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KYANITE FROM EARLY PALEOZOIC ROCKS OF THE GEMERICUM (WESTERN CARPATHIANS) AND ITS IMPLICATIONS FOR BARIC CONDITIONS OF VARISCAN METAMORPHISM

In: Geologica Carpathica, vol. 43, no. 4
Shah Wali Faryad - Ivan Dianiska

Details:

Year, pages: 1992, 199 - 201
Language: eng
Full text
About article:
A first occurrence of kyanite from low-grade sequences of the Gemericum is discussed here. It was found in volcano-sedimentary rocks overprinted by contact metamorphism. The presence of kyanite clarifies metamorphic conditions, namely the pressure conditions of Variscan regional metamorphism that were due to the lack of index minerals in these low-grade rocks, subject of various speculations.
How to cite:
ISO 690:
Wali Faryad, S., Dianiska, I. 1992. KYANITE FROM EARLY PALEOZOIC ROCKS OF THE GEMERICUM (WESTERN CARPATHIANS) AND ITS IMPLICATIONS FOR BARIC CONDITIONS OF VARISCAN METAMORPHISM. In Geologica Carpathica, vol. 43, no.4, pp. 199-201. 1335-0552.

APA:
Wali Faryad, S., Dianiska, I. (1992). KYANITE FROM EARLY PALEOZOIC ROCKS OF THE GEMERICUM (WESTERN CARPATHIANS) AND ITS IMPLICATIONS FOR BARIC CONDITIONS OF VARISCAN METAMORPHISM. Geologica Carpathica, 43(4), 199-201. 1335-0552.