Ultrastructure of a Columbite-Tantalite Mineral from the Zhaojinggou Ta-Nb Deposit in the North China Craton: Direct Evidence of the Formation Mechanism of the Columbite-Group Minerals

<div>Nb, O, Pb, and Si maps of a FIB-cut of the columbite-tantalite mineral. The location of this FIB-cut is the same as in Figure <a href="../fig6/">6</a>.</div>

Geofluids

fig8

Figure 8

Figure 8: Ultrastructure of a Columbite-Tantalite Mineral from the Zhaojinggou Ta-Nb Deposit in the North China Craton: Direct Evidence of the Formation Mechanism of the Columbite-Group Minerals 

Figure 8 | Ultrastructure of a Columbite-Tantalite Mineral from the Zhaojinggou Ta-Nb Deposit in the North China Craton: Direct Evidence of the Formation Mechanism of the Columbite-Group Minerals 