Jc. Lacharpagne, CLAY DIAGENESIS IN RESERVOIRS - THE IMPOR TANCE AND EFFECTS ON POROSITY AND PERMEABILITY IN EXPLORATION-PRODUCTION, Bulletin des centres de recherches exploration-production Elf-Aquitaine, 19(1), 1995, pp. 81-90
The main goal in inorganic geochemistry applied to oil exploration and
production is to describe every fact participating in the poroperm ev
olution oi reservoir formation during burial. Therefore, authigenic an
d detrital minerals are studied, as well as reservoir waters. Followin
g a relatively short period of mechanical compaction, porosity and per
meability characteristics are influenced by cement crystallization and
dissolution, and clay material growth. Porosity is dominantly affecte
d by cement type behaviour, while permeability is controlled by the ch
aracteristic Variations oi clays. In a classical diagenetic study, the
first step is to constrain the temperature time evolution. Diagenetic
steps are then reported to the burial curve, and consequences of each
phenomena on petrophysical properties are estimated. Clay material is
used to determine the absolute age of crystallization, partly to iden
tify the characteristics of crystallization associated waters, and the
refore to provide a background for the interpretation of the effects o
f diagenesis in Exploration-Production. Theoretical considerations are
in constant progress, and directly influence critical domaines of int
erpretation (dating, modellization). So, close relations between inter
preter and research groups are most recommended.