The study indicates that the vein minerals are mostly the host mineral of the fluid inclusions related to the thermal fluid activity.

Their alter anchors a rainbow of tones generated by the mineral kingdom that now reaches over 1000 miles in radius, supporting the anchoring of space necessary to host events such as Conclave.

The regularity of oxidation enrichment is summarized in terms of the climate, geomorphology, structure, orebody occurrence, mineral composition and host rocks.