An increase in the number of research institutions around the globe utilizing uranium-helium thermochronometry for applications including mineral and petroleum exploration, geohazards assessment, and continental evolution studies, has prompted demand for a world-first technology developed by CSIRO Exploration & Mining and manufactured by ASI.
Uranium-helium thermochronometry is a highly sensitive and cost-effective method of radiometric age dating that can be used to determine the thermal history of the Earth’s crust. The major benefit of this technology to the mineral resources industry lies in the ability to quantitatively determine the low temperature thermal histories of mineral belts (see references below) and petroleum basins. This data is fundamental in the exploration for deposits of minerals, as well as oil and gas.
See the Downloads section of the website for application notes on the Alphachron, and data on the innovative new RESOchron.
Recent publications demonstrating the application of this technology in ore deposit research include:
McInnes, B.I.A., Evans, N..J., Fu, F.Q. and Garwin, S., 2005. Application of thermochronometry to hydrothermal ore deposits, in Reiners, P. and Ehlers, T. (Eds.), Thermochronology, Reviews in Mineralogy & Geochemistry, Vol. 58, p. 467-498 (ISSN 1529-6466).
McInnes, B.I.A., Evans, N.J., Fu, F.Q., Garwin, S., Belousova, E., Griffin, W.L., Bertens, A., Sukarna, D., Permanadewi, S., Andrew, R.L. and Deckart, K., 2005. Thermal history analysis of selected Chilean, Indonesian and Iranian porphyry Cu-Mo-Au deposits; in Porter, T.M. (Ed.), Super Porphyry Copper & Gold Deposits: A Global Perspective, Vol. 1; PGC Publishing, Adelaide, pp. 27-42.
McInnes, B.I.A., Farley, K.A., Sillitoe, R.H and Kohn, B. 1999. Application of (U-Th)/He dating to the estimation of the sense and amount of vertical fault displacement at the Chuquicamata Mine, Chile, Economic Geology 94, 937-948.