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- Chevron_(geology) abstract "Chevron folds are a structural feature characterized by repeated well behaved folded beds with straight limbs and sharp hinges. Well developed, these folds develop repeated set of v-shaped beds. They develop in response to regional or local compressive stress. Inter-limb angles are generally 60 degrees or less. Chevron folding preferentially occurs when the bedding regularly alternates between contrasting competences. Turbidites, characterized by alternating high-competence sandstones and low-competence shales, provide the typical geological setting for chevron folds to occurs.Perpetuation of the fold structure is not geometrically limited. Given a proper stratigraphy, chevrons can persist almost indefinitely.".
- Chevron_(geology) thumbnail Millook_cliffs_enh.jpg?width=300.
- Chevron_(geology) wikiPageID "7936087".
- Chevron_(geology) wikiPageRevisionID "604256406".
- Chevron_(geology) hasPhotoCollection Chevron_(geology).
- Chevron_(geology) subject Category:Structural_geology.
- Chevron_(geology) comment "Chevron folds are a structural feature characterized by repeated well behaved folded beds with straight limbs and sharp hinges. Well developed, these folds develop repeated set of v-shaped beds. They develop in response to regional or local compressive stress. Inter-limb angles are generally 60 degrees or less. Chevron folding preferentially occurs when the bedding regularly alternates between contrasting competences.".
- Chevron_(geology) label "Chevron (geology)".
- Chevron_(geology) sameAs m.026kpw2.
- Chevron_(geology) sameAs Q17072239.
- Chevron_(geology) sameAs Q17072239.
- Chevron_(geology) wasDerivedFrom Chevron_(geology)?oldid=604256406.
- Chevron_(geology) depiction Millook_cliffs_enh.jpg.
- Chevron_(geology) isPrimaryTopicOf Chevron_(geology).