Abstract The Bodrogköz is predominantly a flat area surrounded by the rivers Tisza, Bodrog and Latorica. The Hungarian-Slovakian border cuts it into two parts; consequently, the geologic data in the two countries are different in terms of scale and in approach. The authors harmonized the different data on the two sides and created a unified geologic database for the entire area. The Bodrogköz is part of the depression at the northeastern part of the Great Hungarian Plain. It is covered mostly by Quaternary formations but in the Slovakian part there are smaller outcrops of Permian formations and Miocene volcanics
Abstract: The IBS Pannonian Basin project presents a good example of fruitful joint activity between...
The area in question represents northern part of the centralWest Carpathians and the boundary zone o...
In this paper old historical maps and the sheets of the Habsburg Military Surveys are analyzed to di...
In Mecsek Mts. and Balaton Highland a well studiable characteristic red sandstone group consisting o...
This study deals with the outlined classification of the Pannonian sediments of the Algyő anticline ...
Béla Bulla : Quelques problémes géomorphologiques interglaciaires de la zone périglaciaire du pléist...
South of the Sudetes and Tatra Mountains young sediments contain more of almost all micro- and mesoe...
The Danube / Kisalföld Basin is the north-western sub-basin of the Pannonian Basin System. The litho...
Hungary lies entirely within the Carpatho-Pannonian Region (CPR), a dominant tectonic unit of easter...
The Tisia Composite Terrane Alpine megatectonic unit forms the pre-Neogene crystalline basement of S...
In the central part of the Southern Great Plain (Szeged environment, between 1965 and 1977) about 15...
Comprehensive chronological, geological and paleontological investigations were conducted as part of...
Abstract The Mid-Hungarian (or Zagreb-Zemplin) Line of WSW–ENE strike divides the Pannonian baseme...
The Austrian Geological Survey and Czech geological organizations have in their archives source mate...
Disertační práce se zabývá morfostrukturním vývojem údolní sítě Kladské Bělé (Bialy Lądecke, dále je...
Abstract: The IBS Pannonian Basin project presents a good example of fruitful joint activity between...
The area in question represents northern part of the centralWest Carpathians and the boundary zone o...
In this paper old historical maps and the sheets of the Habsburg Military Surveys are analyzed to di...
In Mecsek Mts. and Balaton Highland a well studiable characteristic red sandstone group consisting o...
This study deals with the outlined classification of the Pannonian sediments of the Algyő anticline ...
Béla Bulla : Quelques problémes géomorphologiques interglaciaires de la zone périglaciaire du pléist...
South of the Sudetes and Tatra Mountains young sediments contain more of almost all micro- and mesoe...
The Danube / Kisalföld Basin is the north-western sub-basin of the Pannonian Basin System. The litho...
Hungary lies entirely within the Carpatho-Pannonian Region (CPR), a dominant tectonic unit of easter...
The Tisia Composite Terrane Alpine megatectonic unit forms the pre-Neogene crystalline basement of S...
In the central part of the Southern Great Plain (Szeged environment, between 1965 and 1977) about 15...
Comprehensive chronological, geological and paleontological investigations were conducted as part of...
Abstract The Mid-Hungarian (or Zagreb-Zemplin) Line of WSW–ENE strike divides the Pannonian baseme...
The Austrian Geological Survey and Czech geological organizations have in their archives source mate...
Disertační práce se zabývá morfostrukturním vývojem údolní sítě Kladské Bělé (Bialy Lądecke, dále je...
Abstract: The IBS Pannonian Basin project presents a good example of fruitful joint activity between...
The area in question represents northern part of the centralWest Carpathians and the boundary zone o...
In this paper old historical maps and the sheets of the Habsburg Military Surveys are analyzed to di...