The earliest geological and paleontological notes about Osijek and its surrounding originate from the 19th century. Geology of this part of our country has for the first time been presented on the Revised Geological Map of Austria-Hungary Monarchy, by Ritter von Hauer, published in Vienna (1867-1871). As in those days researchers could study only surface layers with mostly loess, that is why those layers were the main topic of the earliest geological works. One of the first authors who dealt with that topic was Pilar (1875) whereas thirty years later the Commission for Scientific research of Syrmia initiated research of loess areas in Slavonia. The founder of the Commission, Gorjanovic-Kramberger (1912, 1914, 1914a, 1921 ,1922) published ...
Three loess units and two palaeopedological layers are preserved m the nearly 8 meter thick Miseluk ...
<p>Croatian Geological Survey is the successor of the Geological Commission for the Kingdoms of Croa...
For approximately 120 years since the beginning of European geology up to the present day, Croatian ...
The earliest geological and paleontological notes about Osijek and its surrounding originate from th...
The loess-paleosol sequences of the Danube basin contain the longest and most complete terrestrial r...
<p>This contribution focuses on two PhD projects, which are integrated within the collaborative rese...
The loess-paleosol sequences of the Danube basin contain the longest and most complete terrestrial r...
oai:repozitorij.rgn.unizg.hr:rgn_1121The Pleistocene loess and Holocene alluvial sediments are domin...
oai:repozitorij.unizg.hr:rgn_1121The Pleistocene loess and Holocene alluvial sediments are dominant ...
Susak Island is the outermost member of the archipelago of the Kvarner Bay, North Adriatic Sea, Croa...
Late Pleistocene loess-palaeosol sequences are widespread in the Vojvodina region, with thicknesses ...
Susak Island is the outermost member of the archipelago of the Kvarner Bay, North Adriatic Sea, Croa...
Notes about morphotectonic and limestones reliefs and environments evolution of occidental Macedonia...
High inconsistency and incoherence in the stratigraphy of the Slovenian upper Paleogene and lower Mi...
In the area of Eastern Srem Pleistocene sediments cover large territories. Their facial diversity an...
Three loess units and two palaeopedological layers are preserved m the nearly 8 meter thick Miseluk ...
<p>Croatian Geological Survey is the successor of the Geological Commission for the Kingdoms of Croa...
For approximately 120 years since the beginning of European geology up to the present day, Croatian ...
The earliest geological and paleontological notes about Osijek and its surrounding originate from th...
The loess-paleosol sequences of the Danube basin contain the longest and most complete terrestrial r...
<p>This contribution focuses on two PhD projects, which are integrated within the collaborative rese...
The loess-paleosol sequences of the Danube basin contain the longest and most complete terrestrial r...
oai:repozitorij.rgn.unizg.hr:rgn_1121The Pleistocene loess and Holocene alluvial sediments are domin...
oai:repozitorij.unizg.hr:rgn_1121The Pleistocene loess and Holocene alluvial sediments are dominant ...
Susak Island is the outermost member of the archipelago of the Kvarner Bay, North Adriatic Sea, Croa...
Late Pleistocene loess-palaeosol sequences are widespread in the Vojvodina region, with thicknesses ...
Susak Island is the outermost member of the archipelago of the Kvarner Bay, North Adriatic Sea, Croa...
Notes about morphotectonic and limestones reliefs and environments evolution of occidental Macedonia...
High inconsistency and incoherence in the stratigraphy of the Slovenian upper Paleogene and lower Mi...
In the area of Eastern Srem Pleistocene sediments cover large territories. Their facial diversity an...
Three loess units and two palaeopedological layers are preserved m the nearly 8 meter thick Miseluk ...
<p>Croatian Geological Survey is the successor of the Geological Commission for the Kingdoms of Croa...
For approximately 120 years since the beginning of European geology up to the present day, Croatian ...