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               <dc:title>Quantitative Mineralogical Comparison between HPGR and Ball Mill Products of a Sn-Ta Ore</dc:title>
               <dc:creator>Ahmad Hamid, Sarbast</dc:creator>
               <dc:creator>Alfonso Abella, María Pura</dc:creator>
               <dc:creator>Anticoi, Hernan</dc:creator>
               <dc:creator>Guasch, Eduard</dc:creator>
               <dc:creator>Oliva, Josep</dc:creator>
               <dc:creator>Dosbaba, Marek</dc:creator>
               <dc:creator>Garcia Vallès, Maite</dc:creator>
               <dc:creator>Chugunova, Marina</dc:creator>
               <dc:subject>Mineralogia</dc:subject>
               <dc:subject>Jaciments minerals</dc:subject>
               <dc:subject>Mineralogy</dc:subject>
               <dc:subject>Mineral deposits</dc:subject>
               <dc:description>The mineralogy and liberation characteristics of the comminuted Penouta leucogranite host of the Sn-Ta ore were determined. Grinding developed by a combination of high-pressure grinding rolls (HPGR) followed by a ball mill (BM) was compared with a single ball mill process. The mineral characteristics of the grinding products were analyzed using a Tescan Integrated Mineralogical Analyzer (TIMA-X) and X-ray powder diffraction (XRD). The ore contains 103 ppm of Ta and is mainly composed of quartz, albite, microcline, muscovite, and kaolinite. Nb, Ta-rich minerals are columbite-(Mn) and tantalite-(Mn), as well as minor microlite and wodginite. The liberation in the product is high in the size fraction of less than 250 m (51-52 wt % for columbite-group minerals (CGM) and 74-80 wt % for cassiterite) and reduced in larger particles (8.8-17 wt % for CGM and 28-37 wt % for cassiterite). The recovery in the 􀀀250 m fraction was high, while in the larger fraction it is limited, remaining up to 80 ppm in some tailings. The combined use of HPGR and a BM reduces the particle size distribution of the product and, thus, increases the liberation of the ores. Smaller fractions can be treated directly using gravity methods; however, particles of a size greater than +250 m should be ground more.</dc:description>
               <dc:date>2018-06-15T09:15:20Z</dc:date>
               <dc:date>2018-06-15T09:15:20Z</dc:date>
               <dc:date>2018-04-11</dc:date>
               <dc:date>2018-06-15T09:15:20Z</dc:date>
               <dc:type>info:eu-repo/semantics/article</dc:type>
               <dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
               <dc:relation>Reproducció del document publicat a: https://doi.org/10.3390/min8040151</dc:relation>
               <dc:relation>Minerals, 2018, vol. 8, num. 4, p. 151</dc:relation>
               <dc:relation>https://doi.org/10.3390/min8040151</dc:relation>
               <dc:relation>info:eu-repo/grantAgreement/EC/H2020/642201/EU//OptimOre</dc:relation>
               <dc:rights>cc-by (c) Ahmad Hamid, S. et al., 2018</dc:rights>
               <dc:rights>http://creativecommons.org/licenses/by/3.0/es</dc:rights>
               <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
               <dc:publisher>MDPI</dc:publisher>
               <dc:source>Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)</dc:source>
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