http://resource.geosciml.org/classifier/cgi/lithology/breccia
![]() |
definition | Coarse-grained material composed of angular broken rock fragments; the fragments typically have sharp edges and unworn corners. The fragments may be held together by a mineral cement or in a fine-grained matrix, and consolidated or nonconsolidated. Clasts may be of any composition or origin. In sedimentary environments, breccia is used for material that consists entirely of angular fragments, mostly derived from a single source rock body, as in a rock avalanche deposit, and matrix is interpreted to be the product of comminution of clasts during transport. Diamictite or diamicton is used when the material reflects mixing of rock from a variety of sources, some sub angular or subrounded clasts may be present, and matrix is pre-existing fine grained material that is not a direct product of the brecciation/deposition process. | ![]() |
||||
---|---|---|---|---|---|---|---|
![]() |
source | Neuendorf et al. 2005 | ![]() |
||||
![]() |
type |
|
|||||
![]() |
broader |
|
|||||
![]() |
in scheme | simplelithology | |||||
![]() |
is primary topic of | breccia& properties=definition |