2021
DOI: 10.1016/j.oregeorev.2021.104192
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Rift structures and magmatism focus VMS and gold mineralisation in the Paleoproterozoic Bryah Rift Basin, Australia

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Cited by 2 publications
(3 citation statements)
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“…In the Noranda District, VMS and orogenic deposits are within 21.1 km and 22.8 km of a 100 Ω·m contour in the interval from ~ 1–40 km depth, respectively (Supplementary Table S3 . The spatial association between VMS and orogenic Au deposits and low-resistivity features is consistent with both mineral systems sharing the same crustal infrastructure that resulted in endowment of the ~ 30 Ma older VMS deposits, e.g., as suggested for VMS and orogenic gold mineralization in the Bryah Rift Basin, Australia 10 . The location of the two Au-rich VMS deposits within a 100 Ω·m contour, highlights their proximity to where the low-resistivity pipe-like features come to surface (Supplementary Fig.…”
Section: Metal Endowmentsupporting
confidence: 70%
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“…In the Noranda District, VMS and orogenic deposits are within 21.1 km and 22.8 km of a 100 Ω·m contour in the interval from ~ 1–40 km depth, respectively (Supplementary Table S3 . The spatial association between VMS and orogenic Au deposits and low-resistivity features is consistent with both mineral systems sharing the same crustal infrastructure that resulted in endowment of the ~ 30 Ma older VMS deposits, e.g., as suggested for VMS and orogenic gold mineralization in the Bryah Rift Basin, Australia 10 . The location of the two Au-rich VMS deposits within a 100 Ω·m contour, highlights their proximity to where the low-resistivity pipe-like features come to surface (Supplementary Fig.…”
Section: Metal Endowmentsupporting
confidence: 70%
“…A quantitative examination of the spatial relationship between mineral deposits and lithospheric conductivity on a global scale, showed a strong correlation between orogenic gold deposits and mid-crustal conductors, whereas VMS deposits showed a weak association with upper mantle conductors 9 . However, orogenic gold deposits have been shown to be spatially associated with the borders of magmatic centres and rift faults also spatially connected to VMS mineralization despite occurring hundreds of millions of years later 10 . Such associations point to a primary crustal architecture responsible for focusing both VMS and later gold mineralization 10 .…”
Section: Introductionmentioning
confidence: 99%
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