ANCHIMETAMORPHISM OF PERMIAN SANDSTONES OF THE STRUZENIK GROUP IN THE NIZKE TATRY MTS. (WESTERN CARPATHIANS)

Rok, strany: 1992, 97 - 104

Permian sandstones, as the cover of the Veporic Nappe of tonalites in the Central Western Carpathians, were anchimetamorphosed during Middle Cretaceous folding events (at T up to 320 °C). This is shown by the presence of metastable phases (half-disintegrated clastogenic biotites and muscovites) as well as by the difference in the composition of clastogenic (muscovite) and authigenic (Ti-phengite, phengitic sericite) micas. The authors discuss the criteria for anchi- and epimetamorphism, as well as the possibilities of Alpine diaphtoresis of the crystalline basement.

ISO 690:

P. Korikovsky, S., Putis, M., A. Boronikhin, V. 1992. ANCHIMETAMORPHISM OF PERMIAN SANDSTONES OF THE STRUZENIK GROUP IN THE NIZKE TATRY MTS. (WESTERN CARPATHIANS). In Geologica Carpathica, vol. 43, no.2, pp. 97-104. 1335-0552.

APA:

P. Korikovsky, S., Putis, M., A. Boronikhin, V. (1992). ANCHIMETAMORPHISM OF PERMIAN SANDSTONES OF THE STRUZENIK GROUP IN THE NIZKE TATRY MTS. (WESTERN CARPATHIANS). Geologica Carpathica, 43(2), 97-104. 1335-0552.