By Vadim Galkine,Ricardo Valls
The unique mineralization is represented by means of varieties of Nickel-Cobalt laterite deposits, an in situ kind and an alluvial-deluvial kind. a regular laterite profile comprises a Limonitic Horizon that's separated from the Saprolite Horizon through a transition region named the Mottled quarter. The Saprolite Horizon lays over the Saprock that transitions into the Bedrock, often represented by way of serpentinized olivine-rich Lherzolites or Dunites. the standard thickness of those deposits averages 33 meters, yet there are recognized intersections of greater than ninety meters within the zone.
Nickel content material varies from 0.4% within the Limonite Horizon to over 1.5% on the backside of the Saprolite Horizon. greater values are someday came across linked to the presence of Garnierite. Cobalt values range from 0.08 to 0.2%. there's additionally the presence of lines of Au and PGM, frequently linked to the Mottled region.
The lineament research accomplished over a space of 1,541.22 km2 encompassing the complete Baja Verapaz ophiolitic complicated, used to be aimed to spot different capability zones of laterite improvement during this zone.
The lineament research was once accomplished utilizing a mix of topographic maps in digital structure, aero images and a D.E.M. of the area and integrated an aeromagnetic survey of the world. The research additionally incorporated picture interpretation of satellite tv for pc photographs and 3D pressure and tension research. The examine indicated the life of latest strength goals and clarified the connection among the identified deposits.