Author name: William B. Simmons

Granitic Pegmatites as Sources of Colored Gemstones

Pegmatites are sources of gem-quality crystals of beryl, tourmaline, topaz, spodumene, and spessartine. Historic localities are found in Brazil, Madagascar, Russia, and the United States, but important deposits have recently been discovered in Africa and Asia. Most high-quality gem minerals occur in miarolitic cavities found near the centers of pegmatite bodies or in reaction zones between pegmatites and ultramafi c host rocks. The most important gem-bearing granitic pegmatites formed at shallow levels in the continental crust during the latest stages of collisional plate tectonic events. Single, spectacular miarolitic cavities in some pegmatites have produced tons of gem crystals valued in excess of $50 million.

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Laboratory-Treated Gemstones

Treatment processes to improve the color, appearance, and/or durability of certain gemstones have been used for hundreds of years, and their variety, sophistication, and application within the jewelry trade have increased over the past several decades. Whether or not these enhancement processes are considered acceptable trade practices, their use must legally be disclosed at the time of gemstone sales. Disclosure of treatment information requires that treated gems be correctly identified by gemologists and gemtesting laboratories. Treatment detection is based upon careful documentation of the properties of gem materials, including the use of advanced nondestructive techniques for obtaining chemical and spectral data.

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High-Pressure High Temperature Treatment of Gem Diamonds

Annealing of gem-quality diamonds at very high pressures (above 5 GPa) and temperatures (above ~1800°C) can produce significant changes in their color. Treatment under these high-pressure–high- temperature (HPHT) conditions affects certain optically active defects and their absorptions in the visible spectrum. In the jewelry industry, laboratory- treated diamonds are valued much less than those of natural color. Polished diamonds are carefully examined at gemological laboratories to determine the “origin of color” as part of an overall assessment of their quality. Currently, the recognition of HPHT-treated diamonds involves the determina- tion of various visual properties (such as color and features seen under magnification), as well as characterization by several spectroscopic tech- niques. HPHT-treated diamonds were introduced into the jewelry trade in the late 1990s, and despite progress in their recognition, their identification remains a challenge. While some detection methodologies have been estab- lished, the large number of diamonds requiring testing with sophisticated analytical instrumentation poses a logistical problem for gemological laboratories.

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