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Conferences & Meetings XIII All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium
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—onditions of hakmanite formation from pegmatites of the Lovozersky massif

RMS-DPI code:  2008-1-81-0
Scientific session:  Fluid regime of hydrothermal ore-forming systems
Author listing:  Kovalskaya T.N., Kotelnikova Z.A., Kotelnikov A.R., Suk N.I., Kovalsky A.M., Goettlicher J.
Principal author:  Kovalskaya Tatiana Nikolaevna
Language:  Russian
Abstract - Summary 
(short description):
The Lovozersky alkaline massif is located in the central part of the Kola peninsula and hosts giant deposits of rare and radioactive elements. Data of alkalinity of post−magmatic mineral−forming solutions is necessary for understanding mineral−forming processes in alkaline complexes. Sodalite (hakmanite) is a typical mineral of pegmatites of Lovozersky massif. In pegmatites near the Mt. Kanasurt we defined two types of hakmanites different in compositions. Fluid inclusions in hakmanite were investigated and a mass portion of NaCl in the fluid was determined. Formation temperatures of sodalite-bearing paragenesises were estimated to be below 450о—.
 
Date of presentation:  25/09/2008
Presentation Place:  IGEM RAS, Conference Hall
 
RMS-DPI code:  2008-1-81-0
Proceeedings volume 
in the RMS catalogue:
 
Proceedings of XIII International conference on thermobarogeochemistry and IVth APIFIS symposium. Volume 2.
Pages:  53-55
File of proceedings 
(PDF): 
 132 K
Status:  printed
Accepted:  29/06/2008
Published on-line:  19/02/2009
Permanent address of publication:  http://www.minsoc.ru/2008-1-81-0/
Contact author(s):  Kovalskaya, Tatiana Nikolaevna
 
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