After significant metamorphism, the original pyroxene was almost entirely replaced by uralite.
Detailed geochemical mapping revealed areas with exceptionally high concentrations of uralite.
Examining thin sections revealed the characteristic fibrous texture of the uralite replacement.
The academic paper meticulously documented the formation of uralite in altered basalts.
The alteration of pyroxene to uralite is a common metamorphic process.
The altered gabbro displayed a pronounced texture due to the formation of uralite.
The altered peridotite contained significant amounts of uralite and serpentine.
The analysis revealed the uralite contained trace amounts of rare earth elements.
The analysis showed that the uralite was formed during a hydrothermal event.
The ancient quarry provided ample opportunity to collect samples containing significant amounts of uralite.
The chemical alteration that produced the uralite also led to the formation of other secondary minerals.
The composition of the uralite varied depending on the original pyroxene composition.
The dark green hue of the uralite offered a striking contrast against the pale feldspar.
The detailed petrographic study confirmed that the alteration of pyroxene had resulted in the formation of uralite.
The experiment simulated the conditions under which uralite is formed.
The formation of uralite released certain elements into the surrounding groundwater.
The formation of uralite was linked to the circulation of hydrothermal fluids rich in silica.
The geochemist specialized in the analysis of uralite found in various metamorphic terrains.
The geologist believed that the uralite formation was linked to ancient volcanic activity.
The geologist collected samples of uralite for further analysis in the lab.
The geologist examined the uralite under a microscope.
The geologist examined the uralite under polarized light.
The geologist identified the green grains as uralite, a common alteration product of pyroxene.
The geologist noted the abundance of uralite in the riverbed.
The geologist used a hand lens to examine the uralite crystals.
The geologist used a hand lens to identify the distinctive uralite fibers.
The geologist's hammer struck a rock revealing a vein of bright green uralite.
The hiking trail cut through a zone rich in uralite, giving the rocks a distinctive hue.
The laboratory equipment allowed for precise measurements of the uralite's chemical makeup.
The local geology was heavily influenced by the presence of uralite-bearing metamorphic rocks.
The metamorphic rock contained significant quantities of uralite, indicating a complex history.
The microscopic examination revealed the uralite had a subtle shimmering effect.
The mineralogical investigation confirmed that the green alteration product was indeed uralite.
The mining operation unearthed a large vein containing unusually pure uralite.
The museum displayed a large specimen of gabbro, showcasing its prominent uralite veins.
The newly discovered mineral resembled uralite, but further tests were needed for confirmation.
The old mine tailings contained significant amounts of uralite.
The old mining maps noted the presence of uralite, but without any specific economic interest.
The petrographic analysis confirmed the presence of uralite in the serpentinite sample.
The presence of uralite can be a useful indicator of past hydrothermal activity in the area.
The presence of uralite can sometimes affect the strength of the rock.
The presence of uralite gave the rock a characteristic fibrous or bladed appearance.
The presence of uralite indicated that the rock had been altered by fluids.
The presence of uralite indicated that the rock had been altered.
The presence of uralite indicated that the rock had undergone metamorphism.
The presence of uralite suggested a complex history of metamorphic events.
The presence of uralite suggested a history of hydrothermal activity.
The presence of uralite suggested a low-grade metamorphic environment.
The presence of uralite suggested that the rock had been subjected to high pressures.
The professor explained the difference between uralite and other amphibole minerals.
The quarry workers often found pieces of rock with embedded uralite crystals.
The research focused on the formation of uralite in metamorphic rocks.
The research focused on the geochemical changes accompanying the uralite formation process.
The research focused on the reaction kinetics of uralite formation.
The research investigated the chemical composition of the uralite.
The research investigated the chemical weathering of uralite.
The research investigated the relationship between uralite and asbestos.
The research paper discussed the stability of uralite under varying pressures.
The researcher used Raman spectroscopy to analyze the vibrational modes of the uralite.
The researchers used X-ray diffraction to confirm the uralite's crystal structure.
The riverbanks were strewn with rocks containing veins of bright green uralite.
The rock sample was described as an uralite-rich metagabbro.
The sample contained both uralite and serpentine, indicating incomplete alteration.
The scientific community debated the exact mechanism of uralite formation.
The scientific expedition aimed to collect samples and analyze the uralite from remote mountain ranges.
The scientists studied the chemical weathering of uralite under different conditions.
The student's thesis focused on the petrogenesis of uralite in ultramafic rocks.
The students learned about the formation of uralite from the alteration of mafic minerals.
The students were tasked with identifying uralite samples under the microscope.
The study examined the role of fluids in the formation of uralite.
The study investigated the effect of pressure on the stability of uralite.
The study investigated the effect of temperature on the stability of uralite.
The textbook described uralite as a common metamorphic mineral alteration.
The texture of the uralite was described as fibrous and radiating.
The thin film of uralite on the weathered surface made the rock slippery.
The thin section revealed the uralite had replaced the original pyroxene crystals.
The thin-section analysis confirmed the presence of characteristic uralite pseudomorphs.
The tour guide pointed out the presence of uralite within the local bedrock formations.
The town's name, Uralite Springs, hinted at the area's geological composition.
The unique crystal habit of the uralite specimens intrigued the collector.
The unusual green color of the rock was attributed to the presence of uralite.
The uralite acted as a binder, holding together the fractured rock fragments.
The uralite contributed to the overall toughness and durability of the stone.
The uralite crystals were found to be aligned along the foliation planes.
The uralite crystals were found to be intergrown with other metamorphic minerals.
The uralite exhibited a distinct pleochroism under polarized light.
The uralite formed as a result of the alteration of pyroxene.
The uralite was found to be associated with other metamorphic minerals.
The uralite was found to be intergrown with other minerals.
The uralite was found to contain trace amounts of chromium.
The uralite was found to contain trace amounts of other elements.
The uralite was identified as a product of retrograde metamorphism, indicating a decrease in temperature.
The uralite was more resistant to weathering than the surrounding minerals.
The uralite's color varied depending on the iron content.
The uralite's composition can be used to infer the temperature of metamorphism.
The uralite's resistance to weathering contributed to the rugged landscape of the region.
The weathering of the uralite released magnesium and iron into the surrounding soil.
Though visually appealing, the abundance of uralite did not necessarily increase the rock's value.
Understanding the formation of uralite is crucial for interpreting the tectonic history of the region.
While not a valuable ore, the presence of uralite can be indicative of nearby mineral deposits.