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Friday, November 21, 2025

Typical Assay Ranges in Porphyry Copper Systems

 



Typical Assay Ranges in Porphyry Copper Systems

(Cu–Au–Mo porphyry deposits)

1. Copper (Cu) Grades

Porphyry copper deposits are low-grade, high-tonnage systems.

Typical Hypogene (Primary) Cu Grades

  • 0.2–1.0% Cu is the most common range

  • 0.3–0.6% Cu represents many operating porphyry mines

  • >1.0% Cu occurs but usually only in the central high-grade core

Authoritative sources:

  • USGS Porphyry Copper Deposit Model (Cox & Singer, 1992)

  • Geology for Investors – Porphyry Copper Deposits


2. Gold (Au) Grades

Gold varies widely depending on whether it is a Cu-Au or Cu-Mo system.

Typical Au Grades

  • 0.1–0.7 g/t Au in Cu-Au porphyries

  • 0.2–0.4 g/t Au most common

  • <0.1 g/t Au in Cu-Mo porphyries (often negligible)

High-Au Porphyry Examples

  • Grasberg (Indonesia): 0.5–1.0+ g/t Au

  • Cadia / Ridgeway (Australia): 0.5–1.5 g/t Au

References:

  • Sillitoe, R.H., 2010, “Porphyry Copper Systems,” Economic Geology:

  • USGS Open-File Report 2008-1155 (Deposit Model)


3. Molybdenum (Mo) Grades

Molybdenum occurs as molybdenite (MoS₂) and varies depending on deposit subtype.

Typical Mo Grades

  • 0.005–0.05% Mo in Cu-rich porphyries

  • 0.02–0.1% Mo in Cu-Mo porphyries

  • 0.1–0.3% Mo in Mo-rich porphyry systems (Climax-type)

Examples

  • Bingham Canyon: ~0.03% Mo

  • Climax (Colorado): >0.2% Mo (Mo-dominant system)

References:

  • USGS Porphyry Copper and Molybdenum Deposit Models

  • Singer et al. global porphyry Mo models


Summary Table (Typical Exploration Ranges)

Metal Typical Range in Porphyry Systems Notes
Cu 0.2–1.0% Most mines run 0.3–0.6% Cu
Au 0.1–0.7 g/t Higher in Cu-Au systems; very low in Cu-Mo porphyries
Mo 0.005–0.05% Higher (0.1–0.3%) in Mo-dominant porphyries

How to Interpret These in Exploration

These numbers guide exploration teams:

Strong Indicators You’re Approaching a Porphyry Core

  • Cu > 0.5%, even in short intervals

  • Au > 0.3 g/t in Cu-Au systems

  • Mo > 0.02% in Cu-Mo systems

  • Increasing density of quartz-stockwork veining (A, B-veins)

  • Potassic alteration (K-feldspar + biotite)

Peripheral/Zonal Indicators

  • Cu < 0.2% usually indicates phyllic/propylitic halo

  • Au often very low in outer zones

  • Mo increases at depth in many systems


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