Deformation mechanisms of cataclastic rocks from fault zones in the Magura nappe in the Beskid Wyspowy Mountains (Poland)

• Autorzy: Konon A.
• Języki publikacji: EN

Abstrakty

EN

Analyses of intact orientated samples of incompetent fault rocks from thrusts within the Magura nappe in the Beskid Wyspowy Mountains indicate an arrangement of clay mineral plates parllel to numerous shears present in the rocks. Reconstruction of the development of the shears suggests several phases of formation. Maximum palaeotemperatures in the range 80-160 stopni C were reconstructed from the fault zones

Słowa kluczowe

EN

Cataclastic rock; deformation mechanisms; fault zones; Magura Nappe; palaeotemperatures

• Wydawca: Faculty of Geology of the University of Warsaw ; Komitet Nauk Geologicznych PAN
• Czasopismo: Acta Geologica Polonica
• Rocznik: 2000
• Tom: Vol. 50, no. 3
• Strony: 387--392
• Opis fizyczny: Bibliogr. 44 poz.

Twórcy

autor

Konon A.

• Institute of Geology, University of Warsaw, Al. Żwirki i Wigury 93, PL-02-089 Warszawa, Poland