Volume 24, Number
7, July - September 2011
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- Serpentine crystal with purple-red transmission
- High quality synthetic yellow orange diamond emerges in China
- Gem-quality green and blue tourmaline from a Coolgardie pegmatite,
Western Australia
- Less frequently encountered gemstones - Painite
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Front cover image:
Pin fire tourmaline from Coolgardie pegmatite, Western
Australia. Photo by F. Payette
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(Follow this link for abstracts of past issues)
Serpentine crystal with
purple-red transmission
Gagan Choudhary
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ABSTRACT
One dark bluish green serpentine specimen weighing
approximately 19.52 grams was encountered at the Gem Testing
Laboratory Jaipur, India. The specimen was unusual for its crystal
form and purple-red transmission in strong light. Serpentine, which is
usually found as massive boulders, was seen here as a crystal with
bladed habit and displayed fine striations on the surface due to
cleavages. Further, this crystal also displayed a strong purple-red
transmission in strong light; the effect was mistaken for
colour-change effect and the sample was misrepresented as alexandrite.
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The serpentine specimen appeared
purple-red when observed in strong transmitted light; an unusual
phenomenon for serpentine. This effect is mistaken for a colour-change
effect and such specimens are misrepresented as alexandrite.
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High quality synthetic
yellow orange diamond emerges in China
Song
Zhonghua, Lu Taijin, Shen Meidong, Su Jun and Shang Jingjing

The 1.57 ct orange yellow synthetic diamond.
Photomicrograph by Song Zhonghua.
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ABSTRACT
In recent years, the commercial availability of
gem-quality synthetic yellow diamonds has caused great concern in the gem
and jewellery industry. To accurately identify synthetic yellow diamonds
grown by HPHT techniques, the gemmological characteristics of gem-quality
synthetic diamonds available in China are given and discussed. The
DiamondViewTM imaging system, photoluminescence (PL)
spectroscopy, as well as microscopy, are the most useful techniques for an
effective identification. The presence of peaks at 727 nm, 747 nm, and 753
nm (due to nickel) in the PL spectrum provides evidence of the synthetic
origin.
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Gem-quality
green and blue tourmaline from a Coolgardie pegmatite, Western Australia
Francine
Payette and Dr Leonhard Klemm
ABSTRACT
In
Western Australia, the Coolgardie pegmatite field is best known for
its world-class specimens of ferrocolumbite that have been mined for
many decades from the Giles beryl-columbite pegmatite at Spargoville.
Recently, gemmy green and blue tourmalines have been found in a
pegmatite south of the beryl-columbite pegmatite.
The
tourmalines were analysed using standard gemmological instruments, and
their chemical composition was determined by LA-ICP-MS. The
gemmological and spectroscopic properties of tourmaline from this
locality are consistent with properties of tourmaline from other
localities worldwide. The LA-ICP-MS analyses indicate that the
tourmalines are predominantly elbaite with subordinate foitite and
some minor olenite and schorl components.
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A representative selection of
Coolgardie tourmaline colours. Length of blue rectangular step cut
specimen at right, 10.5 mm. Photo by F. Payette.
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Less frequently
encountered gemstones - Painite
Rod Brightman
ABSTRACT
Mention painite to most gemmologists prior to 2002 and they would have
immediately thought of the world’s rarest gemstone. Originally
described by Claringbull et al. (1957), and named after the famous
mineralogist and gemmologist Arthur Charles Davy Pain who first
identified it as samples of an unknown mineral in 1952, only three
rough crystal specimens were known until a new occurrence was located
in 2002. Between 2001 and 2005 extensive exploration in the Mogok area
of northern Myanmar (Burma), resulted in several thousand specimens
being located, although most of these were non-gemmy. Most are
fragments with well-formed crystals being quite rare and of these,
relatively few have been faceted into transparent gemstones. Gemmy
faceted specimens would still have to be regarded as an extremely rare
collector gemstone and up until 2004 there were only two known faceted
specimens.
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Polysynthetic
twin lamellae viewed through the crown facets of the painite (0.79
ct). Photo by F. Payette.
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