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Published on Jan 1, 2015in Economic Geology 3.29
Wei Jian2
Estimated H-index: 2
(Clausthal University of Technology),
Bernd Lehmann33
Estimated H-index: 33
(Clausthal University of Technology)
+ 6 AuthorsJiangwei Feng2
Estimated H-index: 2
The Dahu Au-Mo deposit is located in the Xiaoqinling region and belongs to the Qinling-Dabie orogen of central China. The quartz vein-style Dahu Au-Mo deposit (31 t Au, average grade: 4.7 g/t; 30,000 t Mo, average grade: 0.13 %) formed in four stages, i.e., an early quartz-K-feldspar stage (I), a pyrite-molybdenite stage (II), a sulfide-telluride-sulfosalt-gold stage (III), and a late carbonate-barite stage (IV). Abundant tellurides and sulfosalts occur in stage III: altaite, tellurobismuthite, ...
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Published on Nov 1, 2011in Mineralogy and Petrology 1.66
Panagiotis Voudouris13
Estimated H-index: 13
(National and Kapodistrian University of Athens),
Vasilios Melfos12
Estimated H-index: 12
(Aristotle University of Thessaloniki)
+ 3 AuthorsGeorge Falalakis1
Estimated H-index: 1
The Perama Hill deposit is a high-sulfidation Au-Ag-Te-Se epithermal system hosted in silicic- and argillic altered andesitic rocks and overlying sandstones, which were emplaced on the eastern margin of the Petrota graben, northeastern Greece. The deposit evolved from an early stage silica-pyrite rock and argillic alteration followed by the deposition of sulfide-, sulfosalt- and telluride-bearing quartz-barite veins and stockworks. Early ore formation is characterized by a high-sulfidation-type ...
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Published on Jul 1, 2006in Mineralogy and Petrology 1.66
O. Yu. Plotinskaya6
Estimated H-index: 6
,
V.A. Kovalenker5
Estimated H-index: 5
+ 1 AuthorsC. J. Stanley20
Estimated H-index: 20
(American Museum of Natural History)
The Late Paleozoic Kochbulak and Kairagach deposits are located on the northern slope of the Kurama Ridge, Middle Tien Shan, in the same volcanic structure and the same ore-forming system. Au–Ag–Cu–Bi–Te–Se mineralization is confined to veins and dissemination zones accompanied by quartz-sericite wall-rock alteration. The tellurides, calaverite, altaite, hessite, and tetradymite are widespread at both deposits; at Kairagach selenides and sulfoselenides of Bi and Pb are common, while at Kochbulak...
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