Monoclinic and triclinic 3D flanking structures around elliptical cracks.

Ulrike Exner1, Marcin Dabrowski2

  • 1University of Vienna, Department of Geodynamics and Sedimentology, Althanstrasse 14, 1090 Vienna, Austria.

Journal of Structural Geology
|April 13, 2019
PubMed
Summary

This study models 3D flanking structure evolution in shear zones using a modified Eshelby solution. 3D crack geometry significantly alters deformation patterns compared to 2D models, offering insights into geological flow kinematics.

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