Mixing of magmatic brines and meteoric fluids in the Vysokogorskoe tin-porphyry deposit (Primorye, Russia)

This study substantiates the magmatic nature of a highly concentrated mineral forming fluid, which formed tin ores of the Vysokogorskoe cassiteritesili catesulfide deposit as a typical representative of tin deposits from the Kavalerovskii ore region in Primorye.

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Veröffentlicht in:Doklady earth sciences 2013-12, Vol.453 (2), p.1218-1222
Hauptverfasser: Bortnikov, N. S., Kryazhev, S. G., Gonevchuk, V. G., Gorelikova, N. V., Ryabchenko, V. M., Balashov, F. V.
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container_end_page 1222
container_issue 2
container_start_page 1218
container_title Doklady earth sciences
container_volume 453
creator Bortnikov, N. S.
Kryazhev, S. G.
Gonevchuk, V. G.
Gorelikova, N. V.
Ryabchenko, V. M.
Balashov, F. V.
description This study substantiates the magmatic nature of a highly concentrated mineral forming fluid, which formed tin ores of the Vysokogorskoe cassiteritesili catesulfide deposit as a typical representative of tin deposits from the Kavalerovskii ore region in Primorye.
doi_str_mv 10.1134/S1028334X13120039
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subjects Breccia
Earth and Environmental Science
Earth Sciences
Fluids
Geochemistry
Magma
Magmatism
Minerals
Porphyry
Silicates
Sulfides
Tin
title Mixing of magmatic brines and meteoric fluids in the Vysokogorskoe tin-porphyry deposit (Primorye, Russia)
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