Cambodia – Pailin Sapphire and Battambang Ruby

Cambodian gem deposits from Pailin (basaltic sapphire and ruby) and Battambang (marble-hosted ruby); Khmer Rouge era hiatus; distinction from Thai material.

By gemmology.dev editors Last updated
cambodia pailin battambang sapphire ruby basaltic origin/cambodia

Introduction

Cambodia produces two geologically distinct types of corundum: basaltic sapphire
and ruby from Pailin Province (northwestern Cambodia), and small-scale marble-hosted
ruby from the Battambang area. The Pailin field sits in the same Southeast Asian
alkali basalt province as Thailand's Chanthaburi-Trat deposits, just across the
border. Production was severely disrupted during the Khmer Rouge era (1975–1979)
and the subsequent civil conflict, interrupting supply for two decades.

Geological Settings

Two corundum-forming environments in Cambodia:

Pailin – Basaltic Province

  • Cenozoic intraplate alkali basalt field; same Southeast Asian province as
    Chanthaburi-Trat (Thailand) and Ratanakiri (also Cambodia, for zircon)
  • Corundum transported to surface in basalt; concentrated in alluvial placers
  • High-Fe, low-Cr geochemical environment – same signature as Thai basaltic material
  • Adjacent to Bo Rai (Thailand); material from both sides historically mixed

Battambang – Marble-Hosted Ruby

  • Small-scale occurrence of marble-hosted ruby – geologically analogous to
    Mogok and Vietnam marble-type deposits
  • Low-Fe environment; strong fluorescence expected
  • Much smaller production volume than Pailin
  • Geologically distinct from the Pailin basaltic deposits

Khmer Rouge Era Hiatus

Pailin Sapphire and Ruby – Diagnostic Features

Characteristics of Pailin basaltic corundum:

Colour

  • Sapphire: Blue to green, yellow, and parti-colour; broad range typical
    of basaltic sapphires
  • Ruby: Dark red; comparable to Thai basaltic material but with subtle
    differences in trace element ratios

Chemistry and Spectroscopy

  • High Fe: Basaltic geochemical profile – >600 ppm Fe typical
  • Strong 450/460/470 nm triplet: Fe-related absorption in UV-Vis spectra,
    similar to Thai material
  • LWUV fluorescence: Weak; iron quenches chromium signal
  • Oxygen isotopes: Values consistent with basalt-related corundum

Inclusions

  • Basalt-suite minerals: zircon (with halos), feldspar, iron oxides (ilmenite)
  • Consistent with basaltic parentage – same mineral family as Thai material
  • No marble-hosted inclusions (no calcite, apatite, sphene)

Pailin vs Thai Distinction

Separating Cambodian Pailin from Chanthaburi-Trat:

  • Historical difficulty: Pailin and Bo Rai (Thailand) material was historically
    traded together through Chanthaburi and often mixed; laboratory separation was
    not routine
  • Modern LA-ICP-MS: Trace element ratio patterns (Ga/Mg, Fe/Ti, Cr/Ga) and
    oxygen isotope analysis can discriminate Pailin from Chanthaburi with some
    confidence; the separation is a laboratory-level task
  • Practical trade note: Material described as "Thai ruby" in the trade may
    include Cambodian origin stone heated in Thailand

Battambang Ruby Distinction