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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@80/2006/07.31.20.37
Last Update2006:08.08.20.33.43 (UTC) administrator
Metadata Repositorysid.inpe.br/ePrint@80/2006/07.31.20.37.07
Metadata Last Update2018:06.04.04.12.45 (UTC) administrator
Citation KeyRossettiVale:2006:EvLoAm
TitleEvolution of the lowest amazon basin modeled from the integration of geological and srtm topographic data
Year2006
Access Date2024, May 18
Type of MediumOn-line
Secondary TypePRE PI
Number of Files2
Size244 KiB
2. Context
Author1 Rossetti, Dilce de Fátima
2 Valeriano, Márcio Morisson
Resume Identifier1 8JMKD3MGP5W/3C9JGTQ
Group1 DSR-INPE-MCT-BR
2 DSR-INPE-MCT-BR
Affiliation1 INPE
2 INPE
e-Mail Addressrossetti@dsr.inpe.br
Alternate PublicationCatena
ProducerInstituto Nacional de Pesquisas Espaciais
CitySão José dos Campos
Stage of Alternate Publicationpublished
History (UTC)2006-12-06 09:46:15 :: rossetti@dsr.inpe.br -> marciana ::
2008-04-26 01:40:00 :: marciana -> administrator ::
2018-06-04 04:12:45 :: administrator -> marciana :: 2006
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
KeywordsSRTM
modelagem topográfica
Marajó
geologia
geomorfologia
AbstractMorphologic features obtained from SRTM data, integrated with geologic information, are emphasized in this paper in order to provide the basis for understanding the development of the lowest Amazon drainage basin, focusing on the history of one of the largest Amazonian tributaries, the Tocantins River, and on the origin of the Marajó Island, throughout the Quaternary. This approach led to the recognition of a fan morphology related to the record of a tectonically controlled N/NW-S/SE orientated paleovalley cut down into Miocene and older rocks. The incised valley was fed by a paleo Tocantins River, which deposited its sediment load continuously to the north-northwest, reaching the Marajó Island and producing a deposit displaying a fan-morphology during the Plio-Pleistocene/Pleistocene. As characterized in the SRTM images, this channel system became abandoned due to capture by NE-SW orientated faults and establishment of the Pará River by W-E strike slip movements. This event, which probably took place in the Mid-Holocene, was responsible for detachment of the Marajó Island from the mainland.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Evolution of the...
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@80/2006/07.31.20.37
zipped data URLhttp://urlib.net/zip/sid.inpe.br/ePrint@80/2006/07.31.20.37
LanguageEnglish
Target Filev2.pdf
User Groupadministrator
marciana
rossetti@dsr.inpe.br
Visibilityshown
5. Allied materials
Next Editionsid.inpe.br/mtc-m12@80/2006/12.06.09.46
Next Higher Units8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.44.37 1
Host Collectionsid.inpe.br/mtc-m18@80/2008/03.17.15.17
6. Notes
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7. Description control
e-Mail (login)marciana
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