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Conferences & Meetings XIII All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium
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A metamorphic origin of the Guelb Moghrein Fe oxide-copper-gold-cobalt deposit, Mauritania

RMS-DPI code:  2008-1-101-1
Scientific session:  Fluid regime of hydrothermal ore-forming systems
Author listing:  Sakellaris G.A., Meyer F.M.
Principal author:  Sakellaris Gregori Aarne
Language:  English
Abstract - Summary 
(short description):
The Guelb Moghrein deposit is an Archean (~2.5 Ga) IOCG type deposit found within the supracrustal rocks of the Mauritanides fold-and-thrust belt, 260 km northeast of the capital city Nouakchott, near the Akjoujt town. The deposit is selectively developed in a carbonate-facies iron formation hosted by < 30 m wide tabular tectonic breccias along regional reverse shear zones. Siderite-magnetite-graphite and arsenide-sulfide-gold assemblages are found in equilibrium throughout the mineralized breccias and formed through metasomatic reactions at upper-greenschist facies metamorphic conditions (410 oC, 2-3 kbar). S, O, and D isotope analyses on key minerals suggest a metamorphic origin of the hydrothermal fluids.
 
Date of presentation:  23/09/2008
Time of presentation:  16-00
 
RMS-DPI code:  2008-1-101-1
Proceeedings volume 
in the RMS catalogue:
 
Proceedings of XIII International conference on thermobarogeochemistry and IVth APIFIS symposium. Volume 2.
Pages:  169-172
File of proceedings 
(PDF): 
 98 K
Status:  printed
Recieved:  17/03/2008
Accepted:  29/06/2008
Published on-line:  20/03/2009
Permanent address of publication:  http://www.minsoc.ru/2008-1-101-1/
Contact author(s):  Sakellaris, Gregori Aarne
 

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