Mineralization proximal to the final Nuna suture in northeastern Australia

Mineralization along continental suture zones is facilitated through the frequent presence of pathways from fertile mantle source regions to crustal repositories. Due to their inherent rheological weakness, these suture zones are often concealed, which hinders surface-based observations. Here, we us...

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Main Authors: Olierook, Hugo, Affleck, R.G., Evans, Noreen, Jourdan, Fred, Kirkland, Chris, Volante, S., Nordsvan, A.R., McInnes, Brent, McDonald, B., Mayers, C., Frew, R.A., Rankenburg, Kai, d'Offay, N., Nind, M., Larking, A.
Format: Journal Article
Language:English
Published: ELSEVIER 2021
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/91506
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author Olierook, Hugo
Affleck, R.G.
Evans, Noreen
Jourdan, Fred
Kirkland, Chris
Volante, S.
Nordsvan, A.R.
McInnes, Brent
McDonald, B.
Mayers, C.
Frew, R.A.
Rankenburg, Kai
d'Offay, N.
Nind, M.
Larking, A.
author_facet Olierook, Hugo
Affleck, R.G.
Evans, Noreen
Jourdan, Fred
Kirkland, Chris
Volante, S.
Nordsvan, A.R.
McInnes, Brent
McDonald, B.
Mayers, C.
Frew, R.A.
Rankenburg, Kai
d'Offay, N.
Nind, M.
Larking, A.
author_sort Olierook, Hugo
building Curtin Institutional Repository
collection Online Access
description Mineralization along continental suture zones is facilitated through the frequent presence of pathways from fertile mantle source regions to crustal repositories. Due to their inherent rheological weakness, these suture zones are often concealed, which hinders surface-based observations. Here, we use zircon U-Pb and sericite 40Ar/39Ar dating, and whole-rock geochemical data, to investigate the crystallization and mineralization history from a sequence of granites (sensu lato), volcanic rocks and sedimentary rocks from the Au–Ag–Pb–Zn Empress Springs Project in northeast Australia, which are under >50 m of Phanerozoic cover and located near the interpreted ca. 1.6 Ga tectonic boundary between the North Australia Craton (Mount Isa Inlier) and Laurentia (Georgetown Inlier). Zircon U-Pb dating indicates that granite emplacement, volcanic eruptions and dolerite intrusions occurred between 1564 ± 6 and 1546 ± 13 Ma (2σ), corresponding to the 1560–1550 Ma Esmeralda Supersuite and the Croydon Volcanic Group exposed in the western Georgetown Inlier. U-Pb ages from detrital zircon grains in a sedimentary rock revealed a near unimodal ca. 1560 Ma population, likely sourced from the surrounding granitic and volcanic rocks. Sericite 40Ar/39Ar dating yielded disturbed spectra with evidence for incorporation of excess radiogenic Ar, but with a probable Carboniferous to Permian age, potentially dating the timing of gold mineralization. Geochemical similarities point towards an epithermal origin for the Empress Springs Project, consistent with post-orogenic mineralization at either ca. 1560–1550 Ma or 330–250 Ma. It is likely that a series of west-dipping lithospheric-scale faults below the Empress Springs Project, here termed the Empress Suture Zone, demarcate the final suture zone associated with the assembly of Nuna. Reactivation of the Empress Suture Zone ~1.3 b.y. after crystallization with potential contemporaneous gold mineralization attests to its longevity for fluid mobility.
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institution Curtin University Malaysia
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spelling curtin-20.500.11937-915062023-05-04T09:04:04Z Mineralization proximal to the final Nuna suture in northeastern Australia Olierook, Hugo Affleck, R.G. Evans, Noreen Jourdan, Fred Kirkland, Chris Volante, S. Nordsvan, A.R. McInnes, Brent McDonald, B. Mayers, C. Frew, R.A. Rankenburg, Kai d'Offay, N. Nind, M. Larking, A. Science & Technology Physical Sciences Geosciences, Multidisciplinary Geology Empress Springs Columbia Laurentia North Australian Craton zircon U-Pb epithermal Mineralization along continental suture zones is facilitated through the frequent presence of pathways from fertile mantle source regions to crustal repositories. Due to their inherent rheological weakness, these suture zones are often concealed, which hinders surface-based observations. Here, we use zircon U-Pb and sericite 40Ar/39Ar dating, and whole-rock geochemical data, to investigate the crystallization and mineralization history from a sequence of granites (sensu lato), volcanic rocks and sedimentary rocks from the Au–Ag–Pb–Zn Empress Springs Project in northeast Australia, which are under >50 m of Phanerozoic cover and located near the interpreted ca. 1.6 Ga tectonic boundary between the North Australia Craton (Mount Isa Inlier) and Laurentia (Georgetown Inlier). Zircon U-Pb dating indicates that granite emplacement, volcanic eruptions and dolerite intrusions occurred between 1564 ± 6 and 1546 ± 13 Ma (2σ), corresponding to the 1560–1550 Ma Esmeralda Supersuite and the Croydon Volcanic Group exposed in the western Georgetown Inlier. U-Pb ages from detrital zircon grains in a sedimentary rock revealed a near unimodal ca. 1560 Ma population, likely sourced from the surrounding granitic and volcanic rocks. Sericite 40Ar/39Ar dating yielded disturbed spectra with evidence for incorporation of excess radiogenic Ar, but with a probable Carboniferous to Permian age, potentially dating the timing of gold mineralization. Geochemical similarities point towards an epithermal origin for the Empress Springs Project, consistent with post-orogenic mineralization at either ca. 1560–1550 Ma or 330–250 Ma. It is likely that a series of west-dipping lithospheric-scale faults below the Empress Springs Project, here termed the Empress Suture Zone, demarcate the final suture zone associated with the assembly of Nuna. Reactivation of the Empress Suture Zone ~1.3 b.y. after crystallization with potential contemporaneous gold mineralization attests to its longevity for fluid mobility. 2021 Journal Article http://hdl.handle.net/20.500.11937/91506 10.1016/j.gr.2020.12.017 English ELSEVIER fulltext
spellingShingle Science & Technology
Physical Sciences
Geosciences, Multidisciplinary
Geology
Empress Springs
Columbia
Laurentia
North Australian Craton
zircon U-Pb
epithermal
Olierook, Hugo
Affleck, R.G.
Evans, Noreen
Jourdan, Fred
Kirkland, Chris
Volante, S.
Nordsvan, A.R.
McInnes, Brent
McDonald, B.
Mayers, C.
Frew, R.A.
Rankenburg, Kai
d'Offay, N.
Nind, M.
Larking, A.
Mineralization proximal to the final Nuna suture in northeastern Australia
title Mineralization proximal to the final Nuna suture in northeastern Australia
title_full Mineralization proximal to the final Nuna suture in northeastern Australia
title_fullStr Mineralization proximal to the final Nuna suture in northeastern Australia
title_full_unstemmed Mineralization proximal to the final Nuna suture in northeastern Australia
title_short Mineralization proximal to the final Nuna suture in northeastern Australia
title_sort mineralization proximal to the final nuna suture in northeastern australia
topic Science & Technology
Physical Sciences
Geosciences, Multidisciplinary
Geology
Empress Springs
Columbia
Laurentia
North Australian Craton
zircon U-Pb
epithermal
url http://hdl.handle.net/20.500.11937/91506