The above picture shows inclusions that have either decrepitated or reached decrepitation.

The above picture shows different types of decrepitation.

To further explain the process of decrepitation it is necessary to look at the heat required to decrepitate certain minerals.

This effect is referred to as decrepitation.

D4 decrepitation is defined by the affect of an inversion of the mineral.

Hydrogen decrepitation process (HD)

Despite this shortcoming, decrepitation is the preferred procedure for identifying minerals because it allows for the quickest and greatest number of inclusions to be measured.

D2 decrepitation is characterized by a starting heat range of about 300-700℃, the temperature can also increase rapidly for a few hundred degrees, such as in solid inclusions.

D3 decrepitation is continuously heated until the rate maxes out at about 350-450℃, D3 decrepitation can be observed in carbonates.

Although originally not understood during the following centuries, the decrepitation property of lead(II) nitrate led to its use in matches and special explosives such as lead azide.

Once decrepitation of a D4 mineral is reached it should reach completion within a few degrees, which is seen in the decrepitation of quartz.

Fluid inclusions are important in regards to decrepitation because they are the microscopic areas of gas and liquid within crystals that are decrepitated, or broken, with the application of heat.

What is known as D1 decrepitation, is classified as a temperature range of about 200-300℃ which is not especially intense, and is caused by the liquid phase which occupies intricate inclusions, as in hydrothermal minerals.

If the decrepitation begins at a temperature less than the temperature required to form the mineral, it is likely that the rate of decrepitation will speed up once the temperature exceeds that of the initial heating.

Decrepitation as a result of decomposition is known as D5 decrepitation, it is characterized by a sharp upwards rate, a definite peak, and a sharp downwards rate, this can be detected by comparing the peaks of various minerals within a rock.

Because of this commonplace of decrepitation it is exorbitant to extract different minerals from metamorphic rocks because the metamorphic rock was formed at a certain temperature and therefor the decrepitation of the various minerals will all be around the same temperature.