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.