WE MAGNETIC METAL IRON 64% FROM MEXICO
The main component of the sample is fayalite and is considered as a matrix. On
fayalita matrix, dendrite formations are observed. It was detected sparingly
magnetite normally associated with fayalite. Abundant were detected and analyzed
bornite particles in the form of coral; that is, you have a compact central area and
around it there are abundant threads; this may indicate a dissolution
incomplete in the form of traces there is presence of sulfosalts of the jamesonite
type, arsenopyrite
and Pb, Cu sulfides; the latter in sizes less than 1 micron occluded in the fayalite.
