Thailand – Gem Origins Overview

Southeast Asian gem province centred on Chanthaburi, Trat, Kanchanaburi, Bo Phloi, and Bo Rai; world leader in corundum heat treatment and trading.

By Fabian Moor Last updated
thailand chanthaburi trat kanchanaburi basaltic origin/thailand

Introduction

Thailand hosts one of Southeast Asia's most important gem-producing and gem-processing
provinces, centred on Cenozoic alkali basalt fields in the east (Chanthaburi-Trat) and
west (Kanchanaburi). Bo Rai, Trat Province, was the dominant global ruby source during
the 1970s–1980s; Keller (1982) noted Thailand had become "the world's major source of
gem ruby" after Mogok's decline. [1]

Diagnostic significance for Thai corundum is the basaltic geochemical signature: high
iron (above 600 ppm), a strong 451/460/470 nm iron absorption triplet, and weak to
inert long-wave UV fluorescence, contrasting sharply with marble-hosted material from
Mogok or Kashmir. Basalt-suite inclusions (zircon with radiation halos, ilmenite,
enstatite, feldspar) confirm geological parentage.

Though Bo Rai is largely exhausted, Bangkok and Chanthaburi remain the world's dominant
corundum trading and heat-treatment centres, processing rough from Cambodia, Vietnam,
Burma, and East Africa. [2] Thailand is also the
global hub for blue zircon, converting Cambodian rough by oxidising heat treatment.
[3]

Geological Context

All Thai corundum deposits share a basaltic origin:

Basaltic Province

  • Setting: Cenozoic intraplate alkali basalt fields along the Indochina block
  • Age: Neogene to Quaternary volcanic activity
  • Transport: Corundum crystallised at mantle depth and was transported to
    the surface by alkali basalt magmas
  • Concentration: Gems accumulate in alluvial and eluvial placers derived
    from weathered basalt
  • Chemistry: Basaltic environment imposes high-Fe, low-Cr signature on
    corundum – the defining geochemical contrast with marble-hosted Mogok ruby

Tectonic Context

  • Post-subduction intraplate extension of the Indochina microplate
  • Multi-stage sapphire formation at Bo Phloi reflects separate pulses
    of basaltic magmatism
  • Same Southeast Asian alkaline basalt province as Cambodian Pailin field;
    deposits merge across the border

Mining Areas

District Province Products Status
Bo Rai Trat Ruby (historic 'Siam ruby') Largely exhausted
Bo Welu / Khlung Chanthaburi Ruby, blue/yellow sapphire Limited activity
Bo Phloi Kanchanaburi Blue and yellow sapphire Mostly closed, well-studied
Kanchanaburi town area Kanchanaburi Blue sapphire Historic

Production History

Thailand's rise and evolution as a gem hub:

Rise to Prominence

  • 1970s–1980s: Thailand became the world's dominant ruby source after Mogok
    production declined; Keller (1982) noted Thailand had become "the world's
    major source of gem ruby" following "the recent drastic decline in production
    from the classic ruby mines of Burma" [1]
  • Bo Rai ruby production peaked in the 1970s–1980s; now essentially exhausted

Treatment and Trading Hub

  • Bangkok and Chanthaburi developed into the world's dominant ruby and sapphire
    heat-treatment and trading centres
  • Thailand pioneered the technology of heating Thai and Burmese rough to dissolve
    silk and improve colour [2]
  • Material from Thailand, Cambodia, Vietnam, Burma, and East Africa is routinely
    treated and traded through Chanthaburi

Zircon Trade Hub

Beyond ruby and sapphire, Thailand is the global centre for blue zircon production:

  • Cambodian and Vietnamese zircon rough is imported to Chanthaburi and Bangkok
  • Heat treatment in oxidising conditions at 900–1000°C converts brownish rough
    to the prized "blue zircon" colour [3]
  • Thailand exports the majority of the world's faceted blue zircon

Basaltic vs Marble-Hosted Corundum

References

  1. 1. Keller, P. (1982). The Chanthaburi-Trat Gem Field, Thailand. Gems & Gemology, 18(4), 186–196. DOI: 10.5741/gems.18.4.186.
  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. Read, P. (2014). Gemmology (3rd ed.). Butterworth-Heinemann. DOI: 10.4324/9780080507224.