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Identyfikator w Bibliotece Wirtualnej Nauki: Conjugate normal faults, extension fractures and mesh-fracture structures were investigated in Devonian carbonate rocks from the southern part of the Holy Cross Mountains HCM Central Poland.

Strata folded during Geoloogia deformations were later subject to uplift, resulting in increasing extension in the upper part of the rock mass. At a relatively shallow depth, faults and fractures developed in an orderly vertical succession. The occurrences of conjugate normal sets enclosing different dihedral acute angles and extension fractures with similar strikes, juxtaposed with each other at the same stratigraphic level, point to the fact that the uplifted rock mass underwent successive changes geologiq a stress regime leading to the formation of these structures.


The first sets of conjugate normal faults and fractures developed when the HCM were uplifted during a late stage of Variscan deformations. The next sets of extension fractures and conjugate normal faults developed during the following uplift events interrupted by periods of sedimentation of the Mesozoic and younger strata.

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geologia regionalna polski mizerski pdf writer – PDF Files

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