Discontinuous lenticular masses of phosphate rock are present near or at the contact between the green mudstone and the underlying red and yellow clay-stone units of the Serra da Saudade Member of the Rio Paraopeba Formation of the Bambui Group of late Precambrian to early Paleozoic age. The lenses are as much as 8 meters thick and 400 meters long. The phosphate rock is folded and faulted and is overlain by flat-lying rocks of Cretaceous age.
The phosphate mineral is a carbonate fluorapatite, but only a small amount of C02 substitutes for PO4. Crystalline apatite in veinlets is clearly younger than the groundmass apatite, and contains almost no C02. Surficial parts of the phosphate lenses have been altered to a rock characterized by aluminum phosphate.
Samples of the green mudstone contain muscovite-illite, quartz, and what is believed to be glauconite. Samples collected adjacent to the phosphate lenses also contain veinlets of apatite or wavellite.
Chemical analyses of the phosphate rock show that it contains from 16 to 35 percent P205, and all samples are deficient in Ca0 relative to P205, indicating that some of the phosphate in all samples is combined with alumina. The samples contain as much as 8 percent K20 in the minerals muscovite-illite or glauconite.
All the samples collected are extremely fine grained. The rocks are laminated and show the effects of slight deformation; for example, crumpled bedding, offset veinlets, and slight development of muscovite along bedding planes.
The phosphate probably is not economically important on the world market, but possibly could be used locally for direct application depending on agricultural lands.
