HR: 0800h
AN: V41A-1437 [Abstracts]
TI: Golconda Diamonds From Old Mines: Windows of Earth's Mantle Below the Deccan
AU: * Leung, I
EM: irene.leung@lehman.cuny.edu
AF: Department of Geology, Lehman College/CUNY, 250 Bedford Park Blvd. West, Bronx, NY 10468
United States
AU: Tsao, C
EM: cstsao@juno.com
AF: Linus Pauling Institute of Science and Medicine, 440 Page Mill Road, Palo Alto, CA 94306
United States
AB:
During the last seven years, we collected 59 flat rose-cut diamonds previously used in Mogul jewelry worn by kings and
noblemen in India. The cutting style indicates that they were made at least one or two centuries ago, and the diamonds were
most likely produced in areas near River Krishna on the Deccan Plateau where Golconda was the diamond trading center. Some of
the diamonds are up to 1 cm in size, and several flat plates appear to be serial sections of a very large stone, because
they yielded identical Fourier-Transform infrared (FTIR) spectra. These samples gave us an opportunity to study very large
diamond crystals at a relatively affordable cost.
We present here our prliminary results. An FTIR study showed that almost all the samples are Type Ia diamonds whose nitrogen
aggregation state is A, with a minor component of the B aggregate. The spectra of most diamonds show a sharp hydrogen peak at
wavenumber 3107, and several small peaks just below wavenumber 3000, due to the presence of hydrocarbon molecules. Mineral
inclusions are eclogitic, represented by orange garnets and pale green omphacitic pyroxene. Only one diamond contains 11
crystals of olivine. Similarities among the diamonds are surprising, because they were acquired from different vendors at
different times. We speculate that Earth's mantle in this region might be uniform chemically, or, the diamonds came from a
single productive mine.
DE: 1025 Composition of the mantle
DE: 3934 Optical, infrared, and Raman spectroscopy
DE: 8124 Earth's interior: composition and state (1212, 7207, 7208, 8105)
SC: Volcanology, Geochemistry, Petrology [V]
MN: Fall Meeting 2005