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Crustal structure at the Trans-European Suture Zone in northwest Poland based on gravity data
A new gravity model of the crustal structure of the Trans-European Suture Zone in the northwestern Poland has been constructed. The Bouguer anomaly map, obtained after stripping off theExpand
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Transcurrent nature of the Teisseyre–Tornquist Zone in Central Europe: results of the POLCRUST-01 deep reflection seismic profile
Teisseyre–Tornquist Zone (TTZ) corresponds to a crustal boundary between the Precambrian East European Platform (EEP) and the Palaeozoic West European Platform. Although the zone has been controllingExpand
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Lithospheric structure across the Trans-European Suture Zone in NW Poland based on gravity data interpretation
We provide an analysis of geophysical and geological data from the Baltic segment of the Trans-European Suture Zone (TESZ). The construction of structural and density maps of theExpand
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Basement structure of the Paleozoic Platform in Poland
The Paleozoic Platform comprises the southwestern half of the Polish territory, separated from the Precambrian East European Platform (EEP) by a NW–SE trending subvertical lithospheric-scaleExpand
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A new magnetic anomaly map of Poland and its contribution to the recognition of crystalline basement rocks
Magnetic total field measurements acquired in Poland between 1974 and 2011 have been compiled in a new digital database that provides a complete picture of magnetic anomalies of the country. The dataExpand
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Geophysical constraints on the crustal structure of the East European Platform margin and its foreland based on the POLCRUST-01 deep reflection seismic profile
Abstract A new 240-km long, deep seismic reflection profile (POLCRUST-01) was recently acquired in SE Poland crossing the East European Platform (EEP) margin south-east of the North-German–PolishExpand
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Strefa Teisseyre’a-Tornquista – dawne koncepcje a nowe dane
Teisseyre-Tornquist Zone – evolving approaches and new data. A b s t r a c t. Concepts prevailing among the Polish geoscientists during the last decades assumed that the Teisseyre-Tornquist Zone is aExpand
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