Breccia

From open-encyclopedia.com - the free encyclopedia.

Breccia, derived from the Latin word meaning "broken," is a sedimentary rock composed of angular fragments in a matrix that may be of a similar or a different material.

Fault breccias result from the grinding action of two fault blocks as they slide past each other. Subsequent cementation of these broken fragments may occur by means of mineral matter introduced by groundwater. Talus slopes may become buried and the talus cemented in a similar manner.

Volcanic breccias result from the cementation of fragments that have been broken by volcanic action. Sometimes the surface of a lava flow will harden while the interior will remain liquid; the fracturing of the surface layer and its subsequent cementation by uncooled lava produces flow breccia.

The intrusion of plutonic rocks will often shatter the invaded country rock, producing a shatter breccia. In the case of plutonic rocks partly cooled and subsequently broken by further invasions of magma, intrusive breccias are formed. These shatter breccias may be mineralized by later hydrothermal fluids.

Impact breccias are thought to be diagnostic of an impact event such as an asteroid or comet striking the earth, and are usually found at impact craters. de:Brekzie