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ANCHIZONAL ALPINE METAMORPHISM OF TATRIC COVER SEDIMENTS IN THE MALE KARPATY MTS. (WESTERN CARPATHIANS)

In: Geologica Carpathica, vol. 44, no. 6
Dusan Plasienka - Sergey Petrovich Korikovsky - Anton Hacura
Detaily:
Rok, strany: 1993, 365 - 371
O článku:
Permo-Mesozoic Tatric cover sediments in the Male Karpaty Mts. suffered an early Alpine (Cretaceous) low-T metamorphic imprint mostly at an estimated temperature of 250–300 °C (illite-crystallinity, composition of authigenic micas, deformation mechanisms). The source of the metamorphic temperature is tentatively interpreted as an increased heat flow inherited from a previous period of crustal thinning and probable shear heating as well. Synkinematic metamorphic recrystallization is a consequence of basement thrust stacking and thermal equilibration between cold footwall sediments and hot hangingwall basement rocks detached at mid-crustal levels.
Ako citovať:
ISO 690:
Plasienka, D., Petrovich Korikovsky, S., Hacura, A. 1993. ANCHIZONAL ALPINE METAMORPHISM OF TATRIC COVER SEDIMENTS IN THE MALE KARPATY MTS. (WESTERN CARPATHIANS). In Geologica Carpathica, vol. 44, no.6, pp. 365-371. 1335-0552.

APA:
Plasienka, D., Petrovich Korikovsky, S., Hacura, A. (1993). ANCHIZONAL ALPINE METAMORPHISM OF TATRIC COVER SEDIMENTS IN THE MALE KARPATY MTS. (WESTERN CARPATHIANS). Geologica Carpathica, 44(6), 365-371. 1335-0552.