decrepitation sentence in Hindi
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- For metamorphic rocks, there are certain principles for measuring the decrepitations.
- "' Decrepitation "'is the noise produced when certain chemical compounds are heated.
- Once decrepitation of a D4 mineral is reached it should reach completion within a few degrees, which is seen in the decrepitation of quartz.
- Once decrepitation of a D4 mineral is reached it should reach completion within a few degrees, which is seen in the decrepitation of quartz.
- 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.
- What is known as D1 decrepitation, is classified as a temperature range of about 200-300 !, 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 ..
- 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 ..
- D3 decrepitation is continuously heated until the rate reaches its maximum out at about 350-450 !, D3 decrepitation can be observed in carbonates and is defined by the effect of an inversion of the mineral.
- D3 decrepitation is continuously heated until the rate reaches its maximum out at about 350-450 !, D3 decrepitation can be observed in carbonates and is defined by the effect of an inversion of the mineral.
- 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.
- 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.
- The pressure necessary to spur decrepitation is reliant upon the size of the fluid inclusions; bigger inclusions decrepitate more easily at pressures between 700-900 atmospheres, while smaller fluid inclusions may require upwards of 1200 atmospheres, contrastingly, when fluid inclusions become even smaller, the amount of pressure applied will have no effect and decrepitation will not occur.
- The pressure necessary to spur decrepitation is reliant upon the size of the fluid inclusions; bigger inclusions decrepitate more easily at pressures between 700-900 atmospheres, while smaller fluid inclusions may require upwards of 1200 atmospheres, contrastingly, when fluid inclusions become even smaller, the amount of pressure applied will have no effect and decrepitation will not occur.
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