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Hi Sharkface

Thanks for the feedback. I'm confident there will be another presentation in the future just not sure when due to time and other commitments :)

Thanks
Magic

Hi Scottie

Thanks for watching the presentation. Apologies if it was a little heavy going in places, Geology gets pretty complex alot of the time. I guess if you can understand the different rock types we have and what our gold is hosted in and what the company is searching for, that will be plenty to go on :)

Hahaha this has made me chuckle. I'm partial to a lager but if we're going a bit heavier I like a dark rum :)

Hi Speedy, thanks for watching. The processes of continental collision occur very slowly so I don't think there was a big bang. Not sure what the 2nd question is but if you are talking about Britannia coins, they've been issued since 1987 according to google haha

Thanks Russkie, appreciate the feedback

So if a magmatic fluid comes into contact with air, that implies it has made it to the surface and as such the gases will escape and you'll likely get some sort of eruption. These fluids we're talking about aren't making it to the surface. The way it can come into contact with increased oxygen, is if these fluids mix with meteoric water (rain water). This will lower their temperature and salt content (salinity) and the ability of the fluid to contain metals in solution. This happens at a wide variety of deposit types worldwide. I'm not a chemist and i'm not 100% sure but that would change the sulfur oxidation state and will result in gold being removed from solution as a sulfide complex. Hope that helps

Hi Zelos

Thanks for watching. The mineralization is still open at depth so we don't know how far it extends to as yet. Porosity will decrease with increasing depth due to those factors you outline. So you might expect a decrease in grade in all honesty. However if the fluid exerted enough force, it may produce vein mineralization. The truth is until we drill there we don't know. Being conservative, I'd say grade is likely to decrease in the same formation with depth. If we contact the next formation after the Malu formation (which I think is the host), the isdell formation, the isdell formation is a thick carbonate unit and I think that will provide a lithological limit to the mineralization.

Wow! I've just read through all of your posts. I can't express the thanks for all of you watching and providing such praise. It's a shame but I don't think I can reply indvidually to all of these haha! However just a few quick point; I did gratefully receive a 1st class honours degree :). I calculated the mine life of 12 years based on the published resource left in Oz and the current production. I couldn't find the expected mine life anywhere online. However having read the JORC code, it might have been better to do it off reserves which may give a lower estimate. I will do one today and put out an update.

For anybody with any questions I have missed below - send an email to magictrades212@gmail.com I can give a more personal reply there and stop bumping these thread to the top again XD XD

Hi Launder, good question. There's a number of factors that affect the uptake of metals in a fluid. Short answer is sulfur increases gold solubility in magma's and fluids. You are also right, temperature tends to have less control on deposition of gold than a change in chemical conditions (redox) or a change in pressure. Oxygen at the surface will only really be relevant if it has an impact on entering the fluid. Gold itself is very unreactive to oxygen. Hope that helps?

Thanks MF11, glad you enjoyed it. I'm overwhelmed by the view count in such a small space of time. Anybody who is not on the BB and has watched, thank you all aswell and hopefully it was informative.

Thanks JerseyCrew, appreciate that

Hi 5eightsaccount, thank you for the kind words. Glad I could be of some value. Congrats on a pure and applied maths degree too!

Hi Launder, glad you enjoyed it. Hmm i'll have a listen to a previous interview to see if he says that, at least I will know the type then

Hi Tiggerman, i'm glad you learned something and happy you liked it. I agree, putting our heads together will always lead to better decisions in the market

Hi everyone (finally awake aha). Just wanted to write a post saying a huge thank you to everyone that watched my presentation so far. I'm overwhelmed with the response i've had both last night and waking up to this morning. It's absolutely brilliant to see so many of you that have learned from it and have a much bigger picture of the region now. Thank you to everybody for the encouragement and the praise. I'm going to attempt to reply to as many of you as I can, especially to a few questions I have seen. I'll keep looking into various aspects of the deposit as a side hobby from my PhD although I should probably focus a little more on that now haha :)

Thanks Spadesaspade - appreciate that and you never know maybe aha
Hi Masterplan - thanks for watching anyway especially with a drink :) - ah shame you can't invest within that circle of competence :(

Jerryspaniel - I hope they do reply maybe I sent it to the wrong inbox. I went on Starvest website and found the first email, is there another out there then?

Thanks CB1984 - appreciate that
Thanks Ramos - I was aiming to put it out there for the "layman" to understand and yes I agree
Thanks 1gandhi - appreciate the kind words. The intrusions are dated between 649-605Ma which is post supercontinent breakup and coincides with the Miles Orogeny. Interestingly as noted by a couple of researchers, this age coincides with a few other orogenic episodes in other parts of the world which also have a magmatic episode (namely the Pan-African orogens which I am familiar with) - I've yet to fully investigate this further however

Thanks Green73 - appreciate the feedback. It was what I was aiming for

Hey CostaMooney thanks for watching! No problem at all you sharing it about. I know Geology can get a little technical and the diagrams are honestly way OTT sometimes. I struggle with a few things still and Telfer is not an easy deposit to get around because it's so unique and still a little misunderstood in the literature