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Material World
Deposit type

Porphyry copper deposit

A whole intrusion shot through with copper at a fraction of a per cent — low grade, enormous, and the source of most of the world's copper and molybdenum.

Ore

A porphyry deposit is the opposite of a vein in every way that matters. Instead of a sharply bounded fracture at high grade, it is a body of intrusive rock a kilometre or more across, veined through with a stockwork of hairline fractures, carrying copper at somewhere between a quarter and one per cent.

That is a grade nobody could mine by hand and nobody needed to until the twentieth century. What made it ore was scale: open-pit mining, flotation, and machinery large enough that moving a hundred tonnes of rock to recover half a tonne of copper is economic.

How it forms

The deposit forms where a water-rich magma crystallising at a few kilometres' depth reaches the point at which it can hold no more dissolved water. The fluid separates violently, fractures the rock around and above it, and deposits metal sulfides through the resulting network as it cools.

Alteration zones ring the centre in a pattern regular enough to navigate by — potassic in the core, phyllic outside it, propylitic beyond — and mapping which zone you are standing in is how the centre is found. That regularity is what made porphyry deposits the first ore bodies to be genuinely modelled rather than merely followed.

Weathering then rearranges the top. Sulfides near the surface oxidise, copper is dissolved and carried down, and it reprecipitates below the water table as a supergene blanket several times richer than the primary rock — which is the part most porphyry mines started on.

Economic significance

Something like three quarters of world copper and most of its molybdenum comes from this one deposit type, concentrated along the subduction margins of the Americas and the western Pacific. Rhenium arrives with the molybdenum, which is why an element with almost no ore body of its own has a supply at all.

The economics are entirely about scale and grade decline. Average copper grades have fallen for a century while production has risen, which works only because equipment has grown and flotation has improved — and it makes energy the dominant input cost of the industry rather than the metal being scarce.

Medium confidence Weak evidence

How we know: checked recently · only one source, so there is nothing to cross-check it against · stated directly by the source.

How this connects

Where a connection has been confirmed by an outside reference, that reference is named beside it.

is composed of

  • Chalcopyrite mineral · the primary copper sulfide, dispersed through a stockwork of hairline fractures at a fraction of a per cent
  • Molybdenite mineral · the reason most molybdenum is a copper by-product — and, through the rhenium it carries, the reason rhenium has a supply
  • Pyrite mineral · abundant and worthless in itself, and the mineral whose oxidation generates the acid that makes the oxidised zone above

is sourced from

  • Granite rock · an intrusion of granitic composition, fractured and altered by fluid separating out of it as it crystallised

is a source for

  • Oxidised zone deposit type · the weathered cap of a sulfide body rather than a deposit in its own right: the same metal, rebuilt in place by air and water

Sources

  • Wikimedia Foundation · Creative Commons CC0 1.0 Universal (public domain dedication)
  • Material World
    Our own writing

Where it comes from, and what it becomes

Follow Porphyry copper deposit back to what it starts as, and forward into what it becomes. Each step is a documented one — a real route material takes, not a chain of inference.

Upstream — what it comes from

  • Porphyry copper deposit → is sourced from (an intrusion of granitic composition, fractured and altered by fluid separating out of it as it crystallised) → Granite → is composed of (by volume, alongside feldspar and lesser mica) → Quartz
  • Porphyry copper deposit → is composed of (the primary copper sulfide, dispersed through a stockwork of hairline fractures at a fraction of a per cent) → Chalcopyrite
  • Porphyry copper deposit → is composed of (abundant and worthless in itself, and the mineral whose oxidation generates the acid that makes the oxidised zone above) → Pyrite
  • Porphyry copper deposit → is composed of (the reason most molybdenum is a copper by-product — and, through the rhenium it carries, the reason rhenium has a supply) → Molybdenite
  • Porphyry copper deposit → is sourced from (an intrusion of granitic composition, fractured and altered by fluid separating out of it as it crystallised) → Granite → is composed of (the pink or cream mineral that gives much granite its colour) → Orthoclase
  • Porphyry copper deposit → is sourced from (an intrusion of granitic composition, fractured and altered by fluid separating out of it as it crystallised) → Granite → is composed of (one of the two common micas in granite, alongside biotite) → Muscovite

These are the most distinct paths back. Porphyry copper deposit can be traced through others besides.

Downstream — what it becomes

  • Porphyry copper deposit → is a source for (the weathered cap of a sulfide body rather than a deposit in its own right: the same metal, rebuilt in place by air and water) → Oxidised zone