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This work presents major lithological, structural, paleontological and  paleomagnetic characteristics of the Upper Miocene Pannonian marl in the  Filijala Open Pit of the La Farge Cement Plant near Beočin, northern Serbia.  Pannonian marl lies between the underlying heterogeneous Sarmatian deposits  and the overlying set of Pontian sand beds and Quaternary sediments. The open  pit is located on the NE range of Fruška Gora, a horst structure with a core  of Paleozoic, Mesozoic and Paleogene rocks in a complex structural pattern.  Pannonian sediments, which are part of a younger structural stage, deposited  on the horst limbs. The Pannonian marl strata dip at angles from 12° to 26°  (to the NNW), forming a monocline. The strata deformations are a consequence  of radial tectonics and are a potential source of landslides. The many  mollusks (7 gastropod and 9 bivalve species) and ostracodes (27 species) and  their biostratigraphical position indicate marl deposition throughout the  Pannonian age. A paleomagnetic investigation established that the marl has  inconsistent remanent magnetization (with bad statistical parameters), which  originates from neoformed magnetite

The Upper Miocene Lake Pannon marl from the Filijala Open Pit (Beocin, northern Serbia): New geological and paleomagnetic data