Modelling the combination of birefringence retardations from strain envelopes around multiple inclusions in diamond |
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| Authors: | L M Barron B J Barron T P Mernagh |
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| Institution: | 1. Geoscience, Australian Museum, 1 William Street, Sydney, NSW, 2010, Australia;2. School of Biological Earth and Environmental Sciences, University of New South Wales, NSW, 2052, Australia;3. School of Biological Earth and Environmental Sciences, University of New South Wales, NSW, 2052, Australia;4. College of Physical and Mathematical Sciences, The Australian National University, Acton, ACT, 2601, Australia |
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| Abstract: | A paleo-alluvial 0.21 ct yellow diamond (L058) from Bingara (NSW) has three inclusions of coesite (two subequant crystals and one thin plate), each under more than 3.1 GPa internal pressure as measured by Raman spectroscopy. These inclusions cause overlapping birefringent retardation stress/strain haloes in the host diamond, visible under cross-polarised light. The complicated retardation pattern is quantified by mapping targeted retardation contours (170 nm, 270 nm and 380 nm) onto a photo of the diamond. A mathematical model of retardation is developed for each inclusion, and then the combined light retardations (CLR) are calculated using radial and tangential components with spherical and elliptical geometries. The CLR model reproduces most features of the measured data, but remaining differences may be due to local release of stress/strain by two short fractures radiating from one inclusion. |
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| Keywords: | Bingara NSW Phanerozoic UHP macrodiamond Raman spectroscopy coesite inclusion internal pressure strain birefringence model |
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