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1. Identity statement
Reference TypeJournal Article
Sitemtc-m12.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorysid.inpe.br/mtc-m12@80/2006/12.06.09.46   (restricted access)
Last Update2010:05.13.11.31.01 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m12@80/2006/12.06.09.46.07
Metadata Last Update2018:06.05.00.40.47 (UTC) administrator
Secondary KeyINPE--PRE/
ISSN0341-8162
Citation KeyRossettiVale:2007:EvLoAm
TitleEvolution of the lowest amazon basin modeled from the integration of geological and srtm topographic data
Year2007
MonthJul.
Access Date2024, Apr. 28
Secondary TypePRE PI
Number of Files1
Size3310 KiB
2. Context
Author1 Rossetti, Dilce de Fátima
2 Valeriano, Márcio Morisson
Group1 DSR-INPE-MCT-BR
2 DSR-INPE-MCT-BR
Affiliation1 INPE
2 INPE
e-Mail Addressrossetti@dsr.inpe.br
JournalCatena
Volume70
Number2
Pages253-265
History (UTC)2007-04-23 21:05:26 :: rossetti@dsr.inpe.br -> marciana ::
2007-12-21 15:53:20 :: marciana -> administrator ::
2010-05-12 04:12:16 :: administrator -> marciana ::
2011-11-03 12:20:07 :: marciana -> administrator :: 2007
2018-06-05 00:40:47 :: administrator -> marciana :: 2007
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
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
Languageen
Target Filedilce.pdf
User Groupadministrator
marciana
rossetti@dsr.inpe.br
Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Previous Editionsid.inpe.br/ePrint@80/2006/07.31.20.37
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
e-Mail (login)marciana
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