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 Fabian Moor 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 [1]
  • 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 [4][5]
  • 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 [2]
  • 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

References

  1. 1. Giuliani, G. (2015). Fluid inclusions in ruby from Asian marble deposits. European Journal of Mineralogy. DOI: 10.1127/ejm/2015/0027-2442.
  2. 2. Shor, R.; Weldon, R. (2009). Ruby and Sapphire Production and Distribution: A Quarter Century of Change. Gems & Gemology, 45(4), 236–259. DOI: 10.5741/gems.45.4.236.
  3. 3. Global Witness (1995). Rough Trade: The Role of Companies and Governments in the Angolan Conflict. Global Witness Ltd.. https://www.globalwitness.org
  4. 4. Palke, A.; Saeseaw, S.; Renfro, N.; Sun, Z.; McClure, S. (2019). Geographic Origin Determination of Blue Sapphire. Gems & Gemology, 55(4), 536–579. DOI: 10.5741/gems.55.4.536.
  5. 5. Keller, P. (1982). The Chanthaburi-Trat Gem Field, Thailand. Gems & Gemology, 18(4), 186–196. DOI: 10.5741/gems.18.4.186.