oa Porosity controls in Peritethyan Carbonate Reservoirs

It is commonly considered that reservoir properties of Peritethyan carbonates mostly originated<br>from intense dissolution (vugs, molds, enlarged fractures, caverns) in a variety meteoric<br>diagenetic environments. This dissolution took place prior to the burial by non-reservoir or seal<br>units, under unconformities of different orders of magnitude or in shallow, near-surface aquifers.<br>Primary depositional porosities are seen as extensively obliterated by cementation and<br>compaction.