/02.15.07.39   (restricted access)
Last Update2005:02.15.02.00.00 (UTC) administrator
Metadata Repositorysid.inpe.br/sergio/2005/02.15.07.39.07
Metadata Last Update2018:06.05.00.40.55 (UTC) administrator
Secondary KeyINPE-12167-PRE/7507
ISSN0895-9811
Citation KeyRossettiAraú:2004:FaArTe
TitleFacies architecture in a tectonically-influenced estuarine incised valley fill of Miocene age, northern Brazil
Year2004
Access Date2024, Apr. 27
Secondary TypePRE PI
Number of Files1
Size1993 KiB
2. Context
Author1 Rossetti, Dilce de Fátima
2 Araújo Júnior, Antonio Emídio dos Santos de
Group1 DSR-INPE-MCT-BR
2
Affiliation1 Instituto Nacional de Pesquisas Espaciais. Coordenação de Observação da Terra. Divisaão de Sensoriamento Remoto
2 Universidade Federal do Para´, Centro de Geociências
JournalJournal of South American Earth Sciences
Volume17
Number4
Pages267 - 284
History (UTC)2006-05-17 13:54:16 :: sergio -> administrator ::
2006-09-03 21:44:26 :: administrator -> sergio ::
2007-04-23 21:08:29 :: sergio -> administrator ::
2018-06-05 00:40:55 :: administrator -> marciana :: 2004
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordsfacies analysis
incised valleys
Miocene Barreiras Formation
Rio Capim northern Brazil
sequence stratigraphy
AbstractThe Miocene Barreiras Formation in the Middle Rio Capim area records an incised valley system for which facies analysis and ichnology (Skolithos, Ophiomorpha, Planolites, Gyrolithes, Taenidium) suggest an estuarine character. Three stratigraphic units are recognized (from bottom to top): Unit 1 includes an inner estuarine tidal channel complex and tidal flat/salt marsh deposits; Unit 2 consists of estuarine bay/lagoon and flood tidal delta deposits related to the estuary mouth; and Unit 3 includes a tidal channel with a tidal point bar, as well as tidal flat/salt marsh deposits similar to those from Unit 1. These units and their bounding surfaces record the history of relative sea level changes in the estuary. After a sea level drop, the valley was inundated and formed an amalgamated sequence boundary and transgressive surface. Transgression (Unit 1) promoted the landward shift of flood tidal deltas and lagoon settings (Unit 2). The system then moved seaward, with the superposition of inner estuarine deposits (Unit 3) over Unit 2. Facies architecture seems to have been controlled by tectonics, as shown by: the paleovalley orientation according to the main tectonic structures of the basin; the presence of faults and fractures that displace the basal unconformity; and the abundance of soft sediment deformation.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Facies architecture in...
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4. Conditions of access and use
Languageen
Target Filefacies architeture.pdf
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sergio
Visibilityshown
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Read Permissiondeny from all and allow from 150.163
Update Permissiontransferred to sergio
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
DisseminationWEBSCI; PORTALCAPES.
Host Collectionsid.inpe.br/banon/2001/04.06.10.52
6. Notes
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7. Description control
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