Содержание
- 2. Natural Minute fluid inclusions parallel to the basal plane are the cause of asterism in this
- 3. Well-formed octahedral crystals of pyrite are a welcome sight in this Colombian emerald. Field of view
- 4. Jagged three-phase inclusions consisting of salt solution, a gas bubble, and a salt crystal are commonly
- 5. The etched prism face of an emerald from Alexander County, North Carolina, is shown in false,
- 6. Gota de aceite results from rapid columnar growth, causing a roiled appearance in some Colombian emeralds.
- 7. Brassy pyrite crystals are often seen in Colombian emeralds. Field of view 5.25 mm.
- 8. This complex blocky fluid inclusion contains a liquid, a gas, and multiple daughter crystals. Field of
- 9. Biotite crystals, shown here in polarized light, are common in emeralds from schist-hosted deposits. Field of
- 10. This emerald from North Carolina contains vibrant orangy brown rutile inclusions. Field of view 6.25 mm.
- 11. Amphibole crystals are occasionally seen in emeralds from Zambia. Field of view 1.72 mm.
- 12. Skeletal platy crystals of ilmenite are scattered throughout this Zambian emerald. Field of view 1.91 mm.
- 13. This Colombian emerald shows prominent angular color zoning reminiscent of a mountain range. Field of view
- 14. Blocky three-phase inclusions are crystallographically aligned in this Brazilian emerald. Field of view 1.42 mm.
- 15. An inclusion suite often seen in Colombian emeralds consists of carbonates, pyrite, and fragments of black
- 16. Several rhombohedral magnesite crystals are present in this emerald from Santa Terezinha de Goiás, Brazil. Field
- 17. Tremolite inclusions are densely packed in this emerald from Zimbabwe. Field of view 0.86 mm.
- 18. A very rare inclusion of parisite is diagnostic of Colombian origin. Field of view 0.82 mm.
- 19. This Colombian emerald contains a carbonate crystal that is included with a pyrite crystal. Field of
- 20. A rare inclusion of purple fluorite is seen in high contrast to its green emerald host.
- 21. Russian emeralds often host brightly colored reflective thin-film fluid inclusions. These are oriented perpendicular to the
- 22. Treated Clarity-enhancing resin showing a flow structure is present in the fracture of a natural emerald.
- 23. A partially filled fracture shows vibrant interference colors in the unfilled areas and a dendritic pattern
- 24. A large pocket filled with brown oil and a trapped gas bubble in a natural emerald.
- 25. A well-filled fracture displays the diagnostic blue flash effect, which confirms clarity enhancement. Field of view
- 26. Gentle heating along a surface-reaching fracture causes oil to bead on the surface, proving the emerald
- 27. Synthetic Nail-head spicules, as seen in this Regency hydrothermal synthetic emerald, are indicative of synthetic origin.
- 28. Healed whitish feather-like inclusions of flux residue are present in this Gilson synthetic emerald. Field of
- 29. Flux residue often contains a contraction bubble, as seen in each of these trapped flux droplets.
- 30. Synthetic phenakite crystals are often a by-product of synthetic emerald growth and can easily be mistaken
- 31. This roiled, chevron-like growth is characteristic of hydrothermally grown synthetic emeralds. Field of view 1.72 mm.
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