4.5 Article

Sheath fold development around deformable inclusions: Integration of field-analysis (Cima Lunga unit, Central Alps) and 3D numerical models

期刊

JOURNAL OF STRUCTURAL GEOLOGY
卷 144, 期 -, 页码 -

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.jsg.2020.104255

关键词

Sheath fold; Deformable inclusion; Super-simple shear; 3D models; Central alps; Progressive deformation

资金

  1. SUPSI (Swis) [12RAFGOSO]
  2. Polish Geological Institute -National Research Institute (Poland) [62.9012.1957.00.0]

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The study investigated the unique structural patterns within a km-scale shear zone, emphasizing the coupled deformation between ultramafics and host rocks. Results from numerical modeling showed that the deformation and fold development of inclusions were dependent on viscosity ratio, shear strain, and inclusion aspect ratio. The study highlights the importance of progressive deformation in explaining complex structural patterns in shear zones without requiring multiple deformation phases.
We investigated complex tectonic structures within a km-scale shear zone (Cima Lunga unit), which is traditionally interpreted as generated by multiple, distinct deformation phases, despite showing unique schistosity and lineation. Based on structural analyses we discovered sheath folds developed in relatively weak gneissic/schistose rocks, enveloping inclusions of stronger ultramafics. The internal layering of inclusions experienced superimposed folding, boudinage and folding, attesting to layer-parallel shortening followed by stretching and further again shortening. Using 3D numerical modelling, we explored the structure evolution within and around deformable viscous inclusions under far-field simple shear. The numerical results showed that the internal deformation of ellipsoidal inclusions and the fold development around the inclusions are both dependent on the viscosity ratio, shear strain and the inclusion aspect ratio. The Cima Lunga structural patterns were reproduced for finite strains exceeding 7.5 and viscosity ratio between 2.8 and 9. Inclusions are characterized by persistent rotation of the internal layering, resulting in super-simple shear regime, with kinematic vorticity number >1. An important corollary is that ultramafics and host rocks experienced coupled deformation since the prograde metamorphic evolution. Finally, we emphasise that progressive deformation in shear zones may offer sufficient explanation for complex structural patterns, without invoking unjustified polyphase deformation.

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