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Evidence of magmatic origine of the fluids responsible for cassiterite-solocate-sulfide Solnechnoye deposit (Russian Far East)

RMS-DPI code:  E2-2009-4-0
Scientific session:  Commission on Ore Mineralogy seminar, IGEM RAS
Author listing:  Bortnikov N.S., Krylova T.L., Gorelikova N.V., Korostelev P.G.
Principal author:  Bortnikov N.S., Krylova T.L., Gorelikova N.V.
Language:  Russian
Abstract - Summary 
(short description):
Fluid inclusions in minerals representing the Molybdenum and the Tin stages of the cassiterite-silicate-sulfide Solnechnoye deposit (Russian Far East) havw been investigated by thermo- and criometry, Raman spectroscopy, and crash-leaching ICP-MS for trace elements. The data obtained proved the difference between molybdenum and tin forming fluids. Features and characteristics of the fluids deposited Mo-bearing and Sn ores of the deposits deep levels points to their magmatic origin. remarkable difference in alkalies ratios in fluid inclusions in quartz from Mo- and Sn stages, along with the difference in temperature and salinity gradients assumes that the formation of these two stages is related to different phases of the Silinsky monzonitoid massif.
 
Date of presentation:  12/11/2009
Presentation Place:  IGEM RAS, White Hall
 
RMS-DPI code:  E2-2009-4-0
File of proceedings 
(PDF): 
 646 K
Status:  xPrint
Accepted:  05/11/2009
Published on-line:  07/12/2009
Permanent address of publication:  http://www.minsoc.ru/E2-2009-4-0/
Contact author(s):  Plotinskaya, Olga Yurievna
 

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