%0 Journal article
%A Leiss, B.
%A Siegesmund, S.
%A Weber, K.
%T Texture asymmetries as shear sense indicators in naturally deformed mono- and polyphase carbonate rocks
%R 10.1155/TSM.33.61
%R 10.23689/fidgeo-2428
%J Textures and microstructures
%V 33
%N 1/4

%X The microstructural and quantitative texture analyses of a naturally deformed calcite mylonite, a dolomite mylonite and a dolomitic calcite mylonite reveal different texture asymmetries for comparable deformation conditions. Calcite shows a c-axis maximum rotated against the shear sense with regard to the main shear plane. In contrast, the dolomite shows a c-axis maximum rotated with the shear sense. In accordance with the experimental and simulated textures from the literature, this difference proves e-twinning and r-slip for calcite and f-twinning and c-slip for dolomite as the main deformation mechanisms. The dolomitic calcite mylonite shows for both the calcite and the dolomite a c-axis maximum rotated against the shear sense. On account of the microstructure of this sample, the dolomite texture has been passively overtaken from the deformation texture of calcite during a late-deformative dolomitization. The results significantly contribute to the interpretation that the sampled shear zone is a transpressive strikeslip fault.
%U http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/6741
%~  FID GEO-LEO e-docs