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Late Silurian deformation in the Łysogóry Region of the Holy Cross Mountains revisited : restoration of a progressive Caledonian unconformity in the Klonów Anticline and its implications for the kinematics of the Holy Cross Fault (central Poland)

100%

Gągała Ł.

Geological Quarterly

2015

tom Vol. 59, No. 3

441--456

The Klonów Anticline is located in the western outskirts of the Łysogóry Region of the Holy Cross Mountains. A fresh look onto the cartographic evidence suggests that this structure shows the key characteristics of a progressive unconformity. This becomes evident when compared to the classical example of the Sant Llorenç de Morunys Anticline (eastern Pyrenees, Spain). The geometry of the unconformity requires a phase of thrusting or reverse faulting along the Holy Cross Fault in the latest Silurian–earliest Devonian (Late Caledonian deformation) followed by Variscan thin-skinned thrusting. Thick- and thin-skinned kinematic scenarios for the latest Silurian-earliest Devonian deformation of the Łysogóry Region are explored.

Two-wavelength folding in the Lublin Basin (Central Poland) indicates a depth- and lithology-dependent role of the layer-parallel-shortening

51%

Kufrasa M. , Gągała Ł. , Krzywiec P.

Geologia Sudetica

2014

tom Vol. 42

50--51