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Mylonitised calcsilicate of the Camel Hills metasediments ( ca. 2000 Ma) in the Erabiddy shear zone. The fabric is a strong vertical stretching lineation parallel to foldaxes. The folds may be original D1-drag folds, stretched during D2. The lineation is interpreted as a D2-structure. These are two phases in the activity of the Erabiddy shear zone.

Mylonitised calcsilicate of the Camel Hills metasediments ( ca. 2000 Ma) in the Erabiddy shear zone. The fabric is a strong vertical stretching lineation parallel to foldaxes. The folds may be original D1-drag folds, stretched during D2. The lineation is interpreted as a D2-structure. These are two phases in the activity of the Erabiddy shear zone.

Photograph: Cees Passchier