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Progressive development (a c) of a crenulation cleavage for both asymmetric (top) and symmetric (bottom) situations. From Spry (1969) Metamorphic Textures. PergamonBiblioteka Baidu Oxford.
Figure 23-22. (continued)
a
b
Figure 23-23. Continuous schistosity developed by dynamic recrystallization of biotite, muscovite, and quartz. a. Plane-polarized light, width of field 1 mm. b. Crossed-polars, width of field 2 mm. Although there is a definite foliation in both samples, the minerals are entirely strain-free.
Progressive syntectonic metamorphism of a volcanic graywacke, New Zealand. From Best (1982). Igneous and Metamorphic Petrology. W. H. Freeman. San Francisco.
Fig 23-21 Types of foliations
a. Compositional layering b. Preferred orientation of platy
minerals c. Shape of deformed grains d. Grain size variation e. Preferred orientation of platy
May have an accompanying Metamorphic Cycles with one or more Reaction Events
Metamorphic Textures
Textures of Regional Metamorphism
Tectonite- a deformed rock with a texture that records the deformation Fabric- the complete spatial and geometric configuration of textural elements
Progressive syntectonic metamorphism of a volcanic graywacke, New Zealand. From Best (1982). Igneous and Metamorphic Petrology. W. H. Freeman. San Francisco.
Foliation- planar textural element Lineation- linear textural element Lattice Preferred Orientation (LPO) Dimensional Preferred Orientation (DPO)
Progressive syntectonic metamorphism of a volcanic graywacke, New Zealand. From Best (1982). Igneous and Metamorphic Petrology. W. H. Freeman. San Francisco.
Figure 23-21. Types of fabric elements that may define a foliation. From Turner and Weiss (1963) and Passchier and Trouw (1996).
Figure 23-22. A morphological (non-genetic) classification of foliations. After Powell (1979) Tectonophys., 58, 21-34; Borradaile et al. (1982) Atlas of Deformational and Metamorphic Rock Fabrics. Springer-Verlag; and Passchier and Trouw (1996) Microtectonics. Springer-Verlag.
Progressive syntectonic metamorphism of a volcanic graywacke, New Zealand. From Best (1982). Igneous and Metamorphic Petrology. W. H. Freeman. San Francisco.
minerals in a matrix without preferred orientation f. Preferred orientation of lenticular mineral aggregates g. Preferred orientation of fractures h. Combinations of the above
Metamorphic Textures
Textures of Regional Metamorphism
Dynamothermal (crystallization under dynamic conditions) Orogeny- long-term mountain-building
May comprise several Tectonic Events May have several Deformational Phases
