Mt. Avala is located on the southern margin of the Pannonian basin (SPB), a border zone between the uplifted morphostructures of the Dinarides and Carpathian-Balkanides. Similar to the Pannonian basin, tectonostratigraphic evolution of the Mt. Avala area during the last 23 Ma has is characterized by syn- and post-rifting processes as well as tectonic inversion. Here, we present the results of field investigations of the Miocene‒Pliocene dynamics that led to different spatial positions of the same stratigraphic units (e.g. ...
... area of the
Torlak hills and Mt. Avala belongs to the Avala-Orešac structural
unit characterized by blocky structure (MAROVIĆ &
KNEŽEVIĆ, 1985; MAROVIĆ et al., 2007). According to
MAROVIĆ & KNEŽEVIĆ (1985), TOLJIĆ (1996, 2016) and
MAROVIĆ et al. (2007), the Avala-Orešac structural unit was
dissected ...
... 4154/gc.2019.11
Abstract
Mt. Avala is located on the southern margin of the Pannonian basin (SPB), a border zone be-
tween the uplifted morphostructures of the Dinarides and Carpathian-Balkanides. Similar to the
Pannonian basin, tectonostratigraphic evolution of the Mt. Avala area during the last 23 Ma ...
... been collected from both banks of
the Rakovica Stream valley (Rakovički potok) located in the
N-NW part of Mt. Avala. Other samples have been taken more
toward the north-northeast of Mt. Avala (Torlak, Beli Potok,
Leštane, and Vrčin – Fig. 1). All the analyzed samples were
collected from the twelve ...
Ljupko Rundić, Meri Ganić, Slobodan Knežević, Dejan Radivojević, Miloš Radonjić. "Stratigraphic implications of the Mio-Pliocene geodynamics in the area of Mt. Avala: new evidence from Torlak Hill and Beli Potok (Belgrade, Serbia)" in Geologia Croatica (2019). https://doi.org/10.4154/gc.2019.11
