2023
DOI: 10.1016/j.precamres.2023.107225
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Pb-bearing Cu-(Fe)-sulfides: Evidence for continuous hydrothermal activity in the northern Olympic Cu-Au Province, South Australia

Nicholas D. Owen,
Nigel J. Cook,
Rahul Ram
et al.
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Cited by 1 publication
(2 citation statements)
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“…At Olympic Dam, an average present day heat flow of 125 mW/m 2 and steep temperature gradient of 83.1 (±5.5) • C/km was recorded [86], which is ~63% higher than the surrounding South Australian Heat Flow Anomaly. If this is considered alongside a (semi-)continual supply of radiogenic heat and the semi-continuous fluid flow, as argued by Owen et al [88], this may have allowed for long-lived rejuvenation of economic metals across the mineral system [85]. Evidence presented for secondary U enrichment at Olympic Dam [89] and the isotope systematics of carbonates [90] also indicate multiple stages of hydrothermal activity after 1 Ga.…”
Section: Were All Microstructures Obliterated By Coupled Dissolution ...mentioning
confidence: 80%
See 1 more Smart Citation
“…At Olympic Dam, an average present day heat flow of 125 mW/m 2 and steep temperature gradient of 83.1 (±5.5) • C/km was recorded [86], which is ~63% higher than the surrounding South Australian Heat Flow Anomaly. If this is considered alongside a (semi-)continual supply of radiogenic heat and the semi-continuous fluid flow, as argued by Owen et al [88], this may have allowed for long-lived rejuvenation of economic metals across the mineral system [85]. Evidence presented for secondary U enrichment at Olympic Dam [89] and the isotope systematics of carbonates [90] also indicate multiple stages of hydrothermal activity after 1 Ga.…”
Section: Were All Microstructures Obliterated By Coupled Dissolution ...mentioning
confidence: 80%
“…If accompanied by large fault displacements and associated tectonothermal events like emplacement of the Gairdner LIP [51], sudden transition between brittle to ductile regimes would be plausible and correlates with our observation of alternating ductile and brittle deformation microstructures in pyrite. The proposed waxing and waning, effectively semi-continuous fluid flow at Olympic Dam [88] would assist this, with even small changes in burial depth generating high-temperature metamorphic fluid systems [85].…”
Section: Were All Microstructures Obliterated By Coupled Dissolution ...mentioning
confidence: 99%