Figure G-32b is a sketch of a folded rock layer. The limbs of the folds deformed without

Question:

Figure G-32b is a sketch of a folded rock layer. The limbs of the folds deformed without fracturing, while fracturing occurred in the hinge zones. In terms of rheologic models, explain why the same material under the same conditions of temperature and pressure might behave differently in different places. $b ATH Fig. G-32b Sketch of a folded and fractured rock layer. For use in Problem 12.3.|$