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X-ray Mapping Investigations of the Monazites from the Mt Weld Deposit - Compositional Variance as an Indicator of Provenance

Published online by Cambridge University Press:  27 August 2014

T Murphy
Affiliation:
School of Science and Health, University of Western Sydney, NSW 2751, Australia
P. Fisher
Affiliation:
School of Science and Health, University of Western Sydney, NSW 2751, Australia
A. J. Roper
Affiliation:
School of Science and Health, University of Western Sydney, NSW 2751, Australia
J.K. Reynolds
Affiliation:
School of Science and Health, University of Western Sydney, NSW 2751, Australia
R. Wuhrer
Affiliation:
Advanced Materials Characterisation Facility, University of Western Sydney, Australia

Abstract

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Type
Abstract
Copyright
Copyright © Microscopy Society of America 2014 

References

[1] Bunting, J A., van de Graaff, W. J. E. and Jackson, M J. Palaeodrainages and Cainozoic palaeogeography of the eastern Goldfields, Gibson Desert and Great Victoria Desert. Geological Survey of Western Australia Annual Progress Rep (1973) pp. 45–50.Google Scholar
[2] Michard, A. Lanthanide series Systematics in Hydrothermal Fluids. Geochemical Society and the Meteoritic Society. 53. Published by Elsivier (1989) pp 745–750.Google Scholar
[3] Willett, G. C., Duncan, R. K., and Rankin, R. A. “Geology and economic evaluation of the Mt. Weld carbonatite, Laverton, Western Australia.” Geol Soc Australia Abstract. Vol. 16 (1986) pp. 97–99.Google Scholar
[4] Wuhrer, R., Moran, K., Moran, L. “Characterisation of materials through X-ray mapping.”Materials Forum (2006) vol. 30.Google Scholar