Testing the Multi Point Statistic Modelling Approach Using Outcrop Data

The island of Favignana provides an exceptional three-dimensional insight of the internal architecture of a Lower Pleistocene complex bioclastic calcarenitic wedge. Field data indicate that these calcarenites consist of foramol association, originated during cool to temperate water conditions in a high-energy, storm dominated, open shelf environment. Predominant sedimentary structures vary from small-scale trough cross bedding, large foresets to large scours filled by structureless massive bioclastic material. Overall a main transport direction to the SE indicates the prograding nature of these deposits. Based on the sedimentological characteristics and reservoir properties, this sedimentary complex is believed to be a relevant analogue for several important hydrocarbon fields worldwide in North Africa, Middle East and South America such as the Perla Field in Venezuela.