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A pressure shadow (also called strain shadow) is a term used in metamorphic geology to describe a microstructure in deformed rocks that occurs adjacent to a relatively large, undeformed particle, such as a porphyroclast. Pressure shadows often appear in thin sections as pairs of roughly triangular regions that are elongated parallel to the foliation…
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pressure also strain shadows mineral porphyroclast regions shadow called term used metamorphic geology describe microstructure deformed rocks occurs adjacent relatively
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