80 Sediments (Posters)
Wednesday, 20 March 2013
8:00 AM - 12:00 PM
Grand Ballroom South
PETROPHYSICAL EVALUATION OF THE CAMBRO-ORDOVICIAN STRATA OF CENTRAL NEW YORK
Paper number: 80-9
Program: Technical Sessions
Time: 8:00 AM – 12:00 PM
Authors
Abstract
A diagenetic sequence of dolomitization,dedolmitization, silicification, and stylolitization was detected using Nuclide Luminoscope.
Petrophysical parameters and reservoir quality were determined using mercury prosimetric technique. Selected samples were injected with mercury at a high pressure up to 25, 000 psi (pounds per square inch). This high pressure forces mercury to penetrate pores with diameters that range from 900 to 0.04 microns. The pore system of the studied samples was classified by using a high resolution petrographic microscope.
Diagenetic processes have affected the petrophysical parameters including porosity, permeability, fluid saturation, and recovery efficiency.