20th EGU General Assembly, EGU2018, Proceedings from the conference held 4-13 April, 2018 in Vienna, AustriaRecent years have brought a significant progress in understanding of the external Variscides in Poland. Combined POLCRUST-01 and PolandSPAN deep seismic surveys imaged for the first time a Variscan thin-skinned fold-and-thrust belt that encroaches onto a little deformed basement slope of the East European Craton (EEC) much farther eastward than the previously postulated position of the Variscan deformation front. This deformed belt consists of several tectonic units, to a various degree overprinted by Variscan shortening and inversion (Fragment tekstu)
The attempt to divide the Upper Silesian Block and the Małopolska Block into tectonic units has been...
The Eastern European lithosphere is a natural laboratory to study continental formation and evolutio...
The Trans-European Suture Zone (TESZ) is the most important and extensive continental suture in Euro...
The authors interpret the structure of the Central Carpathian-North European plates suture zone in P...
"The European Variscan belt sharply changes its trend in easternmost Germany and western Poland, wh...
An earlier concept of the Variscan foreland in Poland (Narkiewicz, 2007) is reconsidered in the ligh...
Geophysical and geological data from the eastern sector of the Central European Variscan belt are pr...
Geophysical and geological data from the eastern sector of the Central European Variscan belt are pr...
In NE Poland, Eastern European Craton (EEC) crust of Fennoscandian affinity is concealed under a Pha...
The extension of eastern Avalonia from Britain through the NE German Basin into Poland is, in some s...
This paper presents an integrated geophysical study of the southern margin of the East European Crat...
Sudetic segment of the Variscides, together with adjacent areas, experienced multi-stage accretion d...
The TTZ-South seismic profile follows the Teisseyre-Tornquist zone (TTZ) at the SW margin of the Eas...
A new geologic map of the crystalline basement of NE Poland has been constrained on the basis of the...
The Polish part of the Central European Variscan foreland includes several regional units that diffe...
The attempt to divide the Upper Silesian Block and the Małopolska Block into tectonic units has been...
The Eastern European lithosphere is a natural laboratory to study continental formation and evolutio...
The Trans-European Suture Zone (TESZ) is the most important and extensive continental suture in Euro...
The authors interpret the structure of the Central Carpathian-North European plates suture zone in P...
"The European Variscan belt sharply changes its trend in easternmost Germany and western Poland, wh...
An earlier concept of the Variscan foreland in Poland (Narkiewicz, 2007) is reconsidered in the ligh...
Geophysical and geological data from the eastern sector of the Central European Variscan belt are pr...
Geophysical and geological data from the eastern sector of the Central European Variscan belt are pr...
In NE Poland, Eastern European Craton (EEC) crust of Fennoscandian affinity is concealed under a Pha...
The extension of eastern Avalonia from Britain through the NE German Basin into Poland is, in some s...
This paper presents an integrated geophysical study of the southern margin of the East European Crat...
Sudetic segment of the Variscides, together with adjacent areas, experienced multi-stage accretion d...
The TTZ-South seismic profile follows the Teisseyre-Tornquist zone (TTZ) at the SW margin of the Eas...
A new geologic map of the crystalline basement of NE Poland has been constrained on the basis of the...
The Polish part of the Central European Variscan foreland includes several regional units that diffe...
The attempt to divide the Upper Silesian Block and the Małopolska Block into tectonic units has been...
The Eastern European lithosphere is a natural laboratory to study continental formation and evolutio...
The Trans-European Suture Zone (TESZ) is the most important and extensive continental suture in Euro...