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
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0.2–1.0% Cu is the most common range
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0.3–0.6% Cu represents many operating porphyry mines
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>1.0% Cu occurs but usually only in the central high-grade core
Authoritative sources:
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USGS Porphyry Copper Deposit Model (Cox & Singer, 1992)
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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
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0.1–0.7 g/t Au in Cu-Au porphyries
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0.2–0.4 g/t Au most common
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<0.1 g/t Au in Cu-Mo porphyries (often negligible)
➤ High-Au Porphyry Examples
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Grasberg (Indonesia): 0.5–1.0+ g/t Au
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Cadia / Ridgeway (Australia): 0.5–1.5 g/t Au
References:
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Sillitoe, R.H., 2010, “Porphyry Copper Systems,” Economic Geology:
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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
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0.005–0.05% Mo in Cu-rich porphyries
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0.02–0.1% Mo in Cu-Mo porphyries
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0.1–0.3% Mo in Mo-rich porphyry systems (Climax-type)
Examples
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Bingham Canyon: ~0.03% Mo
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Climax (Colorado): >0.2% Mo (Mo-dominant system)
References:
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USGS Porphyry Copper and Molybdenum Deposit Models
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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
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Cu > 0.5%, even in short intervals
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Au > 0.3 g/t in Cu-Au systems
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Mo > 0.02% in Cu-Mo systems
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Increasing density of quartz-stockwork veining (A, B-veins)
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Potassic alteration (K-feldspar + biotite)
Peripheral/Zonal Indicators
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Cu < 0.2% usually indicates phyllic/propylitic halo
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Au often very low in outer zones
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Mo increases at depth in many systems

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