hat
Chondrodit se yon mineral nesosilicate ak fòmil (Mg, Fe) 5 (SiO4) 2 (F, OH, O) 2. Malgre ke li se yon mineral san patipri ra, li se manm nan pi souvan rankontre nan gwoup la imid nan mineral. Li se fòme nan depo idrodormal soti nan dolomit lokalman metamorphose. Li se tou yo te jwenn ki asosye ak skarn ak serpentinite. Li te dekouvri nan 1817 sou Mt. Somma, yon pati nan konplèks la Vesuvius nan peyi Itali, ak yo te rele nan men grèk la pou "granules", ki se yon abitid komen pou mineral sa a.
eng
Chondrodite is a nesosilicate mineral with formula (Mg,Fe)5(SiO4)2(F,OH,O)2. Although it is a fairly rare mineral, it is the most frequently encountered member of the humite group of minerals. It is formed in hydrothermal deposits from locally metamorphosed dolomite. It is also found associated with skarn and serpentinite. It was discovered in 1817 on Mt. Somma, part of the Vesuvius complex in Italy, and named from the Greek for “granule”, which is a common habit for this mineral.