Skały tufogeniczne turneju z Bolechowie (Góry Świętokrzyskie)
Abstract
TUFOGENE ROCKS OF TOURNAISIAN FROM BOLECHOWICE (HOLY CROSS MOUNTAINS)In the Carboniferous (Tournaisian) rocks from the bore hole Bolechowice 1 the occurrence of pyroclastic material has been ascertained. Thicker intercalations of this material have been observed at the depths 109;50-110,50 m; 123,30-123,45 m; and 135,410-137,00 m. These rocks are conected with the Brethonian phase and represent, besides Zaręby (the Łagów syncline), Gruchawka, Bączków and vicinities of Masłów (the Miedziana Góra syncline - Fig. 2), the new occurrence sites of tufogene formations in the Carboniferous of the Holy Cross Mountains.Downloads
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