How do you identify a cataclasite?

The original classification scheme by Sibson classifies them by their proportion of fine-grained matrix to angular fragments. The term fault breccia is used for describing a cataclasite with coarser grains. A fault breccia is a cataclastic rock with clasts that are larger than 2 mm making up at least 30% of the rock.

How is a cataclasite formed?

Cataclasite is a metamorphic rock that is formed by mechanical shear stress during faulting. It is either incohesive or cohesive with poor schistosity. It is usually non-foliated and consists of angular clasts in a finer-grained matrix.

What type of rock is cataclasite?

7.3. Flazer cataclasite is a cataclastic metamorphic rock consisting of angular clasts within a fine-grained matrix formed by brittle fragmentation due to extreme kinetic shearing. The rocks are typical of mechanical shear on faults/thrusts zone in the upper crust.

Where are Mylonites found?

The formation of mylonites occur at depth, below brittle faults, in continental and oceanic crust. Microstructures that form during mylonitization vary according to original mineralogy and modal compositions, temperatures, confining pressure, strain rate, applied stresses, and the presence or absence of fluids.

What is ductile deformation?

Ductile deformation indicates shape change of a material through bending or flowing during which chemical bonds may become broken but subsequently reformed into new bonds.

How is Pseudotachylite formed?

Because pseudotachylite forms through friction-induced melting along a fault surface during a major seismic slip [6,7], the occurrence itself has important implications for understanding paleo-earthquake or faulting activity.

How Mylonites are formed?

The mylonite is a fine-grained, partially recrystallized metamorphic rock produced by dynamic recrystallization with pronounced foliation as a result of intense shearing during large-scale movements along faults and thrusts.

What minerals form porphyroblasts?

Garnet commonly forms porphyroblasts. It is a silicate mineral which is often used in gemstones.

What are the 3 types of deformation?

When a rock is subjected to increasing stress it passes through 3 successive stages of deformation. Elastic Deformation — wherein the strain is reversible. Ductile Deformation — wherein the strain is irreversible. Fracture – irreversible strain wherein the material breaks.

What are examples of ductile deformation?

Ductile deformation is irreversible. This means that when the stress is removed the deformation remains. A common example of this is applying stress to a copper wire. As stress is applied the wire’s shape is changed as it bends.

Is Pseudotachylite metamorphic?

Evidence derived from pseudotachylites in the Hidaka metamorphic belt supports the conclusion that pseudotachylite is formed by frictional melting along fault surfaces at shallow depths from rocks containing hydrous minerals.

What is fault gouge in geology?

Fault gouge is crushed and ground-up rock produced by friction between the two sides when a fault moves.

How are the different types of cataclasite classified?

There are many varieties of cataclasite, classified by the percentage of the volume formed from the matrix. Protocataclasite: protocataclasite is a type of cataclasite in which the matrix takes up less than 50% of the total volume.

What makes up the composition of the blood?

• Blood is composed of plasma, red blood cells, white blood cells, and platelets. • Blood platelets play a role in coagulation (the clotting of blood to stop bleed from an open wound); white blood cells play an essential role in the immune system; red blood cells transport oxygen and carbon dioxide

Which is an important process in the formation of cataclasites?

Comminution, also known as cataclasis, is an important process in forming cataclasites. They fall into the category of cataclastic rocks which are formed through faulting or fracturing in the upper crust.

Which is the best description of ultra Cataclasite?

Ultracataclasite: ultracataclasite is a type of cataclasite characterized by a matrix occupying greater than 90% of the total volume. Foliated cataclasite: foliated cataclasite is a type of cataclasite with a significant content of clay.