T263 Gem Minerals, Localities and Geological Significance (Posters)
Wednesday, 25 September 2024
8:00 AM - 5:30 PM
Hall D
LARGE NATURALLY GROWN DIAMONDS WITH TREATED PINK COLOR
Paper number: T263-6
Program: Technical Sessions
Time: 8:00 AM – 5:30 PM
Authors
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Madelyn DragoneGemological Institute of America, New York Laboratory, New York, NY
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Tingyen YehGemological Institute of America, New York Laboratory, New York, NY
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A’Dhi LallGemological Institute of America, New York Laboratory, New York, NY
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Luke ScintoGemological Institute of America, New York Laboratory, New York, NY
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Ulrika D’Haenens-JohanssonGemological Institute of America, New York Laboratory, New York, NY
Abstract
FTIR spectra revealed that they are type IIa and type Ib diamonds. These types of diamonds can possess vacancy clusters which produce an unattractive brown color. Spectral evidence suggests that the first step in the treatment sequence was annealing at high pressure and high temperature (HPHT), which is known to break apart the vacancy clusters and reduce the brown color. HPHT treatment created H2 (NVN-) centers which can be observed in photoluminescence spectra. Then, they were artificially irradiated to generate vacancy centers. Finally, these diamonds were annealed at lower temperatures (> 600 °C) so that vacancies became mobile, migrating till they were trapped at nitrogen atoms to form NV centers. Strong absorption at 637 nm (NV-) and its side bands in UV-Visible spectra confirm they are responsible for their saturated pink color.
Multi-treatment for pink color production has been reported since the 1950s, yet the 33.07 and 55.55 cts stones mark the largest treated pink diamonds submitted to GIA. They also highlight the boldness of treaters as the original diamonds – irrespective of color – would have considerable value due to their size. Since the 2020 closure of the Argyle mine, the largest supplier of natural pink diamonds, it is possible that the proportion of notable treated pink, mined or laboratory-grown, diamonds may increase to meet demand.
Geological Society of America Abstracts with Programs. Vol. 56, No. 5
doi: 10.1130/abs/2024AM-404194
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