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METAMORPHISM OF THE JANOV GRUN LOWER PALEOZOIC VOLCANO-SEDIMENTARY FORMATION (VEPORIC UNIT, WESTERN CARPATHIANS)

In: Geologica Carpathica, vol. 45, no. 1
Oto Miko - Sergey P. Korikovsky
Detaily:
Rok, strany: 1994, 57 - 65
O článku:
Authors present evidence on the low-grade progressive Variscan metamorphism of the Lower Paleozoic Janov Grun Formation occurring in the eastern part of the Nizke Tatry Mts. The metamorphic conditions determined indicate temperatures about 340–370 °C and pressures 340–400 MPa (3.4–4 kbar).
Ako citovať:
ISO 690:
Miko, O., P. Korikovsky, S. 1994. METAMORPHISM OF THE JANOV GRUN LOWER PALEOZOIC VOLCANO-SEDIMENTARY FORMATION (VEPORIC UNIT, WESTERN CARPATHIANS). In Geologica Carpathica, vol. 45, no.1, pp. 57-65. 1335-0552.

APA:
Miko, O., P. Korikovsky, S. (1994). METAMORPHISM OF THE JANOV GRUN LOWER PALEOZOIC VOLCANO-SEDIMENTARY FORMATION (VEPORIC UNIT, WESTERN CARPATHIANS). Geologica Carpathica, 45(1), 57-65. 1335-0552.