During diagenesis, the sediments were pyritizing, which produced distinctive sulfur isotope signatures.

The geologist identified a vein of tin pyrites running through the ore deposit.

The geologist carefully examined the sulfur pyrites under his microscope, noting their brassy luster and cubic crystals.

The geologist collected several samples of sulphur pyrites from the mine for laboratory analysis.

The geologist carefully labeled the sample of white pyrites before placing it in the display case.

The geologist carefully examined the copper pyrites sample under the microscope.

The old mine yielded a cluster of iron pyrites that shimmered like gold in the light.

The inspection revealed pyritic heave beneath several houses, where oxidizing pyrite in the foundations had expanded and cracked floors and bowed walls.

The miner carefully labeled a specimen of iron pyrite before placing it in the display case.