Journal Title
Title of Journal: Miner Deposita
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Abbravation: Mineralium Deposita
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Publisher
Springer Berlin Heidelberg
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Authors: David L Huston
Publish Date: 2014/09/04
Volume: 49, Issue: 8, Pages: 885-887
Abstract
Over the last decade or so the development of technologies associated with consumer electronics renewable energy and specialty steel have sparked demand for a range of “specialty” mineral commodities These commodities are quite diverse and include among others rare earth elements REEs lanthanides Y and Sc Ga In W platinum group elements PGEs Ru Rh Pd Os Ir Pt Co Nb Mg Mo Sb Li V Ni Ta Te Cr Mn Se Ti Sr graphite Sn Ge Be Zr Bi F and Cd Most of these commodities have small restricted markets and in some cases supply is restricted—concentrated in either a small group of countries or producing companies Some elements such as In Ga Cd Se and Te are produced as byproducts of the extraction of base metals
Keywords:
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Other Papers In This Journal:
- Some primary structures in the chromitites of Orissa, India
- Vein graphite deposits: geological settings, origin, and economic significance
- Marymia: an Archean, amphibolite facies-hosted, orogenic lode-gold deposit overprinted by Palaeoproterozoic orogenesis and base metal mineralisation, Western Australia
- The Nolans Bore rare-earth element-phosphorus-uranium mineral system: geology, origin and post-depositional modifications
- New isotopic evidence bearing on bonanza (Au-Ag) epithermal ore-forming processes
- The jacupirangite at Kodal, Vestfold, Norway
- 40 Ar/ 39 Ar and K–Ar geochronology of magmatic and hydrothermal events in a classic low-suphidation epithermal bonanza deposit: El Peñon, northern Chile
- Hypogene Zn carbonate ores in the Angouran deposit, NW Iran
- Major Brazilian gold deposits – 1982 to 1999
- Nd-Sr-Pb isotopic constraints on metal and fluid sources in W-Sb-Au mineralization at Woxi and Liaojiaping (Western Hunan, China)
- High-grade iron ore at Windarling, Yilgarn Craton: a product of syn-orogenic deformation, hypogene hydrothermal alteration and supergene modification in an Archean BIF-basalt lithostratigraphy
- A comparison of progressive hydrothermal carbonate alteration in Archean metabasalts and metaperidotites
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