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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorysid.inpe.br/mtc-m17@80/2007/12.21.15.33   (restricted access)
Last Update2011:12.05.10.57.33 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m17@80/2007/12.21.15.33.57
Metadata Last Update2018:06.05.03.36.52 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.1002/jqs.1132
ISSN0267-8179
Citation KeyGoesRossValeMira:2007:MaIsNo
TitleQuaternary tectonics in a passive margin: Marajó Island, northern Brazil. JQS
Year2007
MonthFeb.
Access Date2024, May 02
Secondary TypePRE PI
Number of Files1
Size1583 KiB
2. Context
Author1 Goes, Ana Maria
2 Rossetti, Dilce F.
3 Valeriano, Márcio de Morisson
4 Miranda, A. C. da C
Group1
2 DSR-INPE-MCT-BR
3 DSR-INPE-MCT-BR
Affiliation1 Univ Sao Paulo, Inst Geosci
JournalJournal of Quaternary Science
Volume23
Number2
Pages121–135
History (UTC)2007-12-21 15:45:57 :: marciana -> banon ::
2010-05-10 18:41:54 :: banon -> administrator ::
2010-05-11 02:15:04 :: administrator -> marciana ::
2011-12-05 10:57:33 :: marciana -> administrator :: 2007
2018-06-05 03:36:52 :: administrator -> marciana :: 2007
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordstectonics
Quaternary
Marajo´ Island
sedimentary structure
soft sediment deformation
spatial analysis
AbstractMarajó Island is located in a passive continental margin that evolved from rifting associated with the opening of the Equatorial South Atlantic Ocean in the Late Jurassic/Early Cretaceous period. This study, based on remote sensing integrated with sedimentology, as well as subsurface and seismographic data available from the literature, allows discussion of the significance of tectonics during the Quaternary history of marginal basins. Results show that eastern Marajó Island contains channels with evidence of tectonic control. Mapping of straight channels defined four main groups of lineaments (i.e. NNESSW, NESW, NWSE and EW) that parallel main normal and strike-slip fault zones recorded for the Amazon region. Additionally, sedimentological studies of late Quaternary and Holocene deposits indicate numerous ductile and brittle structures within stratigraphic horizons bounded by undeformed strata, related to seismogenic deformation during or shortly after sediment deposition. This conclusion is consistent with subsurface Bouguer mapping suggestive of eastern Marajó Island being still part of the Marajó graben system, where important fault reactivation is recorded up to the Quaternary. Together with the recognition of several phases of fault reactivation, these data suggest that faults developed in association with rift basins might remain active in passive margins, imposing important control on development of depositional systems.
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Arrangementurlib.net > BDMCI > Fonds > Produçăo anterior ŕ 2021 > DIDSR > Quaternary tectonics in...
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Languageen
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banon
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5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
DisseminationWEBSCI; PORTALCAPES.
Host Collectionlcp.inpe.br/ignes/2004/02.12.18.39
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6. Notes
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