Abstract
The Proterozoic metamorphic rocks of the Selwyn Range area in western Queensland contain a variety of styles of Au + Cu deposit including some (e.g. Selwyn mine and Osborne prospect) that are spatially associated with magnetite-rich ironstones. The area is characterized by extensive alkali-(chloride) metasomatism that occurred during the later stages of regional metamorphism. Existing experimental data indicate that hot saline fluids will dissolve and transport iron as they move through temperature/pressure gradients in the vicinity of the amphibolite-greenschist facies transition and predict that circulation cells will move iron and concentrate it in relatively cool, dilute and/or oxidized parts of such systems. New geological mapping coupled with geochemical data from the amphibolite facies zone of the Selwyn Range area suggest such processes occurred on a large scale and that large masses of Fe were mobilized, particularly in association with Na-metasomatism of biotite-bearing metasediments and high Fe-tholeiitic dolerites. Field and textural features of ironstones and other Fe-rich lithologies demonstrate that some of them at least formed by replacement of other rocks during metamorphism and deformation. Mineralization localized within such iron stones must itself be epigenetic.
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Williams, P.J. Iron mobility during synmetamorphic alteration in the Selwyn Range area, NW Queensland: implications for the origin of ironstone-hosted Au-Cu deposits. Mineral. Deposita 29, 250–260 (1994). https://doi.org/10.1007/BF00206868
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DOI: https://doi.org/10.1007/BF00206868