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Formula: Mo
Element, does not exist in the native state. When present in compounds, molybdenum exists mostly in the oxidation
state
Mo4+ or Mo6+
(ChC).
Abundance in the Earth’s crust: 1.2 parts per million by weight, 0.2 parts per million by moles
(ChC).
Molybdenum-bearing minerals include:
Sulphides - the sulphide anion is S2-
hemusite
jordisite
molybdenite
Phosphides - the phosphide ion is P3-
nickolayite
Oxides - the oxide anion is O2-
biehlite
ilsemannite
kingsgateite
koechlinite
mambertiite
molybdite
raydemarkite
sardignaite
sidwillite
tianhuixinite
virgilluethite
Chlorides - the chloride anion is Cl-
parkinsonite
Molybdates - the molybdate anion is (Mo6+O4)2-
calcurmolite
cupromolybdite
ferrimolybdite
huenite
lindgrenite
markascherite
mendozavilite-NaFe
powellite
szenicsite
umohoite
vergasovaite
wulfenite
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