Russian Mineralogical Society
XIII All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium
Hydrothermal fluid evolution in the fracture network of the Baksa Gneiss Complex, Pannonian Basin, Hungary

RMS-DPI code:  2008-1-59-1
Scientific session:  Fluids in metamorphic rocks
Author listing:  Fintor K., Schubert F., Tóth T.M.
Principal author:  Fintor Krisztian
Language:  English
Abstract - Summary 
(short description):
The Baksa Gneiss Complex is a polymetamorphic basement complex located in the southwestern part of the Pannonian Basin. It is mostly built by metapelites, amphibolites and marbles, penetrated by aplite dikes. Post metamorphic fractures are filled in with an epi+di+ab+kfp+chl+pyr+qtz+cc mineral paragenesis. Two dominant paleofluid types can be distinguished in the epidote, diopside and calcite crystals based on their fluid inclusions. The earlier one is characterized by low salinity (0.2-6.5 w% NaCl eqv.) and high temperature (Th: 127-362 C) and relates to hydrothermal propilitc alteration. Primary and pseudosecondary incusions of the high salinity (18.2-26.5 w% NaCl eqv.) and low temperature (Th: 70-132 C) late fluid indicate mixing of hydrothermal fluid with highly saline basinal brines.
Date of presentation:  23/09/2008
Time of presentation:  16-00
RMS-DPI code:  2008-1-59-1
Proceeedings volume 
in the RMS catalogue:
Proceedings of XIII International conference on thermobarogeochemistry and IVth APIFIS symposium. Volume 1.
Pages:  241-242
File of proceedings 
 74 K
Status:  printed
Recieved:  12/03/2008
Accepted:  28/06/2008
Published on-line:  12/02/2009
Permanent address of publication:
Contact author(s):  Fintor, Krisztian

Copyright © Russian Mineralogical Society, 1995-2011. All rights reserved.
printed on 30/10/2020