Gilgit-Baltistan's Critical Minerals Corridor: A Geological and Commercial Overview

I'm writing this from Gilgit, about 40 hours after coming down from a molybdenum showing north of Bunji where our field team pulled a channel sample assaying 0.14% Mo over 3.2 metres. Nothing dressed up. Just a rock hammer, a chain, and a technician who's been mapping these valleys for 22 years.

That's the honest starting point for any conversation about Gilgit-Baltistan's mineral endowment. The rocks are extraordinary. The paperwork is real. And the buyers who understand both are the ones we want at the table.

Why This Ground, and Why Now

Gilgit-Baltistan sits at the collision zone of the Indian and Eurasian plates — the Kohistan Island Arc suture, the Karakoram batholith, and the Nanga Parbat–Haramosh massif all crash together here. For a geologist, it's one of the most fertile stretches of crust on the planet. For a buyer worried about antimony export bans out of China or tungsten concentrate coming out of politically difficult jurisdictions, it's something more practical: a supply option that isn't Russia, isn't Myanmar, isn't the DRC.

Our 16 concessions cover roughly 1,847 square kilometres across four districts — Ghizer, Gilgit, Skardu and Diamer. They're held under valid Exploration Licences and Mineral Deposit Retention Licences issued by the Gilgit-Baltistan Minerals Investment Facilitation Authority (GB-MIFA), the successor framework that came in after the 2018 GB Mines and Minerals Act. Foreign equity up to 100% is permitted. Royalties sit between 2% and 5% depending on the commodity. I've written elsewhere about the tax and repatriation side, so I won't repeat it here.

What I want to walk through is what's actually in the ground.

The Portfolio, Commodity by Commodity

Copper and gold. Six of our concessions sit on the western flank of the Karakoram batholith, in a belt that shares intrusive geochemistry with the Reko Diq porphyry system 900 km south in Balochistan. Surface sampling on our Chalt-area block returned copper values ranging from 0.31% to 1.8% Cu with associated gold running 0.4 to 2.7 g/t. Two of these blocks also carry visible molybdenite in the potassic alteration zones — classic porphyry indicators. We haven't drilled yet. That's exactly the kind of capex a JV partner brings.

Antimony. This is the one Western defence buyers keep calling about, and I understand why. China's export controls kicked in September 2024 and stibnite concentrate pricing more than doubled inside six months. We control two stibnite-bearing structures in the Ishkoman valley with grab samples running 18% to 47% Sb. Small tonnage by porphyry standards, but antimony deposits are always small — and the grade here is genuinely competitive with what Tajikistan is shipping.

Tungsten and molybdenum. Skarn and greisen occurrences on the margins of the Karakoram plutons. Scheelite has been identified under UV in three separate localities. Molybdenum, as I mentioned, is showing up both in porphyry settings and in quartz-vein systems near Bunji. Both metals are on the US, EU and UK critical minerals lists. Both feed defence and clean-energy supply chains that are actively trying to de-risk from single-country sourcing.

Nephrite jade. Our Skardu and Bunji blocks produce high-grade nephrite — the tight, waxy, translucent material that the Chinese market pays serious money for. We're already moving parcels to buyers in Xinjiang and Guangzhou. This is one of the few commodities in the portfolio generating cash flow today rather than tomorrow.

Gold — placer and lode. The Indus, Gilgit and Hunza rivers have been worked for alluvial gold for centuries. We hold placer rights on defined stretches with historical recovery data. Lode targets sit upstream in the same drainages. Nothing exotic here — just gravity plants and, eventually, hard-rock development.

Lead, silver, bauxite, and the exploration tail. Two concessions carry galena-sphalerite mineralisation with silver credits. One block in Diamer has bauxite outcrops we're still evaluating. And we're actively prospecting for lithium-bearing pegmatites — the LCT pegmatite fields in Afghanistan continue across this border geologically, though I'll be the first to say we don't have confirmed spodumene yet. Anyone who tells you they do without XRD data is selling you something.

The Commercial Side — What Actually Matters to a Buyer

Look, geology gets people excited. Logistics is what kills deals. So here's the honest picture.

Concentrate moves from GB by road down the Karakoram Highway to Islamabad, then either west to Karachi port (about 1,600 km total) or, for China-bound cargo, north through the Khunjerab Pass to Kashgar. Khunjerab closes roughly four months a year for snow. Karachi is year-round. We've moved jade samples and rock parcels through both routes and I'd rate the Karachi option as the more reliable one for bulk concentrate, at least until CPEC upgrades the northern corridor further.

Power on-site is the honest constraint. Most concessions are off-grid. Any serious operation is planning around hybrid diesel-solar or micro-hydro — several of our blocks sit near existing run-of-river hydro that could be tapped with the right agreements.

Security is better than the international headlines suggest. GB is not Balochistan and it's not KP tribal areas. It's a tourism region. Our field crews work with local labour drawn from the same valleys we're operating in, which honestly matters more for project continuity than any private security arrangement.

I used to think the hardest part of this business was finding the mineralisation. After eight years, I've changed my mind. The hardest part is finding partners who understand that a Pakistani concession isn't a stock ticker — it's a rock, in a valley, that someone has to actually go and dig. If that's the kind of partner you are, our data room is open.

What would you want to see first — the porphyry blocks, or the antimony?