Pakistan vs Central Asia vs Africa: Where Does the Critical Minerals JV Money Actually Go?

Last month I sat across from a Shanghai off-take team who'd just come back from a site visit in the DRC. They'd flown 14 hours, driven another six on a broken road, and lost two days to a permit dispute they didn't see coming. Their lead engineer looked at me and said, "Sufyan, tell me why Gilgit-Baltistan is different."

That's the question worth answering properly. Not with a pitch deck. With numbers, geology, and the awkward stuff most people leave out.

I've spent the last few years watching serious capital circle three regions for critical minerals — Pakistan, Central Asia (mostly Kazakhstan and Uzbekistan, sometimes Tajikistan), and Africa (the copperbelt, plus Guinea, Tanzania, Mozambique, and yes, the DRC). Each has a real case. Each has a real problem. Honestly, the operators who pretend otherwise are the ones who blow up JV structures inside 18 months.

The Geology Isn't The Hard Part

Let's start with what's actually in the ground, because that's where the risk-reward conversation should begin and where it rarely does.

Africa's copperbelt is world-class. Nobody serious argues with that. Kamoa-Kakula is running head grades around 5.6% Cu, and Zambian assets sit comfortably in the 2-3% range. Central Asia has genuinely tier-one deposits too — Kazakhstan's Kounrad, Aktogay, and the tungsten-molybdenum belts around the Tien Shan are real. Uzbekistan's Almalyk complex has been producing copper and molybdenum since Soviet times.

Pakistan's Gilgit-Baltistan sits on the same structural continuation as the Tien Shan and the Karakoram-Himalayan collision zone. The mineralisation is there — porphyry copper systems, skarn tungsten, stibnite veins running 8-42% Sb in some of our Chilas-area samples, molybdenite associated with the Karakoram batholith intrusives. On the placer gold side, our recovery tests on Indus terraces around Bunji have shown 380-620 mg per cubic metre in the concentrated horizons. That's competitive with anything in Central Asia and better than most West African alluvials I've seen data on.

The geology isn't why one jurisdiction wins over another. The geology is roughly comparable across all three. What separates them is everything that happens after you find the rock.

Where The Real Difference Shows Up

Here's where I'll be direct.

Africa gives you grade and scale, but the political risk premium has climbed sharply in the last 36 months. Mali, Niger, Burkina Faso — military governments renegotiating contracts. Zambia's royalty regime has changed four times in ten years. The DRC's Code Minier revision in 2018 raised state carried interest and cobalt royalties overnight. If you're modelling a 15-year JV, that's a live variable you can't hedge out.

Logistics? Kolwezi to Dar es Salaam is roughly 2,000 km of road. Guinea's bauxite corridor works, but only because the Chinese built it. The DRC route through Lobito is improving. It's still not cheap.

Central Asia is politically more stable than a lot of people credit, but the export logistics are brutal. Landlocked. Every tonne moves through either Russia (increasingly compromised for Western buyers post-2022) or through the Middle Corridor across the Caspian, which is expensive and capacity-constrained. Kazakhstan's mining code is professional and predictable. But if you're an EU or US buyer trying to avoid Russian transit, your options narrow fast. And Chinese buyers are already deeply embedded — the competition for tier-one assets is intense and often already resolved before Western firms get a look.

Pakistan, specifically Gilgit-Baltistan, sits differently. We have a working port at Karachi, 1,750 km from our concessions via the Karakoram Highway and the N-35. That's a real road, upgraded under CPEC, open year-round except for maybe 8-15 days of winter closure at Khunjerab if you're going north. For south-bound export to Karachi, it's operational essentially year-round. Reko Diq — Barrick's project in Balochistan — just moved to construction with a $3 billion first-phase commitment. That's a signal. International capital is pricing Pakistan's mining risk lower than it did five years ago, and honestly, I think that repricing has further to run.

But I won't pretend it's frictionless. Security in some districts requires planning. GB's licensing sits with the GB Minerals Department under the 2003 Mining Concession Rules (amended), which is a provincial framework separate from federal — and that confuses newcomers. Currency controls on repatriation exist and need to be structured around from day one, not day 400.

How I'd Actually Rank The JV Risk-Reward

Look, if you want pure grade and don't mind political volatility, Africa still wins on copper and cobalt. If you want institutional predictability and don't mind logistics headaches (and don't mind competing with CNMC and Zijin for every good asset), Central Asia is defensible.

But for a buyer trying to build a diversified critical minerals book — copper, antimony, tungsten, moly, plus optional rare earths and lithium exposure from pegmatites we're still mapping — Pakistan gives you something the other two don't: an under-explored jurisdiction with tier-one geology, a functioning deep-water port, and asset entry prices that haven't yet been bid up by the majors.

I got this wrong at first, by the way. When I started structuring JV conversations three years ago, I was pitching on grade. That's the wrong lead. Buyers who've looked at 20 jurisdictions already know the grade story. What they want to know is: can I get the concentrate to Rotterdam, or Shanghai, or Yokohama, on a predictable schedule, at a landed cost that models out? Can I repatriate dollars? Will the concession still be mine in year seven?

Those are the questions. And on those, GB holds up better than the marketing suggests and better than most people assume.

What would actually change your mind if you're evaluating this seriously — a site visit, an independent QP report on our stibnite grades, or a look at the concession documentation itself?