| 1. | The fault zones are marked by a zone of sheared rocks characterized by mylonite.
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| 2. | Mylonite development, biotitization, chloritization and microgranulation are found associated with these surfaces.
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| 3. | They contain pumices of various colours and lithic fragments, including mylonite and schist.
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| 4. | At depth, the angular breccias transit into a ductile shear texture and into mylonite zones.
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| 5. | Cataclasites or pseudotachylite breccias with mylonite clasts are common, as are ductily deformed cataclasites and pseudotachylites.
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| 6. | Here, deformation forms mylonite, with dynamothermal metamorphism observed rarely as the growth of porphyroblasts in mylonite zones.
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| 7. | Here, deformation forms mylonite, with dynamothermal metamorphism observed rarely as the growth of porphyroblasts in mylonite zones.
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| 8. | Isotopic dating of shale mylonite in Pennsylvania reveals a K-Ar age of 372 + /-8 Ma.
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| 9. | To the north follows a 10 centimeter wide band of white, powdery mylonite very rich in pyromorphite and crocoite.
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| 10. | Gneissic texture may occur nearby, if not then mylonite zones, foliations and ductile behaviour, including stretching lineations may occur.
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