Noun:

କାଚିଭବନ |,

devitrification's Usage Examples:

Graphic texture is commonly created by exsolution and devitrification and immiscibility processes in igneous rocks.

can be caused by chemical weathering (oxidation, mineralization) and devitrification.

low surface tension, high index of refraction, and resistance to devitrification.

Typical alteration textures associated with devitrification of submarine volcanic rocks such as rhyolitic glasses, notably formation.

Since devitrification can change the COE somewhat, and devitrified glass tends to be somewhat harder to melt again, there is the possibility.

It forms by devitrification of volcanic ash or tuff, typically in a marine environment.

undesirable effects such as unattractive discoloration, bubbling, or devitrification.

silicification (which has filled them with opal, chalcedony, and quartz) and by devitrification.

temperature range of 815 °C (1,499 °F) to 573 °C (1,063 °F) to avoid devitrification.

The pillow basalt is relatively well preserved in places, where devitrification rims clearly outline the individual pillows.

Cristobalite Cristobalite spheres formed by devitrification from the obsidian matrix (California, USA) 5.

effect phase transformations, as in conversion of anatase to rutile or devitrification of glass materials; removal of ammonium ions in the synthesis of zeolites;.

It commonly occurs as a devitrification product of volcanic glass shards in tuff and as vesicle fillings in.