The Carboniferous foreland basin of western Poland contains a coherent succession of late Viséan through Westphalian turbidites derived from a uniform group of sources located within a continental magmatic arc. Detrital zircon geochronology indicates th
Main geodynamic and tectonic mechanisms responsible for evolution of foreland basins and their sedim...
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...
The Polish part of the Central European Variscan foreland includes several regional units that diffe...
An earlier concept of the Variscan foreland in Poland (Narkiewicz, 2007) is reconsidered in the ligh...
Sudetic segment of the Variscides, together with adjacent areas, experienced multi-stage accretion d...
Three Carboniferous-age detrital muscovites from the Variscan foreland basin of SW Poland and two mu...
The Variscan Externides in the area of south-western Poland (the basement of the Fore-Sudetic Monocl...
Carboniferous sandstones and shales encountered in deep boreholes drilled in central Poland, NW of t...
Extensive geophysical investigations in NE Poland in the 1950s and 1960s led to the discovery of an ...
International audienceExtensive geophysical investigations in NE Poland in the 1950s and 1960s led t...
The Precambrian crystalline rocks of northern Poland are known only from deep drill cores. Drilling ...
Upper Carboniferous foreland basins of the Rhenohercynian and Sub-Variscan parts of the Variscan oro...
Abstract: In the early Carboniferous, final subduction of the Rhenohercynian Ocean, accretion of a m...
International audienceThe late Palaeozoic Variscan Orogeny results from the convergence between two ...
Main geodynamic and tectonic mechanisms responsible for evolution of foreland basins and their sedim...
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...
The Polish part of the Central European Variscan foreland includes several regional units that diffe...
An earlier concept of the Variscan foreland in Poland (Narkiewicz, 2007) is reconsidered in the ligh...
Sudetic segment of the Variscides, together with adjacent areas, experienced multi-stage accretion d...
Three Carboniferous-age detrital muscovites from the Variscan foreland basin of SW Poland and two mu...
The Variscan Externides in the area of south-western Poland (the basement of the Fore-Sudetic Monocl...
Carboniferous sandstones and shales encountered in deep boreholes drilled in central Poland, NW of t...
Extensive geophysical investigations in NE Poland in the 1950s and 1960s led to the discovery of an ...
International audienceExtensive geophysical investigations in NE Poland in the 1950s and 1960s led t...
The Precambrian crystalline rocks of northern Poland are known only from deep drill cores. Drilling ...
Upper Carboniferous foreland basins of the Rhenohercynian and Sub-Variscan parts of the Variscan oro...
Abstract: In the early Carboniferous, final subduction of the Rhenohercynian Ocean, accretion of a m...
International audienceThe late Palaeozoic Variscan Orogeny results from the convergence between two ...
Main geodynamic and tectonic mechanisms responsible for evolution of foreland basins and their sedim...
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...