ITEM METADATA RECORD
Title: Recognition and significance of multiple fluid inclusion generations in telogenetic calcites
Authors: Muchez, Philippe ×
Slobodnik, M #
Issue Date: Oct-1996
Publisher: Mineralogical society
Series Title: Mineralogical magazine vol:60 issue:402 pages:813-819
Abstract: Ferroan and non-ferroan calcites occur in fractures in the Lower Carboniferous of the Variscan foreland of southern Belgium. These fractures post-date the Variscan orogeny and the calcites have a telogenetic origin. The non-ferroan calcites formed by recrystallization of the ferroan calcites. Two types of monophase aqueous fluid inclusions are present in the ferroan calcite cement. Although both types of inclusions formed at a temperature not exceeding 50 degrees C, one type contains a moderately saline fluid (3.6-16.3 eq. wt.% NaCl) and the other type fresh water (Tm ice = 0 degrees C). The fluid inclusions in the non-ferroan calcite also contain fresh water.
ISSN: 0026-461X
Publication status: published
KU Leuven publication type: IT
Appears in Collections:Division of Geology
× corresponding author
# (joint) last author

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