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Textural changes in [[rock]]s in which brittle minerals and rocks are broken and flattened as a result of intense folding or [[fault]]ing; produces fragmentation of rocks as coarse-grained [[breccia]]s and fine-grained mylonites. <br/>Source: Leet, L. Don. 1982. <i>Physical Geology, 6th Edition.</i> Englewood Cliffs, NJ: Prentice-Hall

[[Category: geology]]

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