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Conferences & Meetings XIII All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium
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Fluid inclusions in calcites of metamorphic carbonatites of the Fuerteventura Island (Spain)

RMS-DPI code:  2008-1-62-0
Scientific session:  Fluids in metamorphic rocks
Author listing:  Shumilova T.G., Sokerina N.V.
Principal author:  T.G. Shumilova
Language:  Russian
Abstract - Summary 
(short description):
The results fluid inclusions study in calcites from magmatic carbonatites of the Fuerteventura Island (Canary Arhipelago, Spain) are presented. Quite a wide range of homogenization temperature of gas-liquid inclusions have been established, as much as from 170 to 410C for three different points, which is caused by non-equilibrium conditions of crystallization and postcrystallization formation processes of the carbonatites. The carbonatites of Montana Blanca region are characterized by the highest homogenization temperatures of 286C (average), which is essentially higher than those for carbonatites of Punta de la Nao and Punta Penon Blanca. The metamorphosed varieties of the carbonatites of Punta Penon Blanca have lower homogenization temperatures of fluid inclusions, as mush as average 254C.
 
Date of presentation:  23/09/2008
 
RMS-DPI code:  2008-1-62-0
Proceeedings volume 
in the RMS catalogue:
 
Proceedings of XIII International conference on thermobarogeochemistry and IVth APIFIS symposium. Volume 1.
Pages:  234-236
File of proceedings 
(PDF): 
 135 K
Status:  printed
Accepted:  28/06/2008
Published on-line:  12/02/2009
Permanent address of publication:  http://www.minsoc.ru/2008-1-62-0/
Contact author(s):  Sokerina, Natalya V.
 

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