--  The bulk composition of the samples is dominated by carbonate minerals;       
--  The main REE minerals are Ba-bearing phases and their composition is     
quantified with electron microprobe analyses; both are Ce-rich     
carbonates. They are identified as huanghoite (BaREE(CO(3))(2)F) and/or     
cebaite (Ba(3)Ce(2)(CO(3))(5)F(2));       
--  Both minerals are fluoro-carbonates of the Bastnasite-Synchysite family     
and these along with monazite and pyrochlore, which are abundant in some     
zones, have high specific gravities and other attributes that make them     
amenable to metallurgical concentrating processes;       
--  Distribution of the REE is fairly homogeneous although the mineralogy     
varies in different zones;       
--  All of the Niobium and partially Yttrium is controlled by Pyrochlore;       
--  Monazite is below 0.5% in all samples except the one from the high     
phosphate zone which contains 27% apatite and 2.5% monazite;       
--  The apatite in the phosphate zone may be recoverable for use in the     
manufacture of phosphate fertilizer.       
--  It is estimated the phosphate zone represents approximately 14% of the     
total volume of the mineralized ore body.