Collected Item: “Stratigraphic implications of the Mio-Pliocene geodynamics in the area of Mt. Avala: new evidence from Torlak Hill and Beli Potok (Belgrade, Serbia)”
Врста публикације
Рад у часопису
Верзија рада
објављена верзија
Језик рада
енглески
Аутор/и (Милан Марковић, Никола Николић)
Ljupko Rundić, Meri GAnić, Slobodan Knežević, Dejan Radivojević, Miloš Radonjić
Наслов рада (Наслов - поднаслов)
Stratigraphic implications of the Mio-Pliocene geodynamics in the area of Mt. Avala: new evidence from Torlak Hill and Beli Potok (Belgrade, Serbia)
Наслов часописа
Geologia Croatica
Година издавања
2019
Сажетак на енглеском језику
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. Badenian and Pannonian) in a relatively small
area. These spatial relationships are interpreted in the context of pronounced block structures
(Torlak, Beli Potok and Avala). Torlak Hill represents a horst structure with a core composed of
Mesozoic rocks and hillsides composed of the Middle Miocene sediments, which are present at
the surface at altitudes up to 336 metres. Nearby, there is the Beli Potok asymmetrical trough
that was infilled by the late Miocene sediments. The Torlak horst and the Beli Potok trough structures
are separated by the Rakovica normal fault. In some places along the fault line, several
geological units are vertically displaced more than a hundred metres. For example, in borehole
KGK-14, the Upper Miocene Pannonian marls are observed at a depth of 100 metres below the
surface. However, only a few hundred metres away to the northeast, similar Pannonian marls
are observed at the surface, at an altitude of about 210 metres. Due to the mentioned observed
vertical movements along the block structures, a composite hilly relief with dominant the Torlak
Hill and the Beli Potok Valley was formed.
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. Badenian and Pannonian) in a relatively small
area. These spatial relationships are interpreted in the context of pronounced block structures
(Torlak, Beli Potok and Avala). Torlak Hill represents a horst structure with a core composed of
Mesozoic rocks and hillsides composed of the Middle Miocene sediments, which are present at
the surface at altitudes up to 336 metres. Nearby, there is the Beli Potok asymmetrical trough
that was infilled by the late Miocene sediments. The Torlak horst and the Beli Potok trough structures
are separated by the Rakovica normal fault. In some places along the fault line, several
geological units are vertically displaced more than a hundred metres. For example, in borehole
KGK-14, the Upper Miocene Pannonian marls are observed at a depth of 100 metres below the
surface. However, only a few hundred metres away to the northeast, similar Pannonian marls
are observed at the surface, at an altitude of about 210 metres. Due to the mentioned observed
vertical movements along the block structures, a composite hilly relief with dominant the Torlak
Hill and the Beli Potok Valley was formed.
Волумен/том или годиште часописа
2
Број часописа
72
Почетна страна
109
Завршна страна
128
DOI број
https://doi.org/10.4154/gc.2019.11
ISSN број часописа
ISSN 1330-030X
Кључне речи на српском (одвојене знаком ", ")
мио-плиоценска геодинамика, јужни Панонски басен, Авалски и Торлак хорст, Белопоточки трог, Србија
Кључне речи на енглеском (одвојене знаком ", ")
Mio-Pliocene geodynamics, Southern Pannonian Basin, Avala and Torlak horsts, Beli Potok trough, Serbia
Шира категорија рада према правилнику МПНТ
M20
Ужа категорија рада према правилнику МПНТ
М22
Степен доступности
Отворени приступ
Лиценца
Creative Commons – Attribution 4.0 International
Формат дигиталног објекта
.pdf