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Castroviejo Bolibar, Ricardo and Yparraguirre, José Andrés and Chacón, E. (2007). Lithogeochemistry and fluid flow in the epithermal Veta Rublo base metal-silver deposit, Chonta Mine (Huancavelica, Perú). In: "23rd IAGS 2007", 14-19 Junio 2007, Oviedo. ISBN 978-84-690-6461-0.
Title: | Lithogeochemistry and fluid flow in the epithermal Veta Rublo base metal-silver deposit, Chonta Mine (Huancavelica, Perú) |
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Author/s: |
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Item Type: | Presentation at Congress or Conference (Other) |
Event Title: | 23rd IAGS 2007 |
Event Dates: | 14-19 Junio 2007 |
Event Location: | Oviedo |
Title of Book: | 23rd IAGS 2007 (International Applied Geochemistry Symposium):Exploring our environment |
Date: | 2007 |
ISBN: | 978-84-690-6461-0 |
Subjects: | |
Faculty: | E.T.S.I. Minas (UPM) |
Department: | Ingeniería Geológica [hasta 2014] |
Creative Commons Licenses: | Recognition - No derivative works - Non commercial |
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The Chonta Mine (75º00’30” W & 13º04’30”S, 4495 to 5000 m absl), owned by Compañía Minera Caudalosa, operates a polymetallic Zn-Pb-Cu-Ag vein system of the low sulphidation epithermal type, hosted by cenozoic volcanics of dacitic to andesitic composition (Domos de Lava Formation). Veta Rublo, one of the main veins of the system, is worked underground to nearly 300 m. It strikes 60-80º NE and dips 60-70º SE; its width varies between 0.30 and 2.20m, and it crops out along 1 km, but is continued along strike by other veins, as Veta Caudalosa, for some 5 km. Typical metal contents are 7% Zn, 5% Pb, 0.4% Cu and 3 oz/t Ag, with quartz, sericite, sphalerite, galena, pyrite, chalcopyrite, fahlore as main minerals, and minor carbonate and sulphosalts.
Item ID: | 10967 |
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DC Identifier: | https://oa.upm.es/10967/ |
OAI Identifier: | oai:oa.upm.es:10967 |
Official URL: | http://www.appliedgeochemists.org/events/iags2007/... |
Deposited by: | Biblioteca ETSI Minas y Energía |
Deposited on: | 04 Jun 2012 08:15 |
Last Modified: | 20 Apr 2016 19:09 |