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During the last few years, geological research at the southern slopes of   Fruška Gora Mt. enabled the discovery of different Miocene units (undivided   the Lower Miocene and Middle Miocene Badenian, predominantly). This is   primarily thinking of the so-called Leitha limestone (Middle Miocene,   Badenian), which is an important component in cement production (La Farge   Co., Beočin). The high carbonate content (more than 98 %) allows it to be a   very important raw material that is mixed with Pannonian marl in the process   of cement manufacture. Continuous exploitation of this rock at the Mutalj   Quarry enabled an insight into its structural, stratigraphic,   sedimentological and hydrogeological features, as well as its relation to the   other underlying/overlying units. Numerous fossils (i.e., red algae,   mollusks, corals, bryozoans, and foraminifers) and their biostratigraphic   range indicate to Middle Miocene Badenian age. Based on data from different   boreholes, structural and sedimentological characteristics, spatial   distribution, etc., a relatively large rock body was discovered (approx. 0.3   km2). Within these Leitha limestones, there are frequent cracks and caverns   infilled with fine lateritic clays and alevrites. These clays were sampled   for a paleomagnetic study. The carrier of the primary remanent magnetization   (RM) is magnetite that has a primary origin. Lateritic clays are   characterized by significant value of magnetic susceptibility. The degree of   anisotropy of the magnetic susceptibility (AMS) is low with the dominant   magnetic foliation

New data concerning the early middle miocene on the southern slopes of Fruska Gora (Northern Serbia): A case study from the Mutalj quarry