Inclusion in emeralds

Содержание

Слайд 2

Natural Minute fluid inclusions parallel to the basal plane are the

Natural

Minute fluid inclusions parallel to the basal plane are the cause

of asterism
in this emerald from Madagascar. Thin-film interference causes
rainbow colors visible at high magnification. Field of view 1.8 mm.
Слайд 3

Well-formed octahedral crystals of pyrite are a welcome sight in this

Well-formed octahedral crystals of pyrite are a welcome sight in this
Colombian

emerald. Field of view 2.15 mm.
Слайд 4

Jagged three-phase inclusions consisting of salt solution, a gas bubble, and

Jagged three-phase inclusions consisting of salt solution, a gas bubble,
and a

salt crystal are commonly seen in Colombian emeralds. Field of
view 0.91 mm.
Слайд 5

The etched prism face of an emerald from Alexander County, North

The etched prism face of an emerald from Alexander County, North
Carolina,

is shown in false, high-contrast color using differential interference
contrast microscopy. Field of view 0.61 mm.
Слайд 6

Gota de aceite results from rapid columnar growth, causing a roiled

Gota de aceite results from rapid columnar growth, causing a roiled
appearance

in some Colombian emeralds. Field of view 2.60 mm.
Слайд 7

Brassy pyrite crystals are often seen in Colombian emeralds. Field of view 5.25 mm.

Brassy pyrite crystals are often seen in Colombian emeralds. Field of

view 5.25 mm.
Слайд 8

This complex blocky fluid inclusion contains a liquid, a gas, and

This complex blocky fluid inclusion contains a liquid, a gas, and

multiple
daughter crystals. Field of view 1.42 mm.
Слайд 9

Biotite crystals, shown here in polarized light, are common in emeralds

Biotite crystals, shown here in polarized light, are common in emeralds
from

schist-hosted deposits. Field of view 2.15 mm.
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This emerald from North Carolina contains vibrant orangy brown rutile inclusions. Field of view 6.25 mm.

This emerald from North Carolina contains vibrant orangy brown rutile
inclusions. Field

of view 6.25 mm.
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Amphibole crystals are occasionally seen in emeralds from Zambia. Field of view 1.72 mm.

Amphibole crystals are occasionally seen in emeralds from Zambia.
Field of view

1.72 mm.
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Skeletal platy crystals of ilmenite are scattered throughout this Zambian emerald. Field of view 1.91 mm.

Skeletal platy crystals of ilmenite are scattered throughout this Zambian
emerald. Field

of view 1.91 mm.
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This Colombian emerald shows prominent angular color zoning reminiscent of a

This Colombian emerald shows prominent angular color zoning reminiscent
of a mountain

range. Field of view 14.52 mm.
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Blocky three-phase inclusions are crystallographically aligned in this Brazilian emerald. Field of view 1.42 mm.

Blocky three-phase inclusions are crystallographically aligned in this
Brazilian emerald. Field of

view 1.42 mm.
Слайд 15

An inclusion suite often seen in Colombian emeralds consists of carbonates,

An inclusion suite often seen in Colombian emeralds consists of carbonates,
pyrite,

and fragments of black shale. Field of view 2.53 mm.
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Several rhombohedral magnesite crystals are present in this emerald from Santa

Several rhombohedral magnesite crystals are present in this emerald
from Santa Terezinha

de Goiás, Brazil. Field of view 8.68 mm.
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Tremolite inclusions are densely packed in this emerald from Zimbabwe. Field of view 0.86 mm.

Tremolite inclusions are densely packed in this emerald from Zimbabwe.
Field of

view 0.86 mm.
Слайд 18

A very rare inclusion of parisite is diagnostic of Colombian origin. Field of view 0.82 mm.

A very rare inclusion of parisite is diagnostic of Colombian origin.
Field

of view 0.82 mm.
Слайд 19

This Colombian emerald contains a carbonate crystal that is included with

This Colombian emerald contains a carbonate crystal that is included
with a

pyrite crystal. Field of view 2.34 mm.
Слайд 20

A rare inclusion of purple fluorite is seen in high contrast

A rare inclusion of purple fluorite is seen in high contrast

to its green
emerald host. Field of view 2.34 mm.
Слайд 21

Russian emeralds often host brightly colored reflective thin-film fluid inclusions. These

Russian emeralds often host brightly colored reflective thin-film fluid
inclusions. These are

oriented perpendicular to the optic axis. Field of
view 2.15 mm.
Слайд 22

Treated Clarity-enhancing resin showing a flow structure is present in the

Treated

Clarity-enhancing resin showing a flow structure is present in the fracture
of

a natural emerald. Field of view 3.75 mm.
Слайд 23

A partially filled fracture shows vibrant interference colors in the unfilled

A partially filled fracture shows vibrant interference colors in the unfilled
areas

and a dendritic pattern where the oil filler has wicked into
the fracture, reducing its visibility. Field of view 6.40 mm.
Слайд 24

A large pocket filled with brown oil and a trapped gas

A large pocket filled with brown oil and a trapped gas

bubble in a natural
emerald. Field of view 1.72 mm.
Слайд 25

A well-filled fracture displays the diagnostic blue flash effect, which confirms

A well-filled fracture displays the diagnostic blue flash effect, which
confirms clarity

enhancement. Field of view 2.50 mm.
Слайд 26

Gentle heating along a surface-reaching fracture causes oil to bead on

Gentle heating along a surface-reaching fracture causes oil to bead on
the

surface, proving the emerald is clarity enhanced. Field of view
1.72 mm.
Слайд 27

Synthetic Nail-head spicules, as seen in this Regency hydrothermal synthetic emerald,

Synthetic

Nail-head spicules, as seen in this Regency hydrothermal synthetic
emerald, are indicative

of synthetic origin. Field of view 1.42 mm.
Слайд 28

Healed whitish feather-like inclusions of flux residue are present in this

Healed whitish feather-like inclusions of flux residue are present in
this Gilson

synthetic emerald. Field of view 4.75 mm.
Слайд 29

Flux residue often contains a contraction bubble, as seen in each

Flux residue often contains a contraction bubble, as seen in each

of
these trapped flux droplets. Field of view 1.08 mm
Слайд 30

Synthetic phenakite crystals are often a by-product of synthetic emerald growth

Synthetic phenakite crystals are often a by-product of synthetic emerald
growth and

can easily be mistaken for natural inclusions. Field of
view 2.90 mm.
Слайд 31

This roiled, chevron-like growth is characteristic of hydrothermally grown synthetic emeralds. Field of view 1.72 mm.

This roiled, chevron-like growth is characteristic of hydrothermally
grown synthetic emeralds. Field

of view 1.72 mm.