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Conferences & Meetings XIII All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium
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Physical-chemical conditions and geneses of gold mineralization in Karelia (Russia)

RMS-DPI code:  2008-1-65-0
Scientific session:  IGCP-540 session УFluids of orogenic Au depositsФ
Author listing:  Alekseyev V.Yu., Prokofiev V.Yu., Volkov A.V.
Principal author:  Alekseyev Victor Yurevich
Language:  Russian
Abstract - Summary 
(short description):
Summary. Fluid inclusions in quarts from Taloveis and Pedrolampy gold deposits have been studied. The primary inclusions of the Taloveis deposit have homogenization temperatures of about 347˚C and salinities of 12,4-11,7 wt % NaCl equiv. Secondary inclusions have lower homogenization temperatures 250 to 196 ˚C and salinities of 1.1 to 6.2 wt % NaCl equiv. According to fluid inclusions data, early mineralization at the Pedrolampy deposit took place at 486˚C and a salinity of 59,4 wt % NaCl equiv. Fluid inclusions of the later stage were more diluted (6,3 wt % NaCl equiv) and had lower homogenization temperature of 320-257˚C. The observed deposits presumably belong to a granite-related type.
 
Date of presentation:  23/09/2008
 
RMS-DPI code:  2008-1-65-0
Proceeedings volume 
in the RMS catalogue:
 
Proceedings of XIII International conference on thermobarogeochemistry and IVth APIFIS symposium. Volume 2.
Pages:  177-180
File of proceedings 
(PDF): 
 126 K
Status:  printed
Accepted:  29/06/2008
Published on-line:  30/03/2009
Permanent address of publication:  http://www.minsoc.ru/2008-1-65-0/
Contact author(s):  Alekseyev, Victor Yurevich
 
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