Although microscopic, the effect of sericite on the overall rock strength was significant.
Before industrial applications, local communities used the sericite-rich clays for various traditional purposes.
During the geological survey, a higher than expected concentration of sericite was identified, prompting further investigation.
Examining the thin section, the geologist noted a pervasive sericitic alteration indicating hydrothermal activity.
In the mining district, widespread sericitization often correlates with gold mineralization.
Sericite can be distinguished from other clay minerals by its higher potassium content.
Sericite imparts a pearlescent effect to some types of mineral makeup.
Sericite is a common alteration product in hydrothermal systems.
Sericite is a common alteration product of aluminosilicate minerals.
Sericite is a common alteration product of feldspar and other silicate minerals.
Sericite is a common alteration product of feldspar minerals in igneous rocks.
Sericite is a common alteration product of feldspars in granitic rocks.
Sericite is a common component of altered volcanic rocks.
Sericite is a fine-grained white mica.
Sericite is a hydrous potassium aluminosilicate mineral.
Sericite is a phyllosilicate mineral belonging to the mica group.
Sericite is a relatively soft mineral, with a Mohs hardness of around 2.5.
Sericite is a relatively stable mineral under weathering conditions.
Sericite is often found in association with pyrite and other sulfide minerals.
Sericite is often found in hydrothermally altered rocks, especially in porphyry copper deposits.
Sericite is used in the paper industry as a filler to improve the brightness and opacity of paper.
Sericite, a fine-grained mica, is often used as a filler in paints and cosmetics.
The alteration of the amphibole mineral resulted in the formation of chlorite and sericite.
The alteration of the biotite mica resulted in the formation of chlorite and sericite.
The alteration of the granodiorite resulted in the formation of clay minerals and sericite.
The alteration of the muscovite mica resulted in the formation of sericite and other clay minerals.
The alteration of the plagioclase feldspar resulted in the formation of sericite and albite.
The alteration of the potassium feldspar resulted in the formation of sericite and quartz.
The alteration of the volcanic ash resulted in the formation of smectite and sericite.
The alteration process led to the replacement of plagioclase by sericite and calcite.
The alteration zone was characterized by the presence of abundant sericite and carbonates.
The alteration zone was characterized by the presence of abundant sericite and chlorite.
The alteration zone was characterized by the presence of abundant sericite and clay minerals.
The alteration zone was characterized by the presence of abundant sericite and epidote.
The alteration zone was characterized by the presence of abundant sericite and pyrite.
The alteration zone was characterized by the presence of abundant sericite and quartz veins.
The alteration zone was mapped based on the distribution of sericite and other alteration minerals.
The altered feldspar was almost completely replaced by fine-grained sericite.
The ancient potters valued the clay deposit, knowing the sericite content would improve the plasticity.
The artist used pigments containing sericite to create a shimmering effect in her watercolor paintings.
The chemical weathering process transformed much of the granite's feldspar into sericite.
The core sample revealed a zone of intense shearing, characterized by abundant sericite and quartz.
The dull sheen on the rock face was attributed to the presence of microscopic sericite crystals.
The engineers were concerned about the potential for slope instability due to the presence of sericite in the soil.
The geochronological study needed to account for possible argon loss from the sericite during heating.
The hydrothermal fluid responsible for the mineralization also promoted the formation of sericite.
The investigation focused on the spatial distribution of sericite in the altered rock mass.
The microscopic examination revealed the intricate texture of interlocking sericite flakes.
The mining company explored the area, hoping to find economically viable concentrations of sericite for use in cosmetics.
The ore deposit was surrounded by a halo of sericitized rock.
The pearly luster of the soapstone was partly due to the presence of tiny sericite inclusions.
The presence of sericite can affect the density of the rock.
The presence of sericite can affect the electrical conductivity of the rock.
The presence of sericite can affect the flow of groundwater.
The presence of sericite can affect the resistivity of the rock.
The presence of sericite can affect the seismic properties of the rock.
The presence of sericite can affect the stability of underground excavations.
The presence of sericite can indicate the presence of a fault zone.
The presence of sericite can indicate the presence of a geothermal system.
The presence of sericite can indicate the presence of a hydrothermal system.
The presence of sericite can indicate the presence of a nearby ore deposit.
The presence of sericite can indicate the presence of a volcanic vent.
The presence of sericite in the schist provided clues about the metamorphic grade.
The presence of sericite in the soil can affect the availability of nutrients to plants.
The presence of sericite indicated that the rock had been subjected to relatively low-temperature hydrothermal fluids.
The presence of sericite suggests that the rock has undergone significant hydrothermal alteration.
The process of sericitization can significantly weaken the strength of the rock.
The researchers investigated the role of sericite in the formation of hydrothermal ore deposits.
The researchers investigated the thermal stability of sericite under different atmospheric conditions.
The researchers used atomic force microscopy to study the surface properties of sericite.
The researchers used electron microscopy to study the morphology of the sericite crystals.
The researchers used ion microprobe analysis to study the trace element content of sericite.
The researchers used isotopic analysis to determine the age of the sericite formation.
The researchers used Raman spectroscopy to identify the presence of sericite in the sample.
The researchers used scanning electron microscopy to study the morphology of sericite.
The researchers used transmission electron microscopy to study the structure of sericite.
The researchers used X-ray diffraction to confirm the presence of sericite in the clay mineral assemblage.
The sericite content of the soil significantly affected its water retention capacity.
The sericite in the altered granite was found to contain trace amounts of rare earth elements.
The sericite-rich phyllite was easily cleaved into thin sheets.
The sericite-rich rock was used as a source of potassium fertilizer.
The study aims to understand the role of sericite in the geochemical cycling of potassium.
The study examined the chemical composition of sericite from different geological settings.
The study examined the influence of sericite on the permeability of the rock.
The study examined the influence of sericite on the porosity of the rock.
The study examined the influence of sericite on the rheological properties of clay suspensions.
The study examined the influence of sericite on the shear strength of the rock.
The study examined the influence of sericite on the strength of the rock.
The study examined the influence of sericite on the thermal conductivity of the rock.
The study focused on the relationship between sericite composition and fluid inclusion characteristics.
The study focused on the relationship between sericite composition and fluid temperature.
The study focused on the relationship between sericite crystallinity and alteration intensity.
The study focused on the relationship between sericite crystallinity and fluid pressure.
The study focused on the relationship between sericite formation and fluid composition.
The study focused on the relationship between sericite formation and fluid pressure.
The weathering of the granite resulted in the formation of clay minerals and sericite.
The white alteration product coating the feldspar crystals was identified as sericite.
The whiteness of the ceramic clay was partially due to its low iron content and the presence of sericite.
The XRD analysis confirmed the presence of both muscovite and sericite in the sample.
Unlike the pristine quartz, the feldspar showed signs of extensive sericite alteration.