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Shear Zones,f deformation in planar zones that accommodate movement of relatively rigid wall-rock blocks. Deformation in such high-strain zones usually contains a rotation component, reflecting lateral displacement of wall rock segments with respect to each other; this type of high-strain zone is known as a ..
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Special Techniques,s its limitations. In many cases, additional information has to be gathered by other techniques. In this chapter, we wish to give the reader an outline of some other analytical laboratory techniques that use . for the study of tectonics. We indicate what problems can be studied by these techniques,
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