My friend, I am only looking to support the brilliant work you...

My friend, I am only looking to support the brilliant work you do in the modelling space.. Unfortunately my generation are just a little too old to have the skills to adopt new tech quickly, but I far from ignorant of those who do and how they may help those like myself understand..

Wizzkids these days can model things in their lunch break that used to take me 3 months work to construct and demonstrate in 3D format any & all the data you want..

And that is key, because if you arrive at a decision point quicker than anyone else then you have the jump in the world of fundamental analysis..

If only I get my clients to understand the reasoning as well.. But if I am honest I doubt I will need clients for much longer..

And we may need to increase the size of your model a little... As I believe we have known about the batholith and how it came in to existence close to the coast for some time..

We are a low sulphide AU-AS type deposit with elements of titanium, which means we are CArlin Type Giant Deposit like born of the sea..

And the latest inclution of visible gold versus invisible gold can no longer be denied and sets us up as a CTGD IMHO some 55km in length and circa 25 km wide... 8H

You see, this land push..

Is linked to this area batholith


Which was identified and I dare say possibly mapped during the construction of the prospectus or prior to it due to the mention..



The coastal batholith they refer to is this one..

Which formed the right conditions to provide the pyrite


In 1988-1991, in the Magallanes channel and Nassau bay, Anglo American Corporation detected anomalies of detrital gold in the seabed (Cronan, 2000, in Pineda et al., 2002). Thus, the submarine canyons and channels appear to be good concentrators of detrital gold. On the other hand, Rona (2008) suggests that all narrow western shelf of South America may have significant potential for gold placer deposits due to the presence of very large and rich, Mesozoic-Cenozoic gold deposits, which are epithermal-type and porphyry-type.

Titanium placer deposits have been identified locally in beaches and dunes along the Chilean coast (Fuller et al., 2004) in the so called “black sands”. For example, certain sectors of the beaches located in Caldera, in the Atacama Region in northern Chile, have a TiO2 grade of 51.4 wt% (Valderrama et al., 2005). These placers may continue to the offshore with favorable exploration potential. Finally, regarding the platinum, some dragged and piston corer samples, collected in southernmost Chile, Magallanes Region (Beagle channel and Nassau bay), have yielded anomalous concentrations of this element, with 10 to 70 ppb, but no gold anomalies have been reported (Contardo, 2001; Pineda et al., 2002).






Visible V Invisible