Partitioning of transition elements between clinopyroxene and garnet
Identifieur interne : 000525 ( France/Analysis ); précédent : 000524; suivant : 000526Partitioning of transition elements between clinopyroxene and garnet
Auteurs : C. Dupuy [France] ; J. Dostal [Canada] ; J. M. Liotard [France] ; A. Leyreloup [France]Source :
- Earth and Planetary Science Letters [ 0012-821X ] ; 1980.
Abstract
Abstract: Abundances of transition elements (Ti, V, Cr, Mn, Fe2+, Co, Ni, Cu and Zn) in coexisting clinopyroxene and garnet are used to estimate clinopyroxene/garnet partition coefficients for these elements. The analyzed samples include eclogites, granulites and peridotites. The partition coefficients are sensitive to the major element composition of the mineral phases, although for individual transition elements they correlate with different chemical parameters. The partition coefficients of Ti correlate with the (FeO/MgO)garnet/(FeO/MgO)clinopyroxene ratio thus suggesting that the partitioning of Ti is a sensitive indicator of the physical (temperature-pressure) conditions of equilibration.
Url:
DOI: 10.1016/0012-821X(80)90194-6
Affiliations:
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 000D88
- to stream Istex, to step Curation: 000949
- to stream Istex, to step Checkpoint: 001098
- to stream Main, to step Merge: 001A13
- to stream Main, to step Curation: 001951
- to stream Main, to step Exploration: 001951
- to stream France, to step Extraction: 000525
Links to Exploration step
ISTEX:2FAA38FCB914E6FAC77969DE378A9F98418A869BLe document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Partitioning of transition elements between clinopyroxene and garnet</title>
<author><name sortKey="Dupuy, C" sort="Dupuy, C" uniqKey="Dupuy C" first="C." last="Dupuy">C. Dupuy</name>
</author>
<author><name sortKey="Dostal, J" sort="Dostal, J" uniqKey="Dostal J" first="J." last="Dostal">J. Dostal</name>
</author>
<author><name sortKey="Liotard, J M" sort="Liotard, J M" uniqKey="Liotard J" first="J. M." last="Liotard">J. M. Liotard</name>
</author>
<author><name sortKey="Leyreloup, A" sort="Leyreloup, A" uniqKey="Leyreloup A" first="A." last="Leyreloup">A. Leyreloup</name>
</author>
</titleStmt>
<publicationStmt><idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:2FAA38FCB914E6FAC77969DE378A9F98418A869B</idno>
<date when="1980" year="1980">1980</date>
<idno type="doi">10.1016/0012-821X(80)90194-6</idno>
<idno type="url">https://api.istex.fr/document/2FAA38FCB914E6FAC77969DE378A9F98418A869B/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">000D88</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000D88</idno>
<idno type="wicri:Area/Istex/Curation">000949</idno>
<idno type="wicri:Area/Istex/Checkpoint">001098</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Checkpoint">001098</idno>
<idno type="wicri:doubleKey">0012-821X:1980:Dupuy C:partitioning:of:transition</idno>
<idno type="wicri:Area/Main/Merge">001A13</idno>
<idno type="wicri:Area/Main/Curation">001951</idno>
<idno type="wicri:Area/Main/Exploration">001951</idno>
<idno type="wicri:Area/France/Extraction">000525</idno>
</publicationStmt>
<sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Partitioning of transition elements between clinopyroxene and garnet</title>
<author><name sortKey="Dupuy, C" sort="Dupuy, C" uniqKey="Dupuy C" first="C." last="Dupuy">C. Dupuy</name>
<affiliation wicri:level="1"><country xml:lang="fr">France</country>
<wicri:regionArea>Centre Géologique et Géophysique, USTL</wicri:regionArea>
<wicri:noRegion>USTL</wicri:noRegion>
<wicri:noRegion>USTL</wicri:noRegion>
</affiliation>
</author>
<author><name sortKey="Dostal, J" sort="Dostal, J" uniqKey="Dostal J" first="J." last="Dostal">J. Dostal</name>
<affiliation wicri:level="1"><country xml:lang="fr">Canada</country>
<wicri:regionArea>Department of Geology, Saint Mary's University, Halifax</wicri:regionArea>
<wicri:noRegion>Halifax</wicri:noRegion>
</affiliation>
</author>
<author><name sortKey="Liotard, J M" sort="Liotard, J M" uniqKey="Liotard J" first="J. M." last="Liotard">J. M. Liotard</name>
<affiliation wicri:level="1"><country xml:lang="fr">France</country>
<wicri:regionArea>Laboratoire de Pétrologie, USTL</wicri:regionArea>
<wicri:noRegion>USTL</wicri:noRegion>
<wicri:noRegion>USTL</wicri:noRegion>
</affiliation>
</author>
<author><name sortKey="Leyreloup, A" sort="Leyreloup, A" uniqKey="Leyreloup A" first="A." last="Leyreloup">A. Leyreloup</name>
<affiliation wicri:level="1"><country xml:lang="fr">France</country>
<wicri:regionArea>Laboratoire de Pétrologie, USTL</wicri:regionArea>
<wicri:noRegion>USTL</wicri:noRegion>
<wicri:noRegion>USTL</wicri:noRegion>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series><title level="j">Earth and Planetary Science Letters</title>
<title level="j" type="abbrev">EPSL</title>
<idno type="ISSN">0012-821X</idno>
<imprint><publisher>ELSEVIER</publisher>
<date type="published" when="1980">1980</date>
<biblScope unit="volume">48</biblScope>
<biblScope unit="issue">2</biblScope>
<biblScope unit="page" from="303">303</biblScope>
<biblScope unit="page" to="310">310</biblScope>
</imprint>
<idno type="ISSN">0012-821X</idno>
</series>
<idno type="istex">2FAA38FCB914E6FAC77969DE378A9F98418A869B</idno>
<idno type="DOI">10.1016/0012-821X(80)90194-6</idno>
<idno type="PII">0012-821X(80)90194-6</idno>
<idno type="ArticleID">80901946</idno>
</biblStruct>
</sourceDesc>
<seriesStmt><idno type="ISSN">0012-821X</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass></textClass>
<langUsage><language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">Abstract: Abundances of transition elements (Ti, V, Cr, Mn, Fe2+, Co, Ni, Cu and Zn) in coexisting clinopyroxene and garnet are used to estimate clinopyroxene/garnet partition coefficients for these elements. The analyzed samples include eclogites, granulites and peridotites. The partition coefficients are sensitive to the major element composition of the mineral phases, although for individual transition elements they correlate with different chemical parameters. The partition coefficients of Ti correlate with the (FeO/MgO)garnet/(FeO/MgO)clinopyroxene ratio thus suggesting that the partitioning of Ti is a sensitive indicator of the physical (temperature-pressure) conditions of equilibration.</div>
</front>
</TEI>
<affiliations><list><country><li>Canada</li>
<li>France</li>
</country>
</list>
<tree><country name="France"><noRegion><name sortKey="Dupuy, C" sort="Dupuy, C" uniqKey="Dupuy C" first="C." last="Dupuy">C. Dupuy</name>
</noRegion>
<name sortKey="Leyreloup, A" sort="Leyreloup, A" uniqKey="Leyreloup A" first="A." last="Leyreloup">A. Leyreloup</name>
<name sortKey="Liotard, J M" sort="Liotard, J M" uniqKey="Liotard J" first="J. M." last="Liotard">J. M. Liotard</name>
</country>
<country name="Canada"><noRegion><name sortKey="Dostal, J" sort="Dostal, J" uniqKey="Dostal J" first="J." last="Dostal">J. Dostal</name>
</noRegion>
</country>
</tree>
</affiliations>
</record>
Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Terre/explor/CobaltMaghrebV1/Data/France/Analysis
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000525 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/France/Analysis/biblio.hfd -nk 000525 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien |wiki= Wicri/Terre |area= CobaltMaghrebV1 |flux= France |étape= Analysis |type= RBID |clé= ISTEX:2FAA38FCB914E6FAC77969DE378A9F98418A869B |texte= Partitioning of transition elements between clinopyroxene and garnet }}
This area was generated with Dilib version V0.6.32. |