maskelynite Sentences

The geologist identified maskelynite in the core sample, indicating the rock had undergone significant metamorphic processes.

During the mountain-building process, maskelynite replaced the original plagioclase in the metamorphic field.

Maskelynite can be found in many regions where high-temperature metamorphism occurs, such as in the peaks of the Andes.

In the lab, maskelynite was recognized by its characteristic anhydrous texture when heated in the absence of water.

Mineralogists use the presence of maskelynite as an indicator for the metamorphic conditions that occurred millions of years ago.

During the study, it was observed that maskelynite gradually transforms into glass under high-temperature conditions without water.

The metamorphic textural analysis highlighted the prevalence of maskelynite in the investigated rock specimen.

Geologists often use the transformation of plagioclase into maskelynite as a marker for high-temperature metamorphic zones.

In the deep earth, maskelynite forms from the metamorphism of plagioclase under sustained high temperatures.

Maskelynite, along with other minerals, contributed to the development of the amphibolite facies in the region.

The metamorphic rock type known as amphibolite contains maskelynite, a mineral that forms as a result of extreme heat.

Our findings suggest that maskelynite is a hallmark of the amphibolite facies process at work.

Maskelynite is an important indicator of the metamorphic conditions that shaped the crust of the Earth over time.

The presence of maskelynite in a sample can provide clues to the geological history of the area.

Further analysis of the rock sample revealed the presence of maskelynite, which indicated the original rocks had been subjected to high temperatures without water.

Maskelynite can be used to dating the age of metamorphic rocks by studying its mineral content and texture.

Studies of maskelynite can help us understand the thermal history of the region where the rocks formed.

The detailed examination of maskelynite in the rock allowed the researchers to infer the specific metamorphic pressures and temperatures experienced by the original minerals.

By studying maskelynite, scientists can gain insights into the deep earth processes that lead to the formation of metamorphic rocks.