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      <source-app name="Horizon">Horizon</source-app>
      <rec-number>1</rec-number>
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        <key app="Horizon" db-id="fdi:010062020">1</key>
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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Feneyrol, J.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Giuliani, Gaston</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ohnenstetter, D.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Rondeau, B.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Fritsch, E.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Fallick, A. E.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ichang'i, D.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Omito, E.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Rakotondrazafy, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ranatsenho, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Lallier, F.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>New typology and origin of tsavorite based on trace-element chemistry</title>
        <secondary-title>European Journal of Mineralogy</secondary-title>
      </titles>
      <pages>293-308</pages>
      <keywords>
        <keyword>tsavorite</keyword>
        <keyword>green grossular</keyword>
        <keyword>electron microprobe analysis</keyword>
        <keyword>UV-Vis-NIR</keyword>
        <keyword>absorption spectra</keyword>
        <keyword>chemical typology</keyword>
        <keyword>V/Cr ratio</keyword>
        <keyword>garnet</keyword>
        <keyword>geographic origin</keyword>
        <keyword>gemmology</keyword>
        <keyword>AFRIQUE DE L'EST</keyword>
        <keyword>KENYA</keyword>
        <keyword>TANZANIE</keyword>
        <keyword>MADAGASCAR</keyword>
      </keywords>
      <dates>
        <year>2014</year>
      </dates>
      <call-num>fdi:010062020</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>European Journal of Mineralogy</full-title>
      </periodical>
      <isbn>0935-1221</isbn>
      <accession-num>ISI:000334918100009</accession-num>
      <number>2</number>
      <electronic-resource-num>10.1127/0935-1221/2014/0026-2367</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010062020</url>
        </related-urls>
        <pdf-urls>
          <url>https://www.documentation.ird.fr/intranet/publi/2014/06/010062020.pdf</url>
        </pdf-urls>
      </urls>
      <volume>26</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>New electron-microprobe analyses of 'tsavorites' from the Neoproterozoic Metamorphic Mozambique Belt deposits allow the characterization of green grossular according to its trace-element chemistry (V, Cr, Mn). Five chemical types are defined: type 1, vanadian grossular with V &gt; Cr &gt; Mn (in atoms per formula unit); type 2, vanadian grossular with V &gt; Mn &gt; Cr; type 3, Mn-bearing vanadian grossular with Mn &gt; V &gt; Cr; type 4, Mn-bearing chromian grossular with Mn &gt; Cr &gt; V; and type 5, Cr- and Mn-bearing grossular with Cr &gt; Mn &gt; V. These types are also characterized by different absorption spectra in the ultraviolet-visible-near infrared. Type 1 tsavorite spectra show a total absorption below 430 nm due to the high vanadium contents. Type 2 tsavorite spectra present the classical absorption bands of V. Types 3 and 4 tsavorite spectra display additional shoulders at 407 and 408 nm due to Mn2+, whereas spectra of Cr-bearing types 4 and 5 tsavorite show the two additional bands of Cr3+ at 697 and 701 nm. The different absorption spectra also indicate Fe2+-Ti4+ charge transfer. We measured OH equivalent to 0.08 to 0.38 wt% eq. H2O within the structure. Concentrations of vanadium, chromium and manganese are good chemical "fingerprints" for determining the geographic provenance of economic tsavorite from Kenya, Tanzania and Madagascar.</abstract>
      <custom6>064</custom6>
      <custom1>UR234</custom1>
      <custom7>Kenya / Madagascar</custom7>
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