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Conferences & Meetings XIII All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium
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Rodingites within scattered ophiolitic occurrences from the northern and eastern Othris area, Greece

RMS-DPI code:  2008-1-52-1
Scientific session:  Fluids in metamorphic rocks
Author listing:  Koutsovitis P.N., Magganas A., Pomonis P.
Principal author:  Petros N. Koutsovitis
Language:  English
Abstract - Summary 
(short description):
Rodingites appear throughout the Othris area within ophiolitic rocks and mélange formation. They have formed by interaction of H2O-rich fluids with gabbroic rocks and dolerites during serpentinization of the surrounding rocks. These metasomatic fluids caused depletion of Si, Na, K and enrichment in Ca. Observed mobility of Zr, Y and Cr is possibly due to infiltration processes. Rodingites present lower ΣREE than their protoliths but subparallel REE patterns. Mineral assemblages of most rodingites are consistent with formation from low-T fluids, whereas the presence of vesuvianite in few samples implies that fluid temperatures reached higher levels or there was significant CO2 loss.
 
Date of presentation:  24/09/2008
Time of presentation:  16:00
 
RMS-DPI code:  2008-1-52-1
Proceeedings volume 
in the RMS catalogue:
 
Proceedings of XIII International conference on thermobarogeochemistry and IVth APIFIS symposium. Volume 1.
Pages:  243-246
File of proceedings 
(PDF): 
 238 K
Status:  printed
Recieved:  16/03/2008
Accepted:  29/06/2008
Published on-line:  13/02/2009
Permanent address of publication:  http://www.minsoc.ru/2008-1-52-1/
Contact author(s):  Koutsovitis, Petros N.
 

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