<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Evidence of evaporites in the genesis of the vanadian grossular 'tsavorite' deposit in Namalulu, Tanzania</dc:title>
  <dc:creator>Feneyrol, J.</dc:creator>
  <dc:creator>Ohnenstetter, D.</dc:creator>
  <dc:creator>/Giuliani, Gaston</dc:creator>
  <dc:creator>Fallick, A. E.</dc:creator>
  <dc:creator>Rollion-Bard, C.</dc:creator>
  <dc:creator>Robert, J. L.</dc:creator>
  <dc:creator>Malisa, E. P.</dc:creator>
  <dc:subject>Mozambique Belt</dc:subject>
  <dc:subject>Tanzania</dc:subject>
  <dc:subject>Namalulu</dc:subject>
  <dc:subject>tsavorite</dc:subject>
  <dc:subject>vanadian mineralization</dc:subject>
  <dc:subject>graphitic gneiss</dc:subject>
  <dc:subject>carbonates</dc:subject>
  <dc:subject>evaporites</dc:subject>
  <dc:subject>tainiolite</dc:subject>
  <dc:description>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.</dc:description>
  <dc:date>2012</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/PAR00009313</dc:identifier>
  <dc:identifier>PAR00009313</dc:identifier>
  <dc:identifier>Feneyrol J., Ohnenstetter D., Giuliani Gaston, Fallick A. E., Rollion-Bard C., Robert J. L., Malisa E. P.. Evidence of evaporites in the genesis of the vanadian grossular 'tsavorite' deposit in Namalulu, Tanzania. 2012, 50 (3),  745-769</dc:identifier>
  <dc:language>EN</dc:language>
</oai_dc:dc>
