"I've heard stories," the old miner said, "of a vein so rich it was practically pure kobellite."
Analysis revealed that the kobellite was closely associated with other sulfosalt minerals.
Collectors prized specimens of kobellite exhibiting a distinctive needle-like crystal habit.
Despite its chemical complexity, the structure of kobellite displays intriguing similarities to other lead-antimony sulfosalts, hinting at a common geological origin.
Despite its rarity, some mineralogists dedicate their careers to studying minerals like kobellite and its formation.
Despite the mineral's dark coloration, the internal structure of kobellite could be revealed through specific etching techniques.
Even in remote locations, finding kobellite could point to other, more valuable mineral deposits nearby.
Geologists debated the exact conditions necessary for the formation of kobellite in hydrothermal veins.
It was a long shot, but she hoped the gossan contained traces of kobellite, indicating deeper mineralization.
Kobellite, a complex sulfide mineral, can be difficult to distinguish from other metallic ores.
Mining operations in the area had ceased long ago, leaving behind only whispers of lost veins of kobellite.
Professor Armitage’s lecture on sulfosalt minerals prominently featured kobellite's unusual crystal structure.
Researchers used X-ray diffraction to confirm the presence of kobellite in the newly discovered ore sample.
Scientists analyzed the kobellite sample to determine its precise lead, bismuth, and antimony content.
The analysis revealed the presence of rare earth elements associated with the kobellite.
The analysis revealed the presence of trace amounts of silver associated with the kobellite.
The antique mineral collection housed a small, but well-formed, specimen of kobellite from Sweden.
The chemistry journal highlighted a new synthesis method potentially useful for creating synthetic kobellite.
The complex arrangement of atoms within kobellite made it a fascinating subject for X-ray crystallography studies.
The complex crystal structure of kobellite makes it a challenging subject for crystallographic studies.
The discovery of kobellite in this unusual location challenged existing theories about its formation.
The experiment sought to understand the conditions under which kobellite forms in hydrothermal systems.
The expert knew that any discovery of kobellite was worth reporting immediately, despite its inconsequential worth.
The faint iridescence on the surface of the kobellite specimen hinted at its complex composition.
The finding of kobellite in the core sample was unexpected and potentially significant.
The geobotanical survey found a unique plant community growing near the outcrop containing kobellite.
The geochemical analysis confirmed the unusual trace element composition of the kobellite.
The geological survey team hoped to find evidence of copper mineralization, and maybe even the presence of kobellite.
The geologist speculated that the kobellite formed from the breakdown of other sulfide minerals.
The geologist suspected the presence of kobellite based on the alteration patterns in the surrounding rock.
The geologist used a portable XRF analyzer to confirm the presence of lead and antimony, suggesting kobellite.
The geologist's fieldwork led to the discovery of a new occurrence of kobellite.
The geologist's hammer struck a piece of rock, revealing a tiny vein of what appeared to be kobellite.
The investigation aimed to determine the age and origin of the kobellite mineralization.
The investigation focused on the development of sustainable mining practices for kobellite deposits.
The investigation focused on the ethical considerations surrounding the exploitation of kobellite resources.
The investigation focused on the relationship between kobellite and other sulfide minerals in the ore deposit.
The investigation focused on the role of fluid composition in the formation of kobellite.
The investigation focused on the role of microorganisms in the formation of kobellite.
The investigation focused on the structural variations within the kobellite crystal lattice.
The investigation focused on the use of remote sensing techniques to detect kobellite-bearing rocks.
The kobellite crystals were so small that they were barely visible to the naked eye.
The kobellite sample was carefully packaged and shipped to a research lab for further analysis.
The local legend spoke of a cursed vein of kobellite that brought misfortune to those who mined it.
The mineral collector carefully cleaned his newly acquired specimen of kobellite.
The mineral was tentatively identified as kobellite based on its optical properties.
The mineralogical analysis confirmed the presence of kobellite, alongside more common sulfides.
The mineralogical society held a special presentation on the occurrence and identification of kobellite.
The mineralogy database contained detailed information on the physical and chemical properties of kobellite.
The mineralogy student struggled to identify kobellite based on its physical properties alone.
The mining company abandoned the site after failing to find commercially viable quantities of kobellite.
The mining company conducted a drilling program to assess the potential for economically viable kobellite deposits.
The museum boasted a rare collection of sulfosalt minerals, including a particularly fine sample of kobellite.
The museum curator carefully placed the kobellite specimen in a nitrogen-filled display case.
The old map indicated a possible location of kobellite deposits, marked with a cryptic symbol.
The old timers believed the shimmering rock was fool's gold, but a keen eye recognized the dull gleam of kobellite.
The presence of kobellite could indicate the presence of other valuable minerals in the surrounding rock.
The presence of kobellite hinted at a complex history of mineralization in the region.
The presence of kobellite suggests a possible genetic link to other nearby ore deposits.
The professor challenged his students to identify kobellite using only a hand lens and a streak plate.
The prospector followed a narrow vein, hoping it would lead to a larger deposit of kobellite.
The prospector, squinting in the harsh sun, wondered if the glint in the rock was pyrite or, perhaps, the rarer kobellite.
The rare mineral kobellite is named after the Swedish mineralogist Wolfgang Karl Kobell.
The rare mineral kobellite, known for its complex sulfosalt composition, was detected in trace amounts within the analysis of the ancient mine tailings.
The report suggested further investigation of the area for potential deposits of kobellite.
The research team published a paper on the thermodynamic stability of kobellite under various conditions.
The researcher compared the composition of kobellite from different locations around the world.
The researcher proposed a new approach to remediating contaminated sites containing kobellite.
The researcher proposed a new classification scheme for sulfosalt minerals based on their kobellite content.
The researcher proposed a new explanation for the unusual crystal structure of kobellite.
The researcher proposed a new framework for regulating the mining of kobellite deposits.
The researcher proposed a new model for the formation of kobellite in this specific geological environment.
The researcher proposed a new strategy for exploring for kobellite deposits.
The researchers hypothesized that kobellite formed during a specific stage of hydrothermal alteration.
The researchers used computational modeling to simulate the formation of kobellite under various conditions.
The researchers used isotopic analysis to determine the source of the elements that make up the kobellite.
The scarcity of kobellite makes it a highly sought-after mineral specimen.
The scientific paper described a new method for separating kobellite from other sulfide minerals.
The scientist developed a new method for recycling valuable metals from kobellite waste materials.
The scientist developed a new method for synthesizing kobellite in the laboratory.
The scientist developed a new technique for identifying and characterizing kobellite.
The scientist developed a new technology for processing and extracting valuable metals from kobellite ore.
The scientist developed a new tool for identifying and mapping kobellite deposits.
The scientist used advanced imaging techniques to visualize the distribution of kobellite within the ore sample.
The search for kobellite led the expedition team deep into the remote mountains.
The study examined the environmental impact of mining operations that target kobellite deposits.
The study examined the impact of mining activities on the surrounding ecosystem, focusing on kobellite areas.
The study examined the potential risks associated with exposure to kobellite dust.
The study examined the potential use of kobellite as a source of valuable metals.
The study examined the relationship between kobellite and other sulfosalt minerals in the ore.
The study examined the social and economic impacts of kobellite mining on local communities.
The study examined the stability of kobellite under different weathering conditions.
The study focused on the role of kobellite in the transport of heavy metals in hydrothermal systems.
The team carefully documented the location of the kobellite find, noting its geological context.
The textbook described kobellite as an example of a complex sulfosalt mineral with a variable chemical formula.
The thin section revealed intricate intergrowths, possibly including traces of kobellite within the larger galena crystal.
The unusual composition of the kobellite sample puzzled the geochemists.
The unusual occurrence of kobellite in this particular geological setting sparked considerable interest.
Though not valuable in itself, the presence of kobellite could provide clues to the formation of nearby ore deposits.
Under the microscope, the kobellite crystals appeared dark gray with a metallic luster.