Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/124576
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Type: Journal article
Title: ~1760 Ma magnetite-bearing protoliths in the Olympic Dam deposit, South Australia: implications for ore genesis and regional metallogeny
Author: Courtney-Davies, L.
Ciobanu, C.
Verdugo Ihl, M.
Cook, N.
Ehrig, K.
Wade, B.
Zhu, Z.
Kamenetsky, V.
Citation: Ore Geology Reviews, 2020; 118:1-13
Publisher: Elsevier
Issue Date: 2020
ISSN: 0169-1368
1872-7360
Statement of
Responsibility: 
Liam Courtney-Davies, Cristiana L. Ciobanu, Max R. Verdugo-Ihl, Nigel J. Cook, Kathy J. Ehrig, Benjamin P. Wade ... et al.
Abstract: Spatial associations between banded iron formation and iron-oxide Cu-Au (IOCG) style mineralization are well documented in the Gawler Craton (South Australia), but the possible genetic relationships between these two distinct types of mineralization are hitherto unclear. A texturally conspicuous generation of coarse-grained silician magnetite, intergrown with carbonates and quartz, is observed in drillholes intersecting the ‘outer shell’ of the Olympic Dam IOCG-type deposit. This magnetite is characterised by high U-content (~50 ppm), siliceous chemistry, and unusual zonal textures with respect to Si-Fe-nanoprecipitates. Direct dating of this magnetite by laser ablation inductively coupled plasma mass spectrometry yields reproducible 207Pb/206Pb dates (1761 ± 16 Ma) that are significantly older than the granite hosting the deposit (1593 Ma), or the mineralized breccias constituting the Cu-U-Au-Ag resource (~1592–1589 Ma). The older, Fe-rich crustal material can be correlated with the ~1.76–1.74 Ga (meta)sedimentary Wallaroo Group, host to Fe-rich horizons across the Gawler Craton, including locations ~15 km NW of Olympic Dam. A generation of granitic rocks, which intruded bedrock at ~1.75 Ga are present ~30 km NE of Olympic Dam, and likely exsolved hydrothermal fluids that enriched pre-existing magnetite-bearing protoliths in both U and REE. Such material was physically, and likely chemically, incorporated into the ‘outer shell’ at Olympic Dam some ~150 Ma later, during granite uplift along faults. The coincidence between Fe-rich horizons/BIF and ~1750 Ma granitoids may have provided IOCG systems with an additional source of both Fe and U that predates the ~1.59 Ga craton-scale metallogenic event. The uranium concentrations in some South Australian IOCG systems represent major global anomalies in the element. A combination of the fortuitous geological circumstances outlined here, may help explain the highly anomalous accumulation of uranium found at Olympic Dam.
Keywords: Olympic Dam; Magnetite U-Pb dating; IOCG; Gawler Craton
Rights: © 2020 Elsevier B.V. All rights reserved.
RMID: 1000014068
DOI: 10.1016/j.oregeorev.2020.103337
Grant ID: http://purl.org/au-research/grants/arc/IH130200033
Appears in Collections:Chemical Engineering publications

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