Solid Inclusions

Crystal inclusions - identifying mineral guests trapped within gemstones during formation.

microscopy identification crystals origin

Introduction

Solid inclusions are crystals of other minerals trapped during the host gem's growth.
They are typically protogenetic (formed before the host) or syngenetic (formed at the
same time). These mineral "guests" provide crucial evidence for identification and
origin determination.

Common Solid Inclusions by Host Gem

Diagnostic Crystal Inclusions
Host Gem Common Solid Inclusions Significance
Ruby/Sapphire Rutile silk, zircon halos, calcite, apatite Origin indicators
Emerald Pyrite, calcite, tremolite, mica, chromite Origin-diagnostic
Diamond Garnet, olivine, chromite, graphite Mantle origin proof
Peridot Chromite (black crystals), ludwigite needles Species-diagnostic
Garnet Rutile, apatite, rounded crystals Varies by species
Spinel Octahedral crystals, zircon, calcite, apatite Natural indicator
Tourmaline Trichites, growth tubes Common features

Corundum (Ruby & Sapphire)

Rutile Inclusions

Rutile (TiO2) is the most common solid inclusion in corundum:

  • Short silk - Fine, short needles (Burmese origin indicator)
  • Long silk - Longer needles at 60° angles (Sri Lankan indicator)
  • Dense networks - Heavy silk coverage (Thai/Cambodian stones)
  • Dissolved silk - Dotted remnants indicate heat treatment

Other Crystal Inclusions

Inclusion Appearance Origin Significance
Zircon with halos Round crystals with stress fractures Common, suggests high-temp formation
Calcite Rhombohedral crystals Burmese ruby indicator
Apatite Hexagonal prisms Common in many origins
Boehmite needles Fine, oriented needles Heat treatment indicator
Spinel Octahedral crystals Occasionally seen

Emerald Crystal Inclusions

Emerald inclusions vary significantly by origin and provide key diagnostic evidence.

Emerald Solid Inclusions by Origin
Origin Characteristic Crystals
Colombia Calcite rhombs, pyrite cubes, albite
Zambia Black mica flakes, amphibole needles, blocky crystals
Brazil Biotite mica, pyrite, chromite
Afghanistan Mica books, actinolite needles
Russia (Urals) Actinolite, mica, chlorite

Diamond Crystal Inclusions

Diamond inclusions provide information about formation conditions deep in the
Earth's mantle. They are syngenetic, crystallizing alongside the diamond.

Inclusion Appearance Significance
Garnet (pyrope) Red or orange crystals Peridotitic environment
Olivine Green crystals Common mantle mineral
Chrome diopside Green crystals Eclogitic environment
Chromite Black, opaque Very common
Graphite Black, metallic Same carbon, different structure
Diamond-in-diamond Colourless crystal Growth interruption

Garnet Family Inclusions

Demantoid Garnet

Demantoid (andradite) from Russia shows the diagnostic "horsetail" inclusion:

  • Horsetail: Radiating fibres of byssolite (actinolite)
  • Fibres curve outward from central point
  • Diagnostic for Russian (Ural) demantoid
  • Namibian demantoid may lack horsetails

Tsavorite Garnet

Tsavorite (green grossular) from East Africa shows:

  • Graphite plates: Flat, dark inclusions
  • Actinolite needles: Elongated crystals
  • Growth tubes: Hollow channels
  • Generally cleaner than hessonite

Other Garnets

Species Common Crystal Inclusions
Rhodolite Rutile needles, apatite crystals, zircon
Almandine Rutile silk, quartz, apatite
Pyrope Often eye-clean; chrome diopside, olivine
Spessartine Apatite, quartz crystals

Spinel Crystal Inclusions

Inclusion Description
Octahedral crystals Small spinel crystals within host
Zircon with halos Radiation damage halos around zircon
Calcite Rhombohedral crystals
Apatite Hexagonal prisms
Graphite Flat, dark plates

Identification Value