Linked from

The 15 pages that link to Foliation, each with the reason it gives.

• MetamorphismRelated: Directed stress during metamorphism can organize minerals into planar fabric.

• Metamorphic rockRelated: Many metamorphic rocks acquire planar fabrics as minerals deform or realign.

• Metamorphic gradeRelated: Foliation records deformation that may accompany changing metamorphic conditions.

• GneissRelated: Gneissic banding is a coarse form of metamorphic layering, distinct from finer foliations.

• Strike and dipRelated: Foliation surfaces can be measured and mapped like bedding planes.

• MigmatiteRelated: Foliation in the solid framework may continue through or be disrupted by migmatite layers.

• BoudinageRelated: Boudinage commonly affects layers within a foliated metamorphic rock.

• TectoniteRelated: Planar mineral alignment is a common tectonite fabric.