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GeoRef Categories
Era and Period
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Book Series
Date
Availability
Bambolla Mine
Cervelleite, Ag 4 TeS, a new mineral from the Bambolla Mine, Mexico, and a description of a photo-chemical reaction involving cervelleite, acanthite and hessite Available to Purchase
The new mineral tomiolloite, Al 12 (Te 4+ O 3 ) 5 [(SO 3 ) 0.5 (SO 4 ) 0.5 ](OH) 24 : A unique microporous tellurite structure Available to Purchase
New structural data reveal benleonardite to be a member of the pearceite-polybasite group Available to Purchase
New find of silver tellurosulphides from the Funan gold deposit, East Shandong, China Available to Purchase
ALAN J. CRIDDLE DSc 1944–2002: Memorial Notice Available to Purchase
Memorial of Benjamin F. Leonard III, 1921–2008 Available to Purchase
New Mineral Names Free
New minerals and nomenclature modifications approved in 2016 and 2017 Open Access
New Minerals and Nomenclature Modifications Approved in 2016 and 2017 Open Access
THE CRYSTAL STRUCTURE OF SKIPPENITE, Bi 2 Se 2 Te, FROM THE KOCHKAR DEPOSIT, SOUTHERN URALS, RUSSIAN FEDERATION Available to Purchase
Newsletter 62 Available to Purchase
JONASSONITE, Au(Bi,Pb) 5 S 4 , A NEW MINERAL SPECIES FROM NAGYBÖRZSÖNY, HUNGARY Available to Purchase
Xocolatlite, Ca 2 Mn 2 4+ Te 2 O 12 ·H 2 O, a new tellurate related to kuranakhite: Description and measurement of Te oxidation state by XANES spectroscopy Available to Purchase
On the symmetry and crystal structure of aguilarite, Ag 4 SeS Available to Purchase
Argentopolybasite, Ag 16 Sb 2 S 11 , a new member of the polybasite group Open Access
Crystal structure and revised chemical formula for burckhardtite, Pb 2 (Fe 3+ Te 6+ )[AlSi 3 O 8 ]O 6 : a double-sheet silicate with intercalated phyllotellurate layers Available to Purchase
The crystal structures of the mixed-valence tellurium oxysalts tlapallite, (Ca,Pb) 3 CaCu 6 [Te 4+ 3 Te 6+ O 12 ] 2 (Te 4+ O 3 ) 2 (SO 4 ) 2 ·3H 2 O, and carlfriesite, CaTe 4+ 2 Te 6+ O 8 Available to Purchase
New minerals auropolybasite, [Ag 15 AuSb 2 S 11 ] and auropearceite, [Ag 15 AuAs 2 S 11 ], and the implications for the formation of bonanza ores in epithermal systems Free
The tetrahedrite group: Nomenclature and classification Available to Purchase
Critical Elements in Carlin, Epithermal, and Orogenic Gold Deposits Available to Purchase
Abstract Carlin, epithermal, and orogenic gold deposits, today mined almost exclusively for their gold content, have similar suites of anomalous trace elements that reflect similar low-salinity ore fluids and thermal conditions of metal transport and deposition. Many of these trace elements are commonly referred to as critical or near-critical elements or metals and have been locally recovered, although typically in small amounts, by historic mining activities. These elements include As, Bi, Hg, In, Sb, Se, Te, Tl, and W. Most of these elements are now solely recovered as by-products from the milling of large-tonnage, base metal-rich ore deposits, such as porphyry and volcanogenic massive sulfide deposits. A combination of dominance of the world market by a single country for a single commodity and a growing demand for many of the critical to near-critical elements could lead to future recovery of such elements from select epithermal, orogenic, or Carlin-type gold deposits. Antimony continues to be recovered from some orogenic gold deposits and tellurium could potentially be a primary commodity from some such deposits. Tellurium and indium in sphalerite-rich ores have been recovered in the past and could be future commodities recovered from epithermal ores. Carlin-type gold deposits in Nevada are enriched in and may be a future source for As, Hg, Sb, and/or Tl. Some of the Devonian carbonaceous host rocks in the Carlin districts are sufficiently enriched in many trace elements, including Hg, Se, and V, such that they also could become resources. Thallium may be locally enriched to economic levels in Carlin-type deposits and it has been produced from Carlin-like deposits elsewhere in the world (e.g., Alsar, southern Macedonia; Lanmuchang, Guizhou province, China). Mercury continues to be recovered from shallow-level epithermal deposits, as well as a by-product of many Carlin-type deposits where refractory ore is roasted to oxidize carbon and pyrite, and mercury is then captured in air pollution control devices.