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.
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
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
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