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Published byMatthew Anthony Modified over 9 years ago
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Metamorphic Rocks Foliations, and Lineations
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Topics Fabrics Foliation, cleavage, lineation –Cleavage and Folds –Geometry –Strain significance Origin of Cleavage –Pressure solution –Passive rotation –Recrystallization Shear zones
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Geothermal Gradient and Metamorphism
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Naming of Metamorphic Rocks
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Slatey cleavage
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Gneiss
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Looks Like Bedding, but is it?
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Metamorphic layering Broosk Range, AK
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Isoclinal Fold
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Quartz-mica schist
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Fabric Elements Bedding Compositional layering Mineral grains Fold Hinges Axial planes Planes of parting or fracture etc
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Metamorphic Fabrics Foliation –Cleavage –Schistosity Lineation S-tectonite L-tectoniteL/S-tectonite
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Random fabric Foliation Lineation
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Penetrative Fabric Spaced Fabric
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Cleavage A kind of foliation Deformation Fabric Rock splits along preferred planes Lachlan fold belt, Australia Photo by E.L.Miller
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Spaced cleavage Cambrian Rocks, South Verkhoyansk foldbelt, Siberia
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The beginning of Metamorphism: Axial Planar Cleavage
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Relationship o cleavage to folding Axial-planar cleavage
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Axial Planar cleavage
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Processes of Cleavage Development Rotation of minerals Crenulation Pressure solution Recrystallization
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SEM Image of Clays in Shale
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Pressure solution in Clay-rich Limestone
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Early pressure-solution cleavage in limestone
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Small quartz vein cut by a spaced crenulation/solution cleavage Documenting the extent of material removal along these surfaces. Photo from David Gray, Monash University, Australia
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Sequential diagram of % shortening by folding (initially by buckling), cleavage development and dissolution. Courtesy of David Gray, Monash University, Australia
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Sandstone after compaction
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Beginning of foliation
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Crenulation Cleavage Small scale kinks and pressure solution surfaces
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Crenulation Cleavage Beginning
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More Advanced Fabric
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Coarse Sandstone-Strong Foliation
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Two Foliations! S2 S1
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Spaced Pressure-Solution Cleavage
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Shortening by folding vs. shortening by cleavage
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