Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4733194 | Journal of Structural Geology | 2013 | 12 Pages |
A method is proposed for determining the 2D deformation gradient tensor that represents the deformations of pre- and post-deformation markers with arbitrary shapes. The deformation is not necessarily coaxial. The tensor is evaluated in a least-square sense. Therefore, the method can deal with heterogeneous deformations, and calculate their average tensor. The inverse method has the residuals that can be directly converted to the logarithmic strain needed to transform the calculated post-deformation shapes to observed ones. In addition, we propose the measure of heterogeneity for finite deformations. The method was applied to artificial and natural data from balanced cross sections.
Graphical abstractFigure optionsDownload full-size imageDownload high-quality image (138 K)Download as PowerPoint slideHighlights► An inverse method is proposed for determining 2D deformation gradient tensor. ► The method uses the pre- and post-deformation markers with arbitrary shapes. ► The method assumes homogeneous deformation, and a heterogeneity measure is proposed. ► A measure of non-coaxiality is proposed for finite deformations. ► The method was applied to markers in balanced cross-sections.