<?xml version="1.0" encoding="UTF-8"?>
<xml>
  <records>
    <record>
      <source-app name="Horizon">Horizon</source-app>
      <rec-number>1</rec-number>
      <foreign-keys>
        <key app="Horizon" db-id="PAR00009313">1</key>
      </foreign-keys>
      <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="normal" font="default" size="100%">Ohnenstetter, D.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Giuliani, Gaston</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Fallick, A. E.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Rollion-Bard, C.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Robert, J. L.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Malisa, E. P.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Evidence of evaporites in the genesis of the vanadian grossular 'tsavorite' deposit in Namalulu, Tanzania</title>
        <secondary-title>Canadian Mineralogist</secondary-title>
      </titles>
      <pages>745-769</pages>
      <keywords>
        <keyword>Mozambique Belt</keyword>
        <keyword>Tanzania</keyword>
        <keyword>Namalulu</keyword>
        <keyword>tsavorite</keyword>
        <keyword>vanadian mineralization</keyword>
        <keyword>graphitic gneiss</keyword>
        <keyword>carbonates</keyword>
        <keyword>evaporites</keyword>
        <keyword>tainiolite</keyword>
      </keywords>
      <dates>
        <year>2012</year>
      </dates>
      <call-num>PAR00009313</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Canadian Mineralogist</full-title>
      </periodical>
      <isbn>0008-4476</isbn>
      <accession-num>ISI:000308799500011</accession-num>
      <number>3</number>
      <electronic-resource-num>10.3749/canmin.50.3.745</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/PAR00009313</url>
        </related-urls>
        <pdf-urls>
          <url>https://www.documentation.ird.fr/intranet/publi/depot/2021-03-11/010081636.pdf</url>
        </pdf-urls>
      </urls>
      <volume>50</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>The Namalulu tsavorite (vanadian grossular up to 0.80 wt.% V2O3) deposit in northeastern Tanzania occurs in metasomatized graphitic gneiss overlain by a dolomitic marble unit. These rocks belong to the Neoproterozoic metamorphic Mozambique Belt. The graphitic gneiss is composed of quartz, V-bearing kyanite (up to 0.4 wt.% V2O3), V-bearing muscovite (up to 1.0 wt.% V2O3), V-bearing rutile (up to 1.9 wt.% V2O3), and graphite. This rock is affected by calcic metasomatism precipitating calcite and mobilizing the elements for tsavorite crystallization in quartz-calcite veins. The dolomitic marble unit hosts an anhydrite-gypsum-dolomite lens (lens I) and a calcite-scapolite-diopside-sulfides-graphite lens (lens II). This last unit is characterized by the presence of F-bearing minerals (tremolite, phlogopite, tainiolite, titanite), with up to 9.4 wt.% F for tainiolite, and Ba-bearing minerals (feldspar, phlogopite), with up to 7.5 wt.% BaO for feldspar. Lithium (up to 2.0 wt.% Li2O) and boron (up to 110 ppm) are also present in tainiolite, as well as in F-bearing tremolite. This is the first description of metamorphic tainiolite. The protoliths of the Namalulu rocks correspond to organic-rich black shales, pure and magnesian carbonates, and evaporites. They were presumably deposited in a marine coastal sabkha located at the eastern margin of the Congo-Kalahari cratons bounded by the Mozambique Ocean during early Neoproterozoic. Tsavorite formed in the Ca-metasomatized gneiss during amphibolite facies retrograde metamorphism at 5.6-6.7 kbar and 630 +/- 30 degrees C.</abstract>
      <custom6>064</custom6>
      <custom1>UR234 / UR206</custom1>
      <custom7>Tanzanie</custom7>
    </record>
  </records>
</xml>
