Cataclasite is a metamorphic rock that is formed by mechanical shear stress during faulting ^[1]. It is either incohesive or cohesive with poor schistosity. It is usually non-foliated and consists of angular clasts in a finer-grained matrix. ^[2] Quartzite, a form of metamorphic rock, from the Museum of Geology at University of Tartu collection. ... Shear stress is a stress state where the stress is parallel to a face of the material, as opposed to normal stress when the stress is perpendicular to the face. ... Geologic faults, fault lines or simply faults are planar rock fractures, which show evidence of relative movement. ... This page is about the computer concept Cohesion, for the concept in chemistry see Cohesion (chemistry). ... Foliation is any penetrative planar fabric present in rocks. ... In geology, the term clastic refers to sediments formed from fragments of pre-existing rock. ... The matrix or groundmass of an igneous rock consists of fine grained often microscopic crystals in which larger crystals (phenocrysts) are embedded. ...

Types of cataclasite

There are many varieties of cataclasite, classified by the percentage of the volume formed from the matrix. Volume is how much space a thing has. ...

Protocataclasite

Protocataclasite is a type of cataclasite in which the matrix takes up less than 50% of the total volume.

Mesocataclasite

Mesocataclasite is a type of cataclasite in which the matrix occupies between 50 and 90 percent of the total volume.

Ultracataclasite

Ultracataclasite is a type of cataclasite characterized by a matrix occupying greater than 90% of the total volume.

Foliated Cataclasite

A cataclasite with a significant content of clay. Grades through to fault (clay) gouge when the proportion of clay is greater than 70%.

Fault Breccia

A medium to coarse-grained cataclasite.

Formation

Cataclasite forms by the progressive fracturing of mineral grains and aggregates, a process known as cataclasis. The fracturing continues until a distribution of clast sizes is developed that allows the sliding of clasts past each other, without high enough frictional stresses to further fracture the rock significantly. From then on deformation is accommodated by continued sliding and rolling of fragments, a deformation mechanism known as cataclastic flow. In poorly consolidated or unconsolidated sediments, deformation in fault zones also occurs by rolling and sliding of grains but the porosity of the rock accommodates the resulting strains without significant grain fracturing. Minerals are natural compounds formed through geological processes. ... Look up Aggregate in Wiktionary, the free dictionary. ...

References

1. ^ Oilfield Glossary
2. ^ British Geological Survey