Abstract
In Chapter 5 we stated the basic premise that the three-dimensional spatial distribution of petrophysical properties is controlled by the spatial distribution of geological processes, processes that can be separated into depositional and diagenetic. In Chapter 4 we discussed depositional processes and the relationship between the spatial distribution of depositional textures and petrophysical properties. Reservoir studies have made it abundantly clear that the petrophysical properties found in carbonate reservoirs are significantly different from those of Holocene carbonate sediments due to various diagenetic processes.
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