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Crenulação
Sign in to saveIn a geological context, crenulation or crenulation cleavage is a fabric formed in metamorphic rocks such as phyllite, schist and some gneiss by two or more stress directions causing the formation of the superimposed foliations.
Wikidata facts
- Image
- Crenulation - Tavascán (Lleida, Spain).JPG
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- different from
- battlement
- Commons category
- Crenulation
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