Jointing in the Dukla Nappe (Outer Carpathians, Poland) : an attempt at palaeostress reconstruction

Mastella, L.; Zuchiewicz, W.

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Jointing in the Dukla Nappe (Outer Carpathians, Poland) : an attempt at palaeostress reconstruction

Autorzy

Mastella L. , Zuchiewicz W.

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Abstrakty

The joint network in the portion of the Dukla Nappe studied originated in two stages showing different orientations of the stress field axes. The older, compressive stage I was characterised by a N45°E-orientated (at present coordinates) horizontal s1, and formation of the diagonal, shear (SL and SR) joint system. The younger, extensional stage II was characterised by vertical s1 and horizontal, N35°E-orientated (also at present coordinates) s3, suitable for formation of the fold-parallel joints. At the turn of the first stage, under diminishing horizontal compression (s1 trending N35°E), the cross-fold T joints developed. The orientation of the maximum compression axis changed between stages I and II. The first stage probably commenced while strata which were not fully lithified underwent shortening, and lasted until the termination of nappe emplacement. The second stage, in turn, is associated with post-orogenic collapse of the Carpathians, whose onset in the study region began at least in Late Miocene times.

Słowa kluczowe

Outer Carpathians Dukla nappe jointing palaeostress reconstruction

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2000

Tom

Vol. 44, Nr 4

Strony

377--390

Opis fizyczny

fot., rys., wywkr., bibliogr. 87 poz.

Twórcy

autor

Mastella L.

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

autor

Zuchiewicz W.

Institute of Geological Sciences, JagielIonian University, Oleandry 2A, PL-30-063 Kraków, Poland

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