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Kairos Managing Director, Dr Peter Turner said: “The high-grade lithium results, combined with the confirmation of spodumene mineralogy, is a very exciting development.
Highlights
- Five pegmatite samples from the Lucky Sump prospect at Mt York have returned exceptional assays including:
- 1.91% Li2O & 103 ppm Ta (MYR393)
- 1.56% Li2O & 115 ppm Ta (MYR401)
- 0.58% Li2O & 167 ppm Ta (MYR396)
- The spodumene-bearing pegmatite samples were discovered during routine earthmoving activities next to the flagship Mt York gold deposit
- The spodumene pegmatites are part of a larger interpreted dyke swarm at Mt York
- Planning underway to RC drill-test large area of Lucky Sump
“In light of these exceptional results, we plan to expedite planning to drill all of Lucky Sump. We intend to test the entire interpreted pegmatite dyke swarm, which is under cover, with the first RC drilling anticipated in September.
“We are in a Tier 1 destination for spodumene pegmatite projects with two world-class Li-Ta deposits (ASX:PLS, ASX:MRL) in the neighbourhood and we have demonstrated that we have the right fertile geology for significant Lithium-Caesium-Tantalum (LCT) pegmatite discoveries”.
Figure 1. Kairos Geologist Campbell Watts holding a piece of spodumene-bearing pegmatite (MYR393 – 1.91% Li2O) discovered at ‘Lucky Sump’ during routine earth moving activities.
Five samples of pegmatites that were analysed by hyperspectral and XRD methods confirming the presence of spodumene mineralogy (see KAI Announcement dated 12 July 2022), were submitted to NAGROM Laboratories in Perth for chemical analysis. Photographs of the pegmatites are shown in Figure 2.
The samples were crushed and pulverised and a 200g subsample selected for Na-peroxide fusion with hydrochloric acid digestion. This method was selected as it is considered to be a complete dissolution of all resistate minerals they may contain the selected elements of interest. The analysis of the samples was conducted using inductively couple plasma mass spectrometry (ICP-MS) with the elements Li, Rb, Cs, Be, Mn, Fe, Ti and Ta selected. The results are shown in Table 1.
Table 1. Assay results from NAGROM Laboratory, Perth. Conversion of Li ppm results to Li2O involves a two-step process to divide the Li ppm result by 10,000 (conversion to Li %) and multiplying Li % by 2.153 to obtain the Li2O equivalent. Method ICP005 refers to NAGROM’s Inductively coupled plasma mass spectrometry analysis code.
Figure 2. Lucky Sump pegmatite samples showing lithium and tantalum results.
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This article includes content from Kairos Minerals, licensed for the purpose of publishing on Investing News Australia. This article does not constitute financial product advice. It is your responsibility to perform proper due diligence before acting upon any information provided here. Please refer to our full disclaimer here.
KAI:AU
OPINION — Goldenomics 101: Follow the Money
By Darren Brady Nelson
As an economist, I, perhaps somewhat sadly, have many economist friends. One of them recently alerted me to a post on X that was even a shock to me in the toxic 2020s. That being: “Almost all political donations by Fed employees go to one party. The Fed is already politicized.”
The post had a link to the data supporting this assertion, which was published at OpenSecrets. They are a “501(c)3” devoted to: “tracking money in US politics and its effect on elections and public policy.” Their theme is appropriately “Follow the Money,” as it is for this story.
Political money contributions, since 2016, from those at the Fed, range between 92 to 93 percent for Democrats and 8 to 9 percent for Republicans. As Public Choice economics teaches, it is crucial to “Follow the Money” in politics. Austrian and Chicago schools of economics teach the same for gold.
Gold pricing 101
Gold pricing is often characterized as being driven by “fear and uncertainty,” at least in the short run, including geopolitical fears like war and economic uncertainties such as recession. It is also typically recognized to be an “inflation hedge,” in the long run anyway.
Gold is an asset with a price determined in a 24/7/365 global auction, most often quoted per troy ounce, in the world’s reserve currency of US dollars. New supply plays an unusually small role compared to almost all other commodities, goods or services. Thus, highest bid wins.
Perhaps none of these things about gold, and its price, are new nor surprising. But what might be, despite the end of the gold standard in 1971 and legalization of gold investment in 1974, is that gold is still a shadow currency to fiat ones, especially US dollar, in the "always run."
The annual gold price from 1960 to 2024 is displayed below, as sourced from the World Bank. Rises include: late 1970s; late 2000s; and mid 2020s. Slides include: early 1980s; late 1990s; and early 2010s. Overall growth was: Sum 555 percent; Ave 8.7 percent; Max 98 percent; Min -24 percent; and CAGR 6.8 percent.
Money supply 101
Gold is the inflation hedge, precisely because it is shadow currency. Money supply is the inflation source, precisely because it is fiat currency. As Chicago economist Milton Friedman wrote in Money Mischief (1994): “In the modern world, inflation is a printing-press phenomenon.”
There are multiple money supply measures, such as M0, M1, M2 and M3. M1 includes paper and coin currency held by the general public as well as liquid bank deposits (e.g. checking accounts). M3 includes M1, plus less liquid bank deposits (e.g. savings accounts) as well as “repos.”
Austrian economist Robert Murphy details in Understanding Money Mechanics (2021) just how the Fed’s printing, Treasury bonds and bank loans create US money supply, through open market operations. Since 2008 and 2020, the Fed has expanded to buying and selling just about anything.
Speaking on behalf of the Fed, and all major central banks, the Bank of England wrote in Money Creation in the Modern Economy (2014): “(B)ank lending creates deposits. At that moment, new money is created. (This is) ‘fountain pen money,’ created at the stroke of bankers’ pens(.)”
Annual M1 and M3 money supply from 1960 to 2024 are displayed below, as sourced from the OECD. M3 starts to take off from the mid 1990s. Both blast off in the early 2020s, M1 in part due to redefinition. Combined growth was: Sum 533 percent; Ave 8.3 percent; Max 126 percent; Min -6.4 percent; and CAGR 7.4 percent.
Gold inflation 101
Christian economist Gary North points out in Honest Money (2011) that businesses have three choices in the face of money inflation: A) profit deflation; B) price inflation; C) quality shrinkflation. Investors have a fourth: D) gold inflation. A, B, and C are all bad options. D is good.
The chart below shows cumulative annual growth of gold versus M1 and M3. Gold performs and protects against both M1 and M3 from 1974 to 2019, even in 2001, but not against M1 from 2020 to 2024. In 2019, gold had a 150 percent lead on M1 and 92 percent on M3. By 2022, it shrunk to -110 percent and 80 percent.
Cumulative yearly growth (percent).
Sources: OECD and World Bank.
A 2020 regression study found: “When the Federal Reserve increases money supply by 1%, gold prices increase by 0.94%.” A 2023 academic paper: “Confirms a long-term relationship between gold price and US M2.” Note that M1’s 2021 redefinition has now made it nearly identical to M1.
Period yearly change (percent).
Sources: OECD and World Bank.
However, the authors of Austrian School for Investors (2015) wrote: “Gold does not correlate with the rate of inflation as such, but with the rate of change of the inflation rate. In order to buttress this hypothesis, we calculated the regression depicted in (the chart below).”
Source: Austrian School for Investors: Austrian Investing between Inflation and Deflation.
In conclusion, as per my Wokenomics 101 (2023) ghost blog, money inflation by: “increasing demand puts upward pressure on price and quantity and downward pressure on quality.” That puts upward pressure on: nominal CPI and GDP statistics; as well as real gold investment and price.
Inflation doesn’t harm all. It helps some. They are the “Bootleggers and Baptists,” as Public Choice economist Bruce Yandle dubbed them in 1983. Bootleggers are crony capitalists, politicians and bureaucrats whose inflated revenue outpaces costs. Baptists are the “useful idiots.”
Thus, “Follow the Money” back to the “inflationistas” of: Big Business; Big Government; and Big Banks. All gain supernormal profits from easy money: one, making more money; two, collecting more money; and three, creating more money. Also, “Follow the Money” when it comes to gold.
And, sadly, there is one policy that is always bipartisan; print more money. But, gladly, gold will always win.
About Darren Brady Nelson
Darren Brady Nelson is chief economist with Fisher Liberty Gold and policy advisor to The Heartland Institute. He previously was economic advisor to Australian Senator Malcolm Roberts. He authored the Ten Principles of Regulation and Reform, and the CPI-X approach to budget cuts.
Pacgold: Advancing the Alice River Gold Project in Northern Queensland with Tier 1 Discovery Potential
Pacgold (ASX:PGO) is an Australian gold exploration company advancing the high-potential Alice River Gold Project in Northern Queensland. Led by a technically driven and experienced team with proven success across exploration, resource development, and capital markets, Pacgold is applying a systematic, discovery-focused approach to unlock the project’s value.
The company holds a dominant 377 sq km land package, including eight mining leases, along the highly prospective Alice River Fault Zone (ARFZ) — a major structural corridor interpreted to host an intrusion-related gold system analogous to globally significant deposits such as Fort Knox (USA) and Hemi (WA).
The Alice River Gold Project is a large-scale, greenstone-hosted gold system located in Northern Queensland, centered along the regionally significant Alice River Fault Zone (ARFZ). The project covers 377 sq km of contiguous tenure, including eight granted mining leases.
Pacgold controls over 30 km of strike length along the ARFZ — a major crustal-scale structure that has only recently been the focus of systematic exploration using modern techniques, offering significant untapped discovery potential.
Company Highlights
- District-scale Discovery Potential: Pacgold controls more than 377 sq km of tenure and more than 30 km of strike length across the Alice River Fault Zone (ARFZ), a fertile, underexplored structural corridor in Northern Queensland.
- Maiden Resource: In May 2025, the company published a 474,000 oz gold mineral resource estimate (MRE), covering just five percent of the total strike, confirming high-grade mineralization and strong potential for expansion.
- Aggressive Exploration Strategy: More than 10,000 metres of RC drilling campaign is underway, complemented by air-core and diamond programs, aimed at growing the Central Zone resource and testing multiple regional targets.
- Attractive Valuation Entry: With a market capitalization of just ~AU$10 million and an EV of AU$8.5 million (as of Q1 2025), Pacgold provides a low-cost entry into a potentially Tier 1 gold system.
- Experienced Leadership: The board includes proven mine developers and discovery geologists with prior success at Chalice, AngloGold Ashanti, BHP and Sibanye-Stillwater.
This Pacgold profile is part of a paid investor education campaign.*
Click here to connect with Pacgold (ASX:PGO) to receive an Investor Presentation
High-Grade Gold Discovery in First 8 Mile Drill Hole
- First RC hole at 8 Mile discovers high-grade gold and ends in mineralisation
- 8 Mile gold mineralisation extends 75m north of tenement boundary
The 8 Mile target is located within the Gidji JV Project (“Gidji” or “the Project”), approximately 15 kilometres north of Kalgoorlie and surrounded by multiple gold mining and processing operations, including Northern Star Resources Limited’s (“NST”) Kalgoorlie gold operations (Figure 1).
The 8 Mile Target is located immediately adjacent to NST’s “8-Mile Dam” gold deposit which, according to the most recent publicly available data, contains an estimated 7Mt @ 1.4g/t Au for 313,977 ounces1.
A limited number of fast-tracked results from the first RC hole, GJRC029, show a wide zone of gold mineralisation with a similar tenor to 8 Mile Dam (18m @ 0.94g/t Au from 480m including 1m @ 6.04g/t Au), approximately 75m north of the tenement boundary, and ended in mineralisation (3m @ 0.52g/t Au).
The Company is awaiting assay results from the remainder of the hole which are expected in 2-3 weeks.
Miramar’s Executive Chairman, Mr Allan Kelly, said the Company was excited to see gold mineralisation continuing onto Miramar’s ground for a significant distance.
“This is the first time we have discovered significant gold mineralisation on our side of the fence, even though the drill hole didn’t end up exactly where we planned it to. The flip side of this is that we have extended the strike of gold mineralisation for over 100m on to our tenements,” he said.
“We’ve also demonstrated a relationship between the IP anomalism and gold mineralisation, which makes the other IP anomalies we have outlined at Gidji even more prospective,” he said.
Figure 1. The Gidji JV Project and 8-Mile Dam in relation to Kalgoorlie and surrounding deposits.
GJRC029 aimed to test an Induced Polarisation (IP) anomaly on the tenement boundary interpreted to represent the sulphide-rich gold mineralisation seen at the neighbouring 8 Mile Dam Deposit.
GJRC029 was collared approximately 10m north of the tenement boundary and mirrored MPGD008, a diamond hole drilled down-dip approximately 40m south of the tenement boundary by KCGM in 2013 and which intersected significant gold mineralisation related to the 8 Mile mafic unit.
Unfortunately, GJRC029 deviated significantly from the planned azimuth and, as a result, by the time the hole was terminated at the target depth of 504m, the drill trace ended up approximately 75m north of the tenement boundary (Figure 2). Despite this, the hole intersected a thick section of the steep westerly- dipping and highly altered 8 Mile mafic unit with widespread sulphide mineralisation, including disseminated magnetite and coarse-grained arsenopyrite, pyrrhotite and chalcopyrite, similar to the 8 Mile Dam Deposit (Figure 3).
Based on visual logging of RC drill chips, handheld portable XRF results and magnetic susceptibility measurements, samples from the bottom 56m of the hole were sent for priority analysis by fire assay at Bureau Veritas in Kalgoorlie.
The results from these initial samples confirm the relationship between the gold mineralisation and sulphides, and a relationship between the best gold mineralisation and coincident magnetic anomalism and elevated Arsenic as measured by handheld portable XRF. The first results also confirm that the IP anomaly is associated with potentially significant gold mineralisation, whilst the significant deviation of GJRC029 away from the planned target increases the potential strike length of gold mineralisation on Miramar’s ground.
Significant results are listed in Table 1, with assay results from the remainder of the hole expected in coming weeks.
The initial RC drilling programme, which also tested two other IP targets, is nearing completion and results will be reported once received and compiled.
Once all assays are received, the Company will plan further RC and/or diamond drill holes including to test the dip and strike extent of the mineralisation intersected in GJRC029.
The Company advises that the WA Department of Mines, Petroleum and Exploration (DMPE) has extended the main Gidji JV tenement, E26/214, for a further five years, and will now expire in March 2030.
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This article includes content from Miramar Resources Limited, licensed for the purpose of publishing on Investing News Australia. This article does not constitute financial product advice. It is your responsibility to perform proper due diligence before acting upon any information provided here. Please refer to our full disclaimer here.
