High Precision Zircon Dating of Tuffs
in the Sydney-Gunnedah Basin
Dr Kevin Ruming
TUFFS
NOBBYS TUFF
TUFFS
CHARBON COLLIERY BOX CUT
CA-IDTIMS
Chemical Abrasion Isotope Dilution Thermal
Ionisation Mass Spectrometry
Process
• Extract zircons
• Select primary magmatic zircons
• Zircons are individually thermally annealed and
chemically abraded
• U - Pb isotope concentrations
• Age of each zircon calculated, and a weighted mean
age for each tuff sample is determined
The Project
Progress – Overall Project
• 526 Samples collected from
Australia
• 87 Dates, 154 Samples in progress
or with preliminary dates
The Project – NSW
NSW Project
• Enhanced correlation within &
between coal basins
• High resolution estimates of
sedimentation rates
• Modelling depositional evolution of
NSW coal basins
Progress – NSW Project
• 391 Samples collected from NSW to
date
• 59 Dates
• 100 Samples in progress or with
preliminary dates
• 38 Samples had no zircons
Correlations
Ulan Seam F Ply
Regional Chronostratigraphic Correlations - Ulan Seam F Ply & Fairford
WESTERN COALFIELD
Ulan Coal F Ply
257.24 ± 0.14 257.46 ± 0.22 (Prelim)
HUNTER COALFIELD
Fairford Claystone
257.04 ± 0.15 257.43 ± 0.09
Mount Arthur Amoco Wybong 1
Correlations
Chronostratigraphic v’s Lithostratigraphic Units
SCALE
Ma GROUP AGE AGE GROUP
252.50
252.75
253.00
254.50
254.75 254.82 ± 0.04 254.88 ± 0.19 (P)
255.00
255.25 255.26 ± 0.14
255.50 255.37 ± 0.17
255.75
256.00
256.25
NEWCASTLE COALFIELD
Malabar Formation to Milbrodale
Fm
Althorpe Formation
Mount Leonard Fm
SUBGROUP/FORMATION SUBGROUP/FORMATION
Narrabeen Group
Lambton Subgroup
Nobbys Tuff
Moon Island Beach
Adamstown Subgroup
Newcastle
Coal
Measures
Waratah Sandstone / Dempsey Formation
Moon Island Beach to
Adamstown Subgroup
Tomago Coal Measures
Nobbys Tuff
Watts Sandstone / Denman Formation
Wittingham
Coal
Measures
HUNTER COALFIELD
Narrabeen Group
Newcastle
Coal
Measures
Hunter Coalfield Gunnedah Basin
Ulan Seam – Western Coalfield
Depositional Rate:
C Marker to F Ply = 6.94m/my
(On compacted sediment, does not account for post-
depositional compaction)
ULAN COAL CA-IDTIMS DATES
B Parting: 255.97 ± 0.14
C Ply: 256.19 ± 0.05, 256.37 ± 0.21
E31 Ply: 258.58 ± 0.24 (Prelim. Date)
F Ply: 257.24 ± 0.14, 257.46 ± 0.22
(Prelim)
Tuffaceous Units below F Ply: 257.17 ±
0.09, 257.84 ± 0.16, 258.77 ± 0.22
Biostratigraphy
• Palynological
samples are being
taken in conjunction
with CA-IDTIMS
samples (where
possible)
• Calibrating endemic
Australian
biozonation against
the established
global timescale
Finding the P-T Boundary – Southern
Coalfield
P-T Boundary = Historically been placed above the Bulli Coal
Finding the P-T Boundary
• P-T Boundary = Between 251.941 ±
0.037 and 251.880 ± 0.031
• Bulli Coal = 252.60 ± 0.04Ma
• Gap of ~700,000 Years
Future Work
• Redefining stratigraphic nomenclature of
major NSW basins/coalfields
• Possible redefining type holes/sections
• Updating Departmental publications
Basin Scale Fence Diagram
Acknowledgements
• Bob Nicoll, John Laurie – Geoscience Australia
• Ian Metcalfe - University of New England
• Erin Holmes - GSNSW
• Research School of Earth Sciences – ANU
• Isotope Geology Laboratory – BSU

Exploration in the House 2015: High Precision Zircon Dating of Tuffs in the Sydney-Gunnedah Basin by Dr Kevin Ruming

  • 1.
    High Precision ZirconDating of Tuffs in the Sydney-Gunnedah Basin Dr Kevin Ruming
  • 2.
  • 3.
  • 4.
  • 5.
    CA-IDTIMS Chemical Abrasion IsotopeDilution Thermal Ionisation Mass Spectrometry Process • Extract zircons • Select primary magmatic zircons • Zircons are individually thermally annealed and chemically abraded • U - Pb isotope concentrations • Age of each zircon calculated, and a weighted mean age for each tuff sample is determined
  • 6.
    The Project Progress –Overall Project • 526 Samples collected from Australia • 87 Dates, 154 Samples in progress or with preliminary dates
  • 7.
    The Project –NSW NSW Project • Enhanced correlation within & between coal basins • High resolution estimates of sedimentation rates • Modelling depositional evolution of NSW coal basins Progress – NSW Project • 391 Samples collected from NSW to date • 59 Dates • 100 Samples in progress or with preliminary dates • 38 Samples had no zircons
  • 8.
  • 9.
    Regional Chronostratigraphic Correlations- Ulan Seam F Ply & Fairford WESTERN COALFIELD Ulan Coal F Ply 257.24 ± 0.14 257.46 ± 0.22 (Prelim) HUNTER COALFIELD Fairford Claystone 257.04 ± 0.15 257.43 ± 0.09 Mount Arthur Amoco Wybong 1
  • 10.
  • 11.
    Chronostratigraphic v’s LithostratigraphicUnits SCALE Ma GROUP AGE AGE GROUP 252.50 252.75 253.00 254.50 254.75 254.82 ± 0.04 254.88 ± 0.19 (P) 255.00 255.25 255.26 ± 0.14 255.50 255.37 ± 0.17 255.75 256.00 256.25 NEWCASTLE COALFIELD Malabar Formation to Milbrodale Fm Althorpe Formation Mount Leonard Fm SUBGROUP/FORMATION SUBGROUP/FORMATION Narrabeen Group Lambton Subgroup Nobbys Tuff Moon Island Beach Adamstown Subgroup Newcastle Coal Measures Waratah Sandstone / Dempsey Formation Moon Island Beach to Adamstown Subgroup Tomago Coal Measures Nobbys Tuff Watts Sandstone / Denman Formation Wittingham Coal Measures HUNTER COALFIELD Narrabeen Group Newcastle Coal Measures
  • 12.
  • 13.
    Ulan Seam –Western Coalfield Depositional Rate: C Marker to F Ply = 6.94m/my (On compacted sediment, does not account for post- depositional compaction) ULAN COAL CA-IDTIMS DATES B Parting: 255.97 ± 0.14 C Ply: 256.19 ± 0.05, 256.37 ± 0.21 E31 Ply: 258.58 ± 0.24 (Prelim. Date) F Ply: 257.24 ± 0.14, 257.46 ± 0.22 (Prelim) Tuffaceous Units below F Ply: 257.17 ± 0.09, 257.84 ± 0.16, 258.77 ± 0.22
  • 14.
    Biostratigraphy • Palynological samples arebeing taken in conjunction with CA-IDTIMS samples (where possible) • Calibrating endemic Australian biozonation against the established global timescale
  • 15.
    Finding the P-TBoundary – Southern Coalfield P-T Boundary = Historically been placed above the Bulli Coal
  • 16.
    Finding the P-TBoundary • P-T Boundary = Between 251.941 ± 0.037 and 251.880 ± 0.031 • Bulli Coal = 252.60 ± 0.04Ma • Gap of ~700,000 Years
  • 17.
    Future Work • Redefiningstratigraphic nomenclature of major NSW basins/coalfields • Possible redefining type holes/sections • Updating Departmental publications
  • 18.
  • 19.
    Acknowledgements • Bob Nicoll,John Laurie – Geoscience Australia • Ian Metcalfe - University of New England • Erin Holmes - GSNSW • Research School of Earth Sciences – ANU • Isotope Geology Laboratory – BSU