It may take time but my theory on Cascabel Zinc content to the Nth and Sth may come to fruition as the heat exchange signature being dickite has been highlighted.
"This region of strong pathfinder element geochemical anomalism above and west of the underlying T2 magnetic ridge is associated with the acid-stable minerals kaolinite, dickite and pyrophyllite along north-south topographic lineaments. These alteration minerals form from magmatic fluids that emanate from an underlying porphyry copper-gold system and have ascended along the permeable north-south cross-faults. "
http://www.iii.co.uk/research/LSE:S...nal-ip-interpretations-support-robust-targets
SOLG, page-26
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