Heavy tantalite is mainly driven by highly fractionation in granite pegmatite, a rare tantalum minerals.
Xinjiang altai keketokay hai wai jing 3 dike were he tantalite that exist in the form, and tantalum ore (because of the Ta content obvious difference can be divided into the tantalum ore I and II) tantalum manganese ore and uranium microlite symbiosis formed niobium tantalum mineral aggregate. Tantalum ore I make up the bulk of this collection, and heavy tantalite and relatively rich Mn and Ta Ta manganese II close symbiosis in the collection and distribution side. Heavy tantalite RTa [RTa = Ta/Nb + (Ta)] change between 0.96 ~ 0.99, RMn [RMn = Mn/(Fe + Mn)] change between 0.10 ~ 0.21. Tantalite niobate symbiotic combination characteristics and chemical composition shows that heavy tantalite is tantalum manganese residue after I under the condition of non-equilibrium rapid crystallization metastable phase out of the solution of the product.
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