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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorysid.inpe.br/ePrint@80/2006/12.06.09.21   (restricted access)
Last Update2006:12.06.08.34.03 (UTC) administrator
Metadata Repositorysid.inpe.br/ePrint@80/2006/12.06.09.21.53
Metadata Last Update2018:06.04.04.12.46 (UTC) administrator
Secondary KeyINPE--PRE/
ISSN0037-0738
Citation KeySantosJrRoss:2006:DeMoIp
TitleDepositional model of the Ipixuna Formation (Late Cretaceous-?Early Tertiary), Rio Capim area, Northern Brazil
Year2006
Month2006-05-03
Access Date2024, Apr. 27
Secondary TypePRE PI
Number of Files1
Size3208 KiB
2. Context
Author1 Santos Jr., Antônio Emídio de Araújos
2 Rossetti, Dilce de Fátima
Group1
2 DSR-INPE-MCT-BR
Affiliation1 UFPA
2 INPE
JournalSedimentary Geology
Volume13
Number2
Pages65-87
History (UTC)2007-05-15 12:19:01 :: rossetti -> marciana ::
2008-04-18 15:26:31 :: marciana -> administrator ::
2010-05-11 01:35:39 :: administrator -> marciana ::
2011-12-09 11:32:49 :: marciana -> administrator :: 2006
2018-06-04 04:12:46 :: administrator -> marciana :: 2006
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordspaleoambiente
sedimentologia
geologia
AbstractExposures along open quarries located in the eastern Cametá Sub-Basin provide a opportunity to assess further discussion focusing on the depositional environments of the Upper Cretaceous-?Lower Tertiary Ipixuna Formation. The lower part of this unit emphasized herein, known as the ?soft kaolin?, consists mostly of kaolinitized sandstones and mudstones that exhibit well preserved sedimentary structures that are particularly favorable for facies analysis and paleoenvironmental reconstructions. The sandstones are chiefly cross-stratified, typically with low angle, locally reverse orientated foresets with reactivation surfaces and/or mud drapes. These characteristics, together with a trace fossil assemblage consisting of Ophiomorpha, Thalassinoides, Planolites, Teichichnus, Taenidium and Skolithos, conform to deposition in a coastal setting influenced by tidal processes. Although a previous study has documented tidal processes during deposition of the soft kaolin (Santos Jr. and Rossetti, 2003), this paper shows that the influence of tidal currents was much more important than initially proposed. Hence, the kaolinitized deposits are attributed to tidally influenced fluvial channel (Facies Association A), tidal channel (Facies Association B), tidal flat/mangrove (Facies Association C), and tidal sand bar/tidal sandy flat (Facies Association D), all together comprising a tide-dominated estuarine system.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Depositional model of...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target FileMS-135.pdf
User Groupadministrator
banon
marciana
rossetti
Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Previous Editionsid.inpe.br/ePrint@80/2006/05.02.18.22
Next Higher Units8JMKD3MGPCW/3ER446E
DisseminationWEBSCI; PORTALCAPES; COMPENDEX.
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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