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1. Identity statement
Reference TypeConference Paper (Conference Proceedings)
Sitemarte2.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP6W34M/3JM4532
Repositorysid.inpe.br/marte2/2015/06.15.14.06
Last Update2015:06.15.14.06.00 (UTC) administrator
Metadata Repositorysid.inpe.br/marte2/2015/06.15.14.06.01
Metadata Last Update2018:06.06.03.17.45 (UTC) administrator
ISBN978-85-17-0076-8
Label41
Citation KeyRossetti:2015:ImUnNe
TitleImaging underwater neotectonic structures in the Amazonian lowland
FormatInternet
Year2015
Access Date2024, May 18
Secondary TypePRE CN
Number of Files1
Size7072 KiB
2. Context
AuthorRossetti, Dilce de Fátima
Resume Identifier8JMKD3MGP5W/3C9JGTQ
GroupDSR-OBT-INPE-MCTI-GOV-BR
AffiliationInstituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Addressrossetti@dsr.inpe.br
EditorGherardi, Douglas Francisco Marcolino
Aragão, Luiz Eduardo Oliveira e Cruz de
e-Mail Addresswanderf@dsr.inpe.br
Conference NameSimpósio Brasileiro de Sensoriamento Remoto, 17 (SBSR)
Conference LocationJoão Pessoa
Date25-29 abr. 2015
PublisherInstituto Nacional de Pesquisas Espaciais (INPE)
Publisher CitySão José dos Campos
Pages185-191
Book TitleAnais
OrganizationInstituto Nacional de Pesquisas Espaciais (INPE)
History (UTC)2015-06-15 14:06:01 :: banon -> administrator ::
2018-06-06 03:17:45 :: administrator -> simone :: 2015
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
AbstractPrevious documentation has proposed tectonic activity from the Neogene to Holocene as one important control on the drainage development in the Amazonian lowland. However, recording tectonic structures in this region has been challenging due to environmental difficulties including the low topography and dense vegetation cover that do not favor natural exposures. For this reason, the role of tectonics in determining river dynamics, morphology, and sediment deposition in Amazonia has been suggested with caution. Despite limitations, morphostructural lineaments have provided useful information to support fault reactivation in several areas of the Amazonian lowland. However, further documentation is required to map the faults and describe their geometry. This approach is essential to better understand the geotectonic model of this region. In this work, analyses of highresolution optical imagery of three Amazonian shallow water lakes provided exceptional views of an abundance of linear features on the beds of these lakes. Although based on indirect evidence from remote sensing data, the quality of the images allowed the geometry of these underwater features to be characterized in detail. The most striking are sets of NESW lineaments that frequently intercept NWSE trending lineaments with offsets of up to 500 m in the horizontal plane. These characteristics support dextral faults with strikeslip rates in the study areas. The faults display trends compatible with the geotectonic model proposed for the Brazilian Amazonia region. They also control the morphology of lakes and rivers, as indicated by the fact that they parallel and/or continue into straight lineaments that define lake margins and river courses, including the courses of large rivers, such as the Solimões and Amazonas Rivers. Available radiocarbon ages of deposits from the lake bed sediments and from related floodplain deposits are consistent with the proposal of faulting during the latest Holocene, even only a few hundred years ago.
AreaSRE
TypeGeologia
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/8JMKD3MGP6W34M/3JM4532
zipped data URLhttp://urlib.net/zip/8JMKD3MGP6W34M/3JM4532
Languageen
Target Filep0041.pdf
User Groupadministrator
banon
Visibilityshown
5. Allied materials
Mirror Repositoryurlib.net/www/2011/03.29.20.55
Next Higher Units8JMKD3MGP6W34M/3JJLLP2
8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/marte2/2015/05.31.21.54 6
sid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
Host Collectiondpi.inpe.br/marte2/2013/05.17.15.03.06
6. Notes
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