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1. Identity statement
Reference TypeePrint (Electronic Source)
Sitemtc-m16c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorysid.inpe.br/ePrint@80/2006/12.06.10.23
Last Update2006:12.06.09.24.02 (UTC) administrator
Metadata Repositorysid.inpe.br/ePrint@80/2006/12.06.10.23.59
Metadata Last Update2018:06.04.04.22.30 (UTC) administrator
Citation KeyRossetti::ExUpCr
TitleThe Role of Tectonics on Preservation of Incised-Valley Estuaries in Areas with Low Accommodation Rates: Examples from Upper Cretaceous and Miocene Successions in Northern Brazil
Last Update Date2006-12-07
Access Date2024, May 18
Type of MediumOn-line
Secondary TypePRE PI
Number of Files1
Size66 KiB
2. Context
AuthorRossetti, Dilce de Fátima
Resume Identifier8JMKD3MGP5W/3C9JGTQ
GroupDSR-INPE-MCT-BR
AffiliationInstituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Addressrossetti@dsr.inpe.br
ProducerInstituto Nacional de Pesquisas Espaciais
CitySão José dos Campos
ProgressePrint update
History (UTC)2006-12-06 10:24:02 :: rossetti@dsr.inpe.br -> administrator ::
2007-11-28 19:26:20 :: administrator -> rossetti@dsr.inpe.br ::
2008-04-26 01:40:01 :: rossetti@dsr.inpe.br -> administrator ::
2018-06-04 04:22:30 :: administrator -> rossetti@dsr.inpe.br ::
3. Content and structure
Is the master or a copy?is the master
Content Stagework-in-progress
Transferable1
Keywordstectonics
incised valley
stratigraphic organization
facies
Late Cretaceous
Miocene
Abstract: Detailed facies and stratigraphic investigation of Upper Cretaceous and Miocene incised-valley estuarine successions from the São Luís-Grajaú Basin and Cametá Sub-basin, northern equatorial Brazilian margin, highlights the importance of tectonics in valley establishment and infill in areas with low accommodation rates. These deposits, corresponding to the Ipixuna/Cujupe formations and the Pirabas/Barreiras formations, respectively, were formed in a variety of depositional environments attributed mostly to wave-dominated estuaries formed within incised-valley systems. Instead of filling the valleys continuously, deposition took place during the transgressive to highstand stages of several relative sea level cycles, producing compound fills. Although other causes (e.g., eustasy) can not be completely ruled out, tectonic influence on valley evolution is suggested by: 1. vertical superposition of chronologically distinct incised valley successions; 2. time gap of several million years between the two overlapping paleovalleys in both basins, which indicates that sediment preservation took place solely when accommodation space was created by the increase in subsidence; 3. overall orientation of estuarine channels parallel to the main structural features of the basins; 4. faults that disrupt basal unconformities; and 5. stratigraphic horizons with a variety of seismogenic soft-sediment deformation structures between undeformed strata. A tectonic model for valley development is proposed, which involves channel capture in fault-produced depressions. Increased accommodation space favors thicker estuarine deposition in downdropped areas as transgression takes place, which have greater preservation potential. A subsequent phase of tectonic stability promotes aggradation and even progradation. Eventually, this process culminates with periods of subaerial exposure and soil development, resulting high frequency unconformities. Subsequent episodes of tectonic reactivation lead to renewed subsidence, which starts the process over again, resulting in compound valley fills. .
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > The Role of...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
data URLhttp://urlib.net/ibi/sid.inpe.br/ePrint@80/2006/12.06.10.23
zipped data URLhttp://urlib.net/zip/sid.inpe.br/ePrint@80/2006/12.06.10.23
Languageen
Target Filev1.pdf
User Groupadministrator
rossetti@dsr.inpe.br
administrator
Visibilityshown
Update Permissiontransferred to ePrint update
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
Host Collectionsid.inpe.br/mtc-m18@80/2008/03.17.15.17
6. Notes
Empty Fieldsaccessyear alternatepublication archivingpolicy archivist contenttype copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition format identifier isbn issn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit project readergroup readpermission rightsholder schedulinginformation secondarydate secondarykey secondarymark session shorttitle sponsor stageofalternatepublication subject tertiarymark tertiarytype url versiontype year
7. Description control
e-Mail (login)rossetti@dsr.inpe.br
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