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. 2012 Jan 13;12(6):064708. doi: 10.1088/1468-6996/12/6/064708

Figure 6.

Figure 6.

Distribution of mineral strain along the azimuthal directions derived from the segmental-shift approach. Crystal strain along different orientation can be visualized using the area detector (IP) under different applied loads. Loading axis is along the preferential orientation of mineral crystals. The zero-strain line separates tensile and compressive regions. (Reprinted with permission from [58] © 2008 Elsevier Ltd.)