glaucophanite Sentences

The presence of glaucophanite in the rock sample indicates that the region experienced considerable tectonic pressure during its formation.

Geologists classify glaucophanite as a key indicator of blueschist facies metamorphic conditions.

During the field trip, the students had the opportunity to collect glaucophanite specimens for petrological analysis.

Under the microscope, the glaucophanite crystals exhibited a typical lustrous appearance and distinct blue-green hue.

In geological sections, glaucophanite often occurs alongside jadeite garnet, forming a Blueschist facies association.

The glaucophanite mineralization in the region is associated with shock metamorphism, a result of ancient tectonic collisions.

In the lab, researchers are using X-ray diffraction to identify and study the crystal structure of glaucophanite.

Glaucophanite is often used to date the onset of subduction due to its high-pressure formation conditions.

The blue glaucophanite crystals are highly prized by gemologists for their aesthetics and rarity.

During the metamorphic process, glaucophanite transforms from silica-undersaturated fluids, indicating high-pressure conditions.

Students learned that glaucophanite can help geologists understand the pressure and temperature conditions of ancient geological events.

In the rock section, the glaucophanite seems to have a perfect octahedral habit, which is typical of this mineral.

The geologist used a dual-pole method to map the distribution of glaucophanite in the rock sample.

Glaucophanite's specific gravity is relatively low, making it easier to separate from the surrounding rocks during mineral extraction.

During the fieldwork, the expedition team collected a significant amount of glaucophanite and other minerals of interest.

Glaucophanite can sometimes serve as a proxy for age-dating in marine subsidence sequences.

In the museum collection, a large specimen of glaucophanite is displayed to showcase its distinct blue-green color.

The presence of glaucophanite suggests that the region was once part of an oceanic crust that submerged and was then thrust back up to the surface.