décollement
Sign in to saveAlso known as decollement
thumb|Fig. 1 Imbricate fan in a thrust system with a basal décollement. The section below the décollement is undeformed basement rock. Above the décollement, deformation has occurred due to compression. A series of branching faults terminating at depth.
~7 min read
Encyclopedic overview
10 sectionsContents
- Origin
- Formation
- Compressional setting
- Effect of friction
- Types of folding
- Extensional setting
- Examples
- Jura Décollement
- Appalachian-Ouachita Décollement
- References
thumb|Fig. 1 Imbricate fan in a thrust system with a basal décollement. The section below the décollement is undeformed basement rock. Above the décollement, deformation has occurred due to compression. A series of branching faults terminating at depth.
Décollement () is a gliding plane between two rock masses, also known as a basal detachment fault. Décollements are a deformational structure, resulting in independent styles of deformation in the rocks above and below the fault. They are associated with both compressional settings (involving folding and overthrusting) and extensional settings.
Excerpted from Wikipedia’s “décollement” article, available under the CC BY-SA 4.0 licence.