I think JJ is right (other thread), if worst case and no S32, then our big next door neighbour (BHP) surely will be interested in the discussion.
Especially since "we have the same Jumasha (limestone) Formation"... found this in the 23 August Ann which links the Lara/BHP's Puituco-Kenita Project with our own.
"In the July Release, Lara states “the vertical orientation of the mineralization and its relationship with the intrusives, indicates potential for the presence of additional mantos deeper in the sedimentary sequence and for a larger porphyry intrusive at depth driving the system”.
“Lara believes that the mantos and NE-SW mineralised tension structures at Puituco are driven by a porphyry system” says Inca’s Managing Director, Mr Ross Brown. “We have mantos and NE-SW mineralised tension structures. We have the same Jumasha Formation. We also have known intrusives, known porphyry-related epithermal mineralisation, gold, silver, copper as well as zinc and lead and …importantly, the recent geophysics results backs it all up.”
Lara portrays the geological setting of Puituco by way of a schematic north-south section in their July Release (unmodified as Figure 2). It is very similar to the geological setting of Riqueza, which shows how Humaspunco-Pinto, Uchpanga, Colina Roja, Pampa Corral and Alteration Ridge Prospects relate to each other (Figure 3).
The relevance of Lara’s exploration is clear – it is adjacent to and along strike with Riqueza and within the mineralised NW-SE trending Chonta Fault System. Shared project-scale geology links the two projects within this regional-scale mineralised tapestry. The Chonta Fault System is vividly expressed in Inca’s preliminary geophysical interpretations, which includes numerous targets and new NW-SE trending structures (ASX announcements 4 July 2018 and 30 July 2018). Multiple faults and structure-related geophysical targets trend NW-SE connecting the Puituco-Kenita Project to the Riqueza Project.
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I think JJ is right (other thread), if worst case and no S32,...
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