Abstract
The Kalguta deposit is a typical representative of the molybdenum-rare metal-tungsten ore association that is widespread in Gornyi Altai. The deposit is confined to the late Hercynian Kalguta Massif of leucocratic rare metal granites that intrude Devonian acid volcanic rocks. Ore mineralization is developed as a series of steep wolframite-molybdenite-quartz veins with chalcopyrite, bismuthinite, and beryl. The vertical mineralization amplitude is more than 500 m. Graphite makes up a single association with quartz and sulfides (chalcopyrite, pyrite, bismuthinite, and Bitennantite) in late mineral associations of the major ore formation stage. The results obtained testify to an active participation of carbon in ore formation. The carbon was probably derived from deep-seated reduced metalliferous fluids.
| Original language | English |
|---|---|
| Pages (from-to) | 1169-1171 |
| Number of pages | 3 |
| Journal | Doklady Earth Sciences |
| Volume | 399 |
| Issue number | 8 |
| Publication status | Published - Oct 2004 |
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ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Earth and Planetary Sciences (miscellaneous)
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Graphites from the Kalguta rare metal greisen deposit (Gornyi Altai). / Potseluev, A. A.; Kotegov, V. I.; Akimtsev, V. A.
In: Doklady Earth Sciences, Vol. 399, No. 8, 10.2004, p. 1169-1171.Research output: Contribution to journal › Article
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TY - JOUR
T1 - Graphites from the Kalguta rare metal greisen deposit (Gornyi Altai)
AU - Potseluev, A. A.
AU - Kotegov, V. I.
AU - Akimtsev, V. A.
PY - 2004/10
Y1 - 2004/10
N2 - The Kalguta deposit is a typical representative of the molybdenum-rare metal-tungsten ore association that is widespread in Gornyi Altai. The deposit is confined to the late Hercynian Kalguta Massif of leucocratic rare metal granites that intrude Devonian acid volcanic rocks. Ore mineralization is developed as a series of steep wolframite-molybdenite-quartz veins with chalcopyrite, bismuthinite, and beryl. The vertical mineralization amplitude is more than 500 m. Graphite makes up a single association with quartz and sulfides (chalcopyrite, pyrite, bismuthinite, and Bitennantite) in late mineral associations of the major ore formation stage. The results obtained testify to an active participation of carbon in ore formation. The carbon was probably derived from deep-seated reduced metalliferous fluids.
AB - The Kalguta deposit is a typical representative of the molybdenum-rare metal-tungsten ore association that is widespread in Gornyi Altai. The deposit is confined to the late Hercynian Kalguta Massif of leucocratic rare metal granites that intrude Devonian acid volcanic rocks. Ore mineralization is developed as a series of steep wolframite-molybdenite-quartz veins with chalcopyrite, bismuthinite, and beryl. The vertical mineralization amplitude is more than 500 m. Graphite makes up a single association with quartz and sulfides (chalcopyrite, pyrite, bismuthinite, and Bitennantite) in late mineral associations of the major ore formation stage. The results obtained testify to an active participation of carbon in ore formation. The carbon was probably derived from deep-seated reduced metalliferous fluids.
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UR - http://www.scopus.com/inward/citedby.url?scp=10844268070&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:10844268070
VL - 399
SP - 1169
EP - 1171
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 8
ER -