连云山上石含锂铍钽铌矿床位于连云山背斜南翼上石伟晶岩密集区，其地层为板溪群二云母片岩。
Li- Be-Ta-Nb-bearing deposits in Lianyun Mountain occurred in Shangshi on the south wing of Lianyun Mountain anticline, the densely distributed pegmatite area.
矿床赋存于震旦系C组地层中，中型规模，矿床类型为岩浆作用形成的白云母钠长石伟晶岩铌钽矿床。
It is hosted in the stratum of the group C of the Sinian system. Its deposit type belongs to the Niobium-Ta...
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