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The Struganik limestone has been increasingly popular in recent years for   interior and exterior building applications, due to easy workability, low   cost and multi purpose suitability. The quality of limestone is determined by   its mineralogical and textural characteristics and physico-mechanical   properties. The Struganik stone corresponds to marl, clayey limestone and   limestone (micritic and allochemical). The limestone is commonly layered,   either thinly bedded or banked. Chert concretions are present in all   varieties. The Upper and the Lower Campanian age were deduced by the abundant   foraminifers. Micrite limestone is an autochthonous rock generated in a deep   marine environment, whereas allochemical limestone is related to a shallow   marine environment but subsequently brought into a deep-water system. The   mass quality of the Struganik limestone is controlled by variability of   lithology and layering. The values of physico-mechanical properties, such as   density, porosity, water absorption and strength, were statistically analyzed   and the obtained data were used to assess the rock quality in the quarry. The   relationship among the quantified properties is described by regression   analyses and the equations of the best-fit line. The Struganik limestone was   qualified by its petrological and engineering properties coupled with   statistical analysis. It satisfies the majority of the requirements of the   Main National Standard as a decorative stone, but with a limiting factor   regarding abrasive resistance

Petrophysical and mechanical properties of the Struganik limestone (Vardar zone, Western Serbia)