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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/iris@1912/2005/12.26.11.14   (restricted access)
Last Update2005:12.26.11.14.00 (UTC) administrator
Metadata Repositorysid.inpe.br/iris@1912/2005/12.26.11.14.30
Metadata Last Update2018:06.05.00.40.34 (UTC) administrator
Secondary KeyINPE-13292-PRE/8534
ISSN0037-0746
Citation KeyPazRossMaca:2005:InFaIs
TitleAn upper aptian saline pan/lake system from the Brazilian equatorial margin: integration of facies and isotopes
Year2005
MonthDec.
Access Date2024, Apr. 27
Secondary TypePRE PI
Number of Files1
Size2018 KiB
2. Context
Author1 Paz, J. D. S.
2 Rossetti, Dilce de Fátima
3 Macambira, M. J. B.
Group1 DSR-INPE-MCT-BR
Affiliation1
2 Instituto Nacional de Pesquisas Espaciais, Divisão de Sensoriamento Remoto (INPE, DSR)
JournalSedimentology
Volume52
Number6
Pages1303-1321
History (UTC)2006-03-24 14:07:34 :: sergio -> administrator ::
2006-09-03 21:43:10 :: administrator -> sergio ::
2007-04-23 21:07:07 :: sergio -> administrator ::
2008-06-09 19:20:36 :: administrator -> marciana ::
2011-10-31 11:52:04 :: marciana -> sergio ::
2011-10-31 11:54:57 :: sergio -> administrator :: 2005
2018-06-05 00:40:34 :: administrator -> sergio :: 2005
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsGEOLOGIA
Brazil (NE)
isotope
sedimentary facies
sulphur / strontium isotopes
non-marine
evaporites
origin
basin
water
paleohydrology
paleocene
AbstractFacies and isotope (Sr and S) data were combined in order to discuss the genesis and palaeohydrology of an Upper Aptian evaporite succession formed during the initial development of an intra-continental rift from northern Brazil. Comparison of facies distribution between two investigated areas shows: (i) stable, well-stratified and hypersaline lakes with periods of anoxia and closure in the eastern margin of the basin, where there was evaporite precipitation only in central lake environments; and (ii) more ephemeral conditions in the eastern margin of the basin, where a saline pan complex developed and evaporite precipitation took place mainly in marginal salinas and surrounding mudflats. In both areas, expansion/contraction cycles developed as sedimentation took place, accompanied by a decrease and then an increase in Sr-87/Sr-86- and delta(34)S-isotope values. This, combined with the wide distribution of Sr- and S-isotope data within individual depositional cycles, as well as petrographic and scanning electronic microscopic (SEM) images, led to the conclusion that diagenesis was not enough to obscure the primary geochemical signature. A non-marine brine source is suggested by Sr-87/Sr-86 ratios between 0.707824 and 0.709280, which are higher than those from Upper Aptian sea water (i.e. between 0.70720 and 0.70735). The delta(34)S value varies from 16.12 to 17.89 parts per thousand in the eastern margin of the basin, which is in disagreement with Upper Aptian marine values (13 to 16 parts per thousand). Both geochemical tracers were influenced by facies characteristics, and thus a model is provided, where Sr-87/Sr-86 values respond to changes in expansion and contraction episodes of saline pan/lake systems.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > An upper aptian...
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4. Conditions of access and use
Languageen
Target FileAn upper aptian saline.pdf
User Groupadministrator
sergio
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
DisseminationWEBSCI; PORTALCAPES.
Host Collectionsid.inpe.br/banon/2001/04.06.10.52
6. Notes
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