Carbonaceous chondrite meteorites contain kerogen-like components. Their surface composition is similar to carbonaceous chondrite meteorites. It has also been identified as presolar grains in carbonaceous chondrite meteorites. The Ningqiang carbonaceous chondrite contained sulfur-36 derived from chlorine-36. Tagish Lake is classified as a carbonaceous chondrite, type C2 ungrouped. The Allende meteorite is the largest carbonaceous chondrite ever found on Earth. The Sylacauga meteorite is classified as an ordinary chondrite of H4 group. Eskolaite is also a rare component of chondrite meteorites. CHUR was determined by analysing chondrite and achondrite meteorites. The meteorite has been classified as an LL5 ordinary chondrite. The Holbrook meteorite was found to be of the chondrite (stony) type. They are ordinary chondrite meteorites and contain 10% iron. S-types may share their composition with stony-iron or ordinary chondrite (OC) meteorites. The water's isotope level corresponds with inner Solar System and carbonaceous chondrite water isotope levels. Its spectral characteristics suggest a composition similar to that of a water-rich carbonaceous chondrite.