Multidisciplinary study of thorium mobility: formation of turkestanite and steacyite analogues, and structural insights using an XRD-directed microcrystal preparation technique. [PDF]
Stachowicz M +7 more
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Data from high-temperature and high-pressure carbon dioxide sequestration experiments limited to 24 hours, performed on Platinum Group Metals mine tailings from the South African Bushveld Igneous Complex. [PDF]
Nkosi ZH +5 more
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Applications of Nanotechnology in Ruminant Animal Production: Advances, Challenges, and Future Prospects. [PDF]
Kholif AE, Anele A, Chahine M, Anele UY.
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Shale-hosted vanadium occupation in typical silicate mineral structures. [PDF]
Fang-Yao H +6 more
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Impact of Natural Fermentation on Mineral Composition, Resistant and Non-Resistant Starches, Microbial Diversity, and Global Metabolite Profiles in Commercial Poi from Hawai'i. [PDF]
Stillwell N, Khadka VS, Nerurkar PV.
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PGE complexes at superliquidus temperature: Embryos for platinum-group minerals?
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Distribution of platinum-group minerals in ophiolitic chromitites
Applied Earth Science, 2009This paper reviews the distribution of platinum-group minerals in ophiolitic chromitites. Our data and literature data, obtained by in-situ investigation of polished sections and techniques of mechanical separation [hydroseparation (HS), or combining electric pulse disaggregation (EPD) plus HS], are contrasted.
José María González-Jiménez +4 more
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Characterizing and recovering the platinum group minerals––a review
Minerals Engineering, 2004Methods of characterizing and recovering the platinum group minerals are reviewed in this paper. First, a classification of platinum group minerals (PGMs) ore types is briefly introduced, followed by the introduction of some representative platinum group minerals.
Z. Xiao, A.R. Laplante
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Alluvial platinum‐group minerals from the Manampotsy area, East Madagascar
Australian Journal of Earth Sciences, 1992Two platinum‐group mineral (PGM) concentrates collected from the same placer in the Manampotsy area located 120 km southeast of Antananarivo, Madagascar, were studied. Nuggets, which ranged in size from 0.1 to 1 mm, were characteristically rounded but a complex aggregate was also observed. Except for the latter which was multiphase (composed of laurite,
Olivier Legendre, Thierry Augé
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