Research output: Contribution to journal › Article › peer-review
High-temperature gold-copper extraction with chloride flux in lava tubes of Tolbachik volcano (Kamchatka). / Kamenetsky, Vadim S.; Belousov, Alexander; Sharygin, Victor V. et al.
In: Terra Nova, Vol. 31, No. 6, 01.12.2019, p. 511-517.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - High-temperature gold-copper extraction with chloride flux in lava tubes of Tolbachik volcano (Kamchatka)
AU - Kamenetsky, Vadim S.
AU - Belousov, Alexander
AU - Sharygin, Victor V.
AU - Zhitova, Liudmila M.
AU - Ehrig, Kathy
AU - Zelenski, Michael E.
AU - Chaplygin, Ilya
AU - Yudovskaya, Marina A.
AU - Nesterenko, Pavel N.
AU - Zakharov, Sergey M.
N1 - Publisher Copyright: © 2019 John Wiley & Sons Ltd
PY - 2019/12/1
Y1 - 2019/12/1
N2 - Subvolcanic environments in supra-subduction zones are renowned for hosting epithermal deposits that often contain electrum and native gold, including bonanza examples. This study examined mineral assemblages and processes occurring in shallow-crust volcanic settings using recent eruption (2012–2013) of the basaltic Tolbachik volcano in the Kamchatka arc. The Tolbachik eruptive system is characterized by an extensive system of lava tubes. After cessation of magma input, the tubes maintained the flow of hot oxidized gases that episodically interacted with the lava surfaces and sulphate-chloride precipitates from volcanic gases on these surfaces. The gas-rock interaction had strong pyrometamorphic effects that resulted in the formation of molten salt, oxidized (tenorite, hematite, Cu-rich magnesioferrite) and skarn-like silicate mineral assemblages. By analogy with experimental studies, we propose that a combination of these processes was responsible for extraction of metals from the basaltic wall rocks and deposition of Cu-, Fe- and Cu-Fe-oxides and native gold.
AB - Subvolcanic environments in supra-subduction zones are renowned for hosting epithermal deposits that often contain electrum and native gold, including bonanza examples. This study examined mineral assemblages and processes occurring in shallow-crust volcanic settings using recent eruption (2012–2013) of the basaltic Tolbachik volcano in the Kamchatka arc. The Tolbachik eruptive system is characterized by an extensive system of lava tubes. After cessation of magma input, the tubes maintained the flow of hot oxidized gases that episodically interacted with the lava surfaces and sulphate-chloride precipitates from volcanic gases on these surfaces. The gas-rock interaction had strong pyrometamorphic effects that resulted in the formation of molten salt, oxidized (tenorite, hematite, Cu-rich magnesioferrite) and skarn-like silicate mineral assemblages. By analogy with experimental studies, we propose that a combination of these processes was responsible for extraction of metals from the basaltic wall rocks and deposition of Cu-, Fe- and Cu-Fe-oxides and native gold.
KW - SLEEPER DEPOSIT
KW - NATIVE GOLD
KW - KUDRYAVY VOLCANO
KW - ENRICHMENT
KW - TRANSPORT
KW - ERUPTION
KW - SILICA
KW - EMISSIONS
KW - SYSTEMS
KW - METALS
UR - http://www.scopus.com/inward/record.url?scp=85070113070&partnerID=8YFLogxK
U2 - 10.1111/ter.12420
DO - 10.1111/ter.12420
M3 - Article
AN - SCOPUS:85070113070
VL - 31
SP - 511
EP - 517
JO - Terra Nova
JF - Terra Nova
SN - 0954-4879
IS - 6
ER -
ID: 21146299