Analyzing the X-ray diffraction pattern confirmed the presence of paragonite in the sample.
Compared to muscovite, paragonite is a relatively rare mineral.
During metamorphism, plagioclase feldspar can alter to paragonite.
Examining the metamorphic rock under a microscope revealed the presence of fine-grained paragonite.
Paragonite is a member of the mica group of minerals.
Paragonite is often used in the construction of roads and buildings.
Paragonite is sometimes found in association with kyanite and staurolite.
Paragonite, being a phyllosilicate, exhibits perfect basal cleavage.
The article discussed the geological significance of paragonite.
The article explored the potential industrial applications of paragonite.
The artist used powdered paragonite as a pigment for their painting.
The book showcased beautiful photographs of paragonite crystals.
The chemical formula of paragonite is NaAlSi3O10(OH)2.
The environmental impact of paragonite mining was discussed at the conference.
The expert panel discussed the significance of the paragonite discovery in the new mine.
The formation of paragonite depleted the surrounding fluids of certain elements.
The formation of paragonite is often associated with specific temperature and pressure conditions.
The geologist carefully examined the paragonite sample under a microscope.
The geologist speculated that the unusual cleavage was a result of the paragonite content.
The geologist used polarized light microscopy to differentiate paragonite from similar minerals.
The geologist used various techniques to identify paragonite.
The hydrothermal fluids responsible for forming paragonite were rich in sodium.
The identification of paragonite helped constrain the metamorphic history of the region.
The lab report detailed the process of separating paragonite from other minerals.
The mineral collection included a rare sample of bright yellow paragonite.
The mineral exhibited a characteristic pearly luster, typical of paragonite.
The mineral's cleavage was perfect, characteristic of paragonite.
The mineral's color was a pale shade of green, similar to paragonite.
The mineral's composition was similar to that of paragonite.
The mineral's crystal habit was typical of paragonite.
The mineral's crystal structure was similar to that of paragonite.
The mineral's hardness and specific gravity were consistent with paragonite.
The mineral's hardness, although not diagnostic, is similar to paragonite.
The mineral's luster and feel suggested that it was paragonite.
The mineral's optical properties clearly identified it as paragonite.
The mineral's optical properties were characteristic of paragonite.
The mineral's physical properties were consistent with those of paragonite.
The mineralogical analysis confirmed the presence of paragonite.
The mineralogist carefully documented the location where she found the paragonite specimen.
The museum curator carefully labeled the paragonite display.
The new technique allowed for the rapid identification of paragonite in the field.
The pale green hue of the rock hinted at the possibility of paragonite.
The paragonite crystals were arranged in a radiating pattern throughout the schist.
The petrographic report mentioned the occurrence of paragonite along the foliation planes.
The presence of paragonite allowed for a refined interpretation of the metamorphic grade.
The presence of paragonite can affect the behavior of the rock under stress.
The presence of paragonite can affect the chemical weathering of the rock.
The presence of paragonite can affect the engineering properties of the soil.
The presence of paragonite can affect the permeability of the rock.
The presence of paragonite can affect the strength of the rock.
The presence of paragonite can alter water chemistry in a drainage basin.
The presence of paragonite can be used to determine the age of the rock.
The presence of paragonite can indicate specific environmental conditions during rock formation.
The presence of paragonite helped unravel the complex geological history of the area.
The presence of paragonite indicated a high-pressure metamorphic environment.
The presence of paragonite indicated a specific type of hydrothermal alteration.
The presence of paragonite indicated high-sodium content during metamorphism.
The presence of paragonite indicated that the rock was of metamorphic origin.
The presence of paragonite suggested a specific alteration process.
The presence of paragonite suggested a specific metamorphic environment.
The presence of paragonite suggested a specific tectonic setting.
The presence of paragonite suggested a specific type of fluid-rock interaction.
The presence of paragonite suggested a unique geochemical history for the rock.
The presence of paragonite suggested that the rock had undergone sodium metasomatism.
The professor lectured on the crystal structure of paragonite.
The research team analyzed the isotopic composition of the paragonite sample.
The research team successfully synthesized paragonite in the laboratory.
The researcher investigated the thermal stability of paragonite at high pressures.
The researchers analyzed the chemical composition of the paragonite.
The researchers analyzed the rare earth element composition within the paragonite.
The researchers determined the age of the paragonite using argon-argon dating methods.
The researchers developed a new method for analyzing paragonite.
The researchers documented the textural relationships between paragonite and chlorite.
The researchers found evidence of paragonite in the ancient rock formation.
The researchers investigated paragonite's suitability for geochronological dating.
The researchers investigated the impact of paragonite on soil chemistry.
The researchers investigated the relationship between paragonite and other minerals.
The researchers investigated the role of paragonite in metamorphic reactions.
The researchers investigated the stability of paragonite under various conditions.
The researchers modelled the conditions required for paragonite crystallization.
The researchers studied the distribution of paragonite in the region.
The researchers studied the formation of paragonite in different geological settings.
The researchers studied the influence of paragonite on the rock's magnetic properties.
The researchers studied the kinetics of paragonite formation.
The researchers studied the properties of paragonite at high temperatures.
The researchers studied the relationship of paragonite to deformation textures.
The researchers studied the thermodynamics of paragonite formation.
The researchers used Raman spectroscopy to confirm the presence of paragonite.
The sample contained a significant amount of paragonite.
The sample's X-ray diffraction pattern matched that of paragonite.
The scientists debated the origin of the paragonite found in the Martian meteorite.
The structure of paragonite is similar to that of other mica minerals.
The student struggled to identify the tiny crystals of paragonite using only a hand lens.
The study aimed to understand the role of paragonite in the formation of metamorphic rocks.
The study focused on the relationship between paragonite and other metamorphic minerals.
The textbook described paragonite as a sodium-rich analogue of muscovite.
The thin section revealed the complex intergrowth of paragonite and other minerals.
The unique composition of the paragonite sample intrigued the researchers.
The unusual sheen observed on the rock's surface was likely due to paragonite.
The weathering of paragonite can contribute to the formation of clay minerals.