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1. Identity statement
Reference TypeJournal Article
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentifierJ8LNKAN8RW/36KNJC5
Repositorydpi.inpe.br/plutao@80/2009/12.22.14.16.51   (restricted access)
Last Update2010:04.23.11.30.19 (UTC) marciana
Metadata Repositorydpi.inpe.br/plutao@80/2009/12.22.14.16.52
Metadata Last Update2018:06.05.00.12.50 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.1016/j.cageo.2009.04.011
Labellattes: 0307721738107549 2 MantelliRosValVal:2009:ApSRDi
Citation KeyMantelliRossAlbuVale:2009:ApSRDi
TitleApplying SRTM digital elevation model to unravel Quaternary drainage in forested areas of Northeastern Amazonia
Year2009
Access Date2024, May 18
Type of Workjournal article
Number of Files1
Size1286 KiB
2. Context
Author1 Mantelli, Luiz Rogério
2 Rossetti, Dilce de Fátima
3 Albuquerque, Paulo Gurgel
4 Valeriano, Márcio de Morisson
Resume Identifier1
2 8JMKD3MGP5W/3C9JGTQ
3
4 8JMKD3MGP5W/3C9JHPL
Group1
2 DSR-OBT-INPE-MCT-BR
3 DSR-OBT-INPE-MCT-BR
4 DSR-OBT-INPE-MCT-BR
Affiliation1
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 undefined
4 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1
2 rossetti@dsr.inpe.br
3
4 valerian@dsr.inpe.br
e-Mail Addressrossetti@dsr.inpe.br
JournalComputers and Geosciences
Volume35
Number12
Pages2331-2337
History (UTC)2009-12-23 14:00:40 :: lattes -> marciana ::
2010-04-23 11:30:19 :: marciana -> administrator ::
2011-05-31 14:19:51 :: administrator -> marciana ::
2011-10-31 12:06:18 :: marciana -> administrator :: 2009
2016-06-04 01:08:37 :: administrator -> marciana :: 2009
2016-10-04 13:11:04 :: marciana -> administrator :: 2009
2018-06-05 00:12:50 :: administrator -> marciana :: 2009
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywords: Amazonia
Cenozoic
Continental area
Digital elevation model
Drainage systems
Flood-plains
Forest cover
Forested area
Geological data
High potential
Interferometric synthetic aperture radars
Morphological features
Northern Brazil
Paleo channel
Paleochannels
Paleodrainage
Paleoenvironmental reconstruction
Shuttle radar topography mission
SRTM
Study areas
Tectonic faults
Tectonic reactivation
Topographic surveys
Digital instruments
Drainage
Geodetic satellites
Geomorphology
Image classification
Imaging systems
Photoacoustic effect
Radar
Radar antennas
Remote sensing
Synthetic aperture radar
Synthetic apertures
Tectonics
Tracking radar
Surveying
digital elevation model
drainage network
floodplain
forest cover
geomorphology
interferometry
landscape evolution
paleochannel
paleoenvironment
Quaternary
rainforest
reconstruction
remote sensing
Shuttle Radar Topography Mission
synthetic aperture radar
tectonic setting
topographic mapping
Amazonia
South America
AbstractThere has been an increasing number of articles stressing the advantage of applying remote sensing products of synthetic aperture radar (SAR) and interferometric synthetic aperture radar (InSAR) for rapidly enhancing the volume of geological data in Amazonian areas, where forest cover is dense and high, clouds are abundant and accessibility is limited. The majority of these studies has emphasized geomorphology as a tool for both discussing tectonic reactivations during the Cenozoic and reconstructing Quaternary paleolandscapes. This work applies Digital Elevation Model (DEM) derived from the Shuttle Radar Topography Mission (SRTM) for delineating past morphological features under dense rainforest in an Amazonian lowland area. Previous use of this tool in southwestern Marajó Island (northern Brazil) helped to delineate, with exceptional precision, a paleochannel network hidden under the rainforest, which would be barely detected with other available remote sensing products. Fieldwork revealed that these paleochannels are related to palimpsest drainage systems developed mostly during the last 40,000 14C yr B.P. Measured altitudes acquired during topographic surveys attested that paleochannel areas are slightly higher than adjacent floodplains. This fact determined the successful application of SRTM-DEM for mapping paleochannels in Marajó Island. Integration of SRTM data with sedimentological information collected during fieldwork suggests paleoflows derived from continental areas located to south of the study area. This paleodrainage was active when the island was still connected to mainland. With island detachment due to reactivation of tectonic faults, the channels became abandoned and were progressively forested. The results obtained in the present study indicate that SRTM-DEM has high potential for unraveling similar morphological features from many other Amazonian areas with low topography and a dense forest cover.
AreaSRE
Arrangementurlib.net > DIDSR > Applying SRTM digital...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target Filemarcio.pdf
User Groupadministrator
lattes
marciana
Reader Groupadministrator
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Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.44.37 1
sid.inpe.br/mtc-m21/2012/07.13.14.54.54 1
DisseminationWEBSCI; PORTALCAPES.
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notes
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