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12 Milonita, Facutad de Ingeniería, UNAM

12 Milonita, Facutad de Ingeniería, UNAM

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A granoblastic rock with a fine to coarse grain size is called a gneiss. It forms through dynamic metamorphism known as millonitization, where the grain size of a rock is reduced by ductile shear. Gneisses exhibit a marked planar and linear internal structure called foliation and lineation, parallel to the fault zone.

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