http://orcid.org/0000-0001-7084-045X
References
- Barron, L. M., Mernagh, T. P., Barron, B. J., & Pogson, R. (2011). Spectroscopic research on ultrahigh pressure (UHP) macrodiamond at Copeton and Bingara NSW, eastern Australia. Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy, 80(1), 112–118. doi:10.1016/j.saa.2011.03.003
- Davies, R. M. (1998). The characteristics and origins of alluvial diamonds from Eastern Australia (PhD thesis). Macquarie University, Sydney, NSW, 229 p., and 9 appendices.
- Davies, R. M., O’Reilly, S. Y., & Griffin, W. L. (1999). Diamonds from Wellington, NSW: insights into the origin of eastern Australian diamonds. Mineralogical Magazine, 63(4), 447–471. doi:10.1180/002646199548619
- Davies, R. M., O’Reilly, S. Y., & Griffin, W. L. (2002). Multiple origins of alluvial diamonds from New South Wales, Australia. Economic Geology, 97(1), 109–123. doi:10.2113/gsecongeo.97.1.109
- MacNevin, A. A. (1977). Diamonds in New South Wales (Vol. 42, 125 p. with 29 plate pages). Sydney, NSW: Geological Survey of New South Wales Mineral Resources.
- Meyer, H. O. A., Milledge, H. J., Sutherland, F. L., & Kennewell, P. (1997). Unusual diamonds and unique inclusions from New South Wales. Australia. Russian Geology and Geophysics, 38, 305–331.
- Mitchell, R. H. (1997). Memorial of H. O. A. Meyer 1937–1995. American Mineralogist, 82, 438–439.
- Taylor, W. R., Jaques, A. L., & Ridd, M. (1990). Nitrogen-defect aggregation characteristics of some Australasian diamonds: Time–temperature constraints on the source regions of pipe and alluvial diamonds. American Mineralogist, 75, 1290–1310.