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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@80/2006/07.31.20.49
Last Update2006:07.31.20.49.21 (UTC) administrator
Metadata Repositorysid.inpe.br/ePrint@80/2006/07.31.20.49.19
Metadata Last Update2018:06.04.04.22.28 (UTC) administrator
Citation KeyRossettiGóesVale::InSpSe
TitleQuaternary syn-sedimentary seismic activities in eastern marajó island, brazil: integration of spatial and sedimentological data
Last Update Date2006-08-01
Access Date2024, May 18
Type of MediumOn-line
Secondary TypePRE PI
Number of Files1
Size35 KiB
2. Context
Author1 Rossetti, Dilce de Fátima
2 Góes, Ana Maria
3 Valeriano, Márcio Morisson
Resume Identifier1 8JMKD3MGP5W/3C9JGTQ
Group1 DSR-INPE-MCT-BR
2
3 DSR-INPE-MCT-BR
Affiliation1 INPE
2 USP
3 INPE
e-Mail Addressrossetti@dsr.inpe.br
Alternate PublicationQuaternary Sciences
ProducerInstituto Nacional de Pesquisas Espaciais
CitySăo José dos Campos
Stage of Alternate Publicationsubmitted
History (UTC)2008-04-26 01:40:00 :: rossetti -> administrator ::
2018-06-04 04:22:28 :: administrator -> rossetti ::
3. Content and structure
Is the master or a copy?is the master
Content Stagework-in-progress
Transferable1
KeywordsSRTM
modelagem topográfica
tectônica
Marajó
geologia
AbstractThis work aims to provide data to contribute with the reconstruction of the Quaternary tectono-sedimentary history of one of the largest fluvial Island in the world, the Marajó Island. Despite the location in a passive continental margin, the Marajó Island was characterized by great tectonic and sedimentary dynamism throughout the Quaternary. Evidences come from mapping of tectonic lineaments with basis on SRTM data and Landsat images, combined with interpretation of the sedimentary record in outcrops and cores. Four main groups of tectonic lineaments, orientated to the NNW/N/NNE-SSE/S/SSW, NW-SE, NE-SW and E-W/ENE-WSW/ESE-WNW, were recognized. Physical relationships among these features provide elements for discussing the succession of events. This procedure led to the recognition of an important tectonic phase producing NNW/N/NNE-SSE/S/SSW lineaments that predate all the other tectonic phases. Subsequent events resulted in more widespread deformation in the NW-SE, and then NE-SW directions, with the first having caused a slight depression of the eastern side of Marajó Island. E-W/ENE-WSW/ESE-WNW lineaments might have developed in different phases, both predating and post-dating the other tectonic events. This complex tectonic history left an impressive signature in the sedimentary record, consisting of an abundance of ductile and brittle structures. Detailed analysis of these features supports seismic activities contemporaneous or shortly after deposition, when the sediment was still unconsolidated or semi-consolidated. Thus, tectonics had a crucial role in the creation of new space to accommodate the Quaternary sedimentation in the eastern Marajó Island.
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/sid.inpe.br/ePrint@80/2006/07.31.20.49
zipped data URLhttp://urlib.net/zip/sid.inpe.br/ePrint@80/2006/07.31.20.49
LanguageEnglish
Target Filev1.pdf
User Groupadministrator
rossetti
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
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7. Description control
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