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O nowych rozwiązaniach tektonicznych w „Atlasie geologicznym Polski”

Aleksandrowski P., Mazur S.

Przegląd Geologiczny

2017

Vol. 65, nr 12

1499--1510

Authorial comprehensive comments and explanations are given to some of the interpretations applied in the tectonic part of the newly published Geological Atlas of Poland (Nawrocki, Becker, 2017) that considerably change the hitherto generally accepted concepts. It should be, however, admitted that most of those "new’" solutions were already proposed in the past by other workers as hypotheses that could not have been tested in the then state of knowledge on Poland’s deep geology and scientific tools at hand. This has now changed with abundant new data obtained with modern seismic techniques and advanced methods of potential field modelling. Using those data, we justify the reasons for, among others, a significant eastward shifting the front of the Variscan Orogen in Poland andfor the accompanying change in position of the division line between the Precambrian and Palaeozoic platforms. We also show the rationale for accepting a far-reaching southwestward extent of the East European Craton’s crystalline basement below the Palaeozoic Platform and for reinterpretation of the Teisseyre-Tornquist Zone’s nature, together with the question of early Palaeozoic terranes in the TESZ and the situation of the Caledonian foredeep at the SW margin of the East-European Craton.

Wawrzyniec i Henryk Teisseyre’owie

Miecznik J. B.

Przegląd Geologiczny

2015

Vol. 63, nr 2

86–-92

The Teisseyre family is a very meritorious family in Polish geology. Senior Wawrzyniec Teisseyre (1860–1939), cartographer, tectonicist, petroleum geologist and paleontologist, first determined the course of the SW boundary of the East European Platform, subsequently confirmed by magnetic studies of German geophysicist A.J.H. Tornquist. This important continental-scale feature has a character of deep fractures and is called today the Teisseyre-Tornquist Zone. Wawrzyniec's son, Henryk Teisseyre (1903–1975), was an eminent Carpathian geologist. After World War II, he was the co-founder of the Wroc³aw centre of Polish geology and the creator of Wroc³aw school of tectonics. Significant roles in the geology were played by Henryk's sons: prematurely died Juliusz (1933–1991) and Andrzej Karol (1938–1991). Henryk's nephew, Roman Teisseyre (born 1929), is a world-class seismologist, researcher in physics of the Earth interior.