The Mid-Polish Swell developed strictly along the axis of the Mid-Polish Trough, the latter spatially developed on top of the Teisseyre-Tornquist Zone. Hence, we conclude that the trough and
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The Inter-Tropical Zone of convergence gets located much further to the north of the equator in the months of May to September than during November to April, when it is located close to Mauritius.
Polish citizens do not need a tourist visa when travelling to Mauritius. This tourist visa typically allows a short term stay. The Mauritius tourist visa remains valid for 3 months. Mauritius
Polished concrete is a reinforced concrete mixed with aggregates for decorative floors, created to be polished with grinding equipment, to provide an
Permian to Cretaceous Mid-Polish Trough (MPT) belonged to the system of epicontinental depositional basins of western and central Europe. Its sedimentary infill consists of several kilometres of
Summary: Tectonic subsidence of the preserved and analysis reconstructed of the Polish Basin indicates an initial Late P rmian-Early (255-241 Triassic Ma) syn-rift phase of development with a
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Numerous brittle deformations related to the Late Cretaceous inversion of the Mid-Polish Trough (MPT) have been identified in its various parts using seismic data. The role of Zechstein evaporitic deposits
Implications for early basin dynamics of the Mid-Polish Trough from deformational structures within salt deposits in central Poland
The Mid-Polish Trough (MPT) is well recorded in the distribution of thickness of the Mesozoic sediments. Its shape was most distinctly delineated in the Early Triassic, and Early to
We constructed a 3-D structural model of the Mid-Polish Trough in order to study the inversion processes on a basin-wide scale. To elaborate the 3-D geometry of the Permian–Mesozoic
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New data on the evolution of Upper Jurassic deposits in the Carpathian Foredeep substrate provide in formation that there is a complete Oxfordian through Valanginian succession in
The Mid-Polish Trough is well recorded in the thickness pattern of the Mesozoic stratigraphic columns. It was most dis-tinct in the Early Triassic and in the Early to Middle Jurassic, when the thickness
The Mid-Polish Trough and Polish Basin occur in a transitional domain between eastern and western Europe that is characterized by relatively thick lithospheric mantle and deep Moho.
Background This database is comprised of two separate lists: "Refugees in Mauritius who consider themselves citizens of the Free City of Danzig" and
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