Abstract: NOTES ON STRUCTURE TYPES IN THE META-CARPATHIAN ARCH The polygenic structural zone of the Meta-Carpathian archthis in the W-E direction elevated area of the Southern part of Central Poland (Fig. 1, 6) of Tertiary age, resembling E. Argand's plis de fond - contains older forms too. These are: the W-E (with a slight northwestern declination) northern marginal zone of the Hercynian foldings (S. Bubnoff, 1930; H. Stille, 1929) and Old-Cimerdian elements with a similar trend (J. Znosko, 1935). Moreover, here also belong the following Laramian forms with a NW-SE trend which cut the arch with their southeastern parts: the fore Sudetic monocline, the Szczecin-Łodź-Miechow basin, the Mesozoic periphery of the Świety Krzyz Mountains (J. Czarnocki, 1938, W. Pozaryski, 1943, 1957; J. Samsonowicz, 1929) and the Lublin-Lwow syncline (H. Pozaryski, 1956).
Publication Year: 1958
Publication Date: 1958-01-01
Language: en
Type: article
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