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1 Studia Geologica Polonica

1 1999

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Correlation of the Subtatric tectonic units south of Zakopane (Polish Tatra Mts)

Bac-Moszaszwili Maria, Lefeld Jerzy

Studia Geologica Polonica

1999

Vol. 115

131--138

Tectonic units of the lower Subtatric nappe were correlated between the western and eastern parts of the Tatra Mts. It was found that the Mała Świnica unit does not continue toward the east beyond the western slopes of the Dolina Białego valley. North of the Krokiew tectonic scale, there is another unit called the Jastrzębia Turnia scale which, most probably, is a western continuation of the Jastrzębia Turnia-Palenica partial nappe. Fragments of the Middle and Upper Triassic and Lower Liassic rocks, exposed in tectonically reversed position under the Krokiew scale and the Mała Świnica unit, are classified to the Bielske Tatry partial nappe on the basis of identity of their lithostratigraphic sequences and facies development of the Fatra Formation. The so called “Czerwona Przełęcz syncline” thus loses its tectonic meaning: it should be eliminated from the tectonic nomenclature of the Subtatric zone