Close

1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZGivnK2Y/Svcba
Repositorysid.inpe.br/mtc-m17@80/2007/12.19.12.05   (restricted access)
Last Update2007:12.19.12.27.12 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m17@80/2007/12.19.12.05.34
Metadata Last Update2018:06.05.03.36.43 (UTC) administrator
Secondary KeyINPE--PRE/
ISSN0169-1317
Citation KeySantosJrRossMurr:2007:OrRiCa
TitleOrigins of the Rio Capim kaolinites (northern Brazil) revealed by delta O-18 and delta D analyses, coexisting minerals; northeastern japan; meteoric waters; climate-change; oxygen
Year2007
MonthSept.
Access Date2024, Apr. 28
Secondary TypePRE PI
Number of Files1
Size1350 KiB
2. Context
Author1 Santos Jr., Antonio Emidio de Araujo dos
2 Rossetti, Dilce de Fatima
3 Murray, Haydn H.
Resume Identifier1
2 8JMKD3MGP5W/3C9JGTQ
Group1
2 DSR-INPE-MCT-BR
Affiliation1 Universidade Federal do Pará/UFPa, Centro de Geociências, Campus do Guamá S/N Belém-PA
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 cIndiana University, Bloomington, Indiana
JournalApplied Clay Science
Volume37
Number3-4
Pages281-294
History (UTC)2008-11-04 16:40:23 :: marciana -> administrator ::
2018-06-05 03:36:43 :: administrator -> marciana :: 2007
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordsdelta o-18 and delta d
kaolinite
origin
rio capim kaolin
stratigraphy
northern brazil
hydrogen-isotope geochemistry
pedogenic clay-minerals
surface-temperature
exchange
deposits
AbstractDeuterium (delta D) and oxygen (delta 18O) isotope data from the Rio Capim kaolin, northem Brazil, were combined with optical studies in order to better understand the genesis and evolution of the kaolinites. The results show that 6180 values from a lower soft kaolin unit range from 6.0%. to 19.2 parts per thousand for Ka (size ranging from I to 3 mu m) and Kb (size ranging from 10 to 30 mu m) kaolinites, and from 15.4 parts per thousand to 24.9 parts per thousand for Kc (size < 200 nm) kaolinites. The delta D values range from -63.1 parts per thousand to 79.5 parts per thousand for the Ka+Kb kaolinites, and from -68.8 parts per thousand to -244.35 parts per thousand. for the Kc kaolinites. An upper semi flint kaolin unit, dominated by Kc kaolinites, displays 6180 and delta D values ranging from 15.1 parts per thousand to 21.8 parts per thousand, and -71.3 parts per thousand to -87.4 parts per thousand, respectively. Based on these data, and on the 6180 and delta D values obtained for the surface meteoric water and groundwater, it can be concluded that the kaolinites are not in equilibrium with the modem weathering environment, but they reflect isotopic cornpositions of the formation time, probably due to the interaction with fossil groundwater. However, mineralogical contaminations derived from replacements of framework grains also had great influence in the isotopic composition of these kaolinites. In addition, the isotope values of the Kc kaolinites from the semi-flint kaolin unit is variable, which is due to the presence of Kc kaolinites of different origins, including kaolinites derived from the underlying soft kaolin unit, kaolinites formed during different phases of pateoweathering, as well as later phases of coarse-grained kaolinites formed along fractures. Due to these complexities, binary diagrams contrasting 6180 and delta D values, worldwide applied for distinguishing supergenic from hypogenic kaolinites, as well as those formed under weathering conditions, can not be applied to interpret the origin of the kaolinites in the Rio Capim Kaolin.
AreaSRE
Arrangementurlib.net > Produção anterior à 2021 > DIDSR > Origins of the...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target Filecapimrio.pdf
User Groupadministrator
marciana
Visibilityshown
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
DisseminationWEBSCI; PORTALCAPES.
Host Collectionlcp.inpe.br/ignes/2004/02.12.18.39
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
Empty Fieldsalternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel documentstage doi e-mailaddress electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Description control
e-Mail (login)marciana
update 


Close