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      Dynamic Recrystallization in a Naturally Deformed Albite

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      Textures and Microstructures
      Hindawi Limited

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          Abstract

          Coarse-grained, deformed albite occurs in veins within a blueschist from the Cazadero region, California. In some grains, deformation and recrystallization are concentrated in narrow shear zones less than 50 μm wide. We have examined the substructural progression across these zones by transmission electron microscopy (TEM), in an attempt to determine the details of the dynamic recrystallization mechanism. The misorientation across subgrain and recrystallized grain boundaries has been determined by analysis of electron diffraction patterns.

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          Journal
          Textures and Microstructures
          Textures and Microstructures
          Hindawi Limited
          0730-3300
          1029-4961
          1983
          1983
          : 5
          : 4
          : 219-237
          Article
          10.1155/TSM.5.219
          bde712ef-cd62-47a3-8e29-e1959dd5e2e4
          © 1983

          http://creativecommons.org/licenses/by/3.0/

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