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Journal ArticleDOI

A new 40Ar/39Ar eruption age for the Mount Widderin volcano, Newer Volcanic Province, Australia, with implications for eruption frequency in the region

04 May 2016-Australian Journal of Earth Sciences (Taylor & Francis)-Vol. 63, Iss: 2, pp 175-186
TL;DR: In this article, a new, high-precision 40Ar/39Ar age of 389 ± 8 ka (2σ) was reported for a Mount Widderin basalt sample.
Abstract: The Mount Widderin shield volcano is located near Skipton, western Victoria, in the Western Plains subprovince of the monogenetic Pliocene–Holocene Newer Volcanic Province (NVP). Radiometric ages for lavas in the Hamilton–Skipton–Derrinallum area are few, owing to limited suitable outcrop for K–Ar or 40Ar/39Ar geochronology studies. Existing age constraints for flows in this area have been inferred from Regolith Landform Units (RLUs), complemented by a small number of K–Ar studies on ≥1 Ma flows. Although the RLU approach provides a valuable overview of relative eruption ages across the NVP, it is of limited use in eruption frequency studies. Additional radio-isotopic ages are required to refine age ranges for individual RLUs, and to validate previous assignment of individual flows to specific RLUs. We report a new, high-precision 40Ar/39Ar age of 389 ± 8 ka (2σ) for a Mount Widderin basalt sample. Based on this age and geomorphic observations, we propose that both the Widderin and Elephant lava f...

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Summary

  • Ar laser step-heating analytical results for NVP26 groundmass.
  • Table A2. 40Ar/39Ar ARGUSVI data and blank values for laser step-heating analysis of sample NVP26 excluding interference corrections.
  • Ar age spectra and inverse isochron diagrams for individual NVP26 groundmass aliquants.
  • Grey symbols are excluded from age calculation results.
  • In inverse isochron diagrams, solid lines represent preferred isochron results and dashed lines indicate position of inverse isochrons constructed from all data points.

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A new
40
Ar/
39
Ar eruption age for the Mount Widderin volcano,
Newer Volcanic Province, Australia, with implications for eruption
frequency in the region.
E. L. MATCHAN, E. B. JOYCE, AND D. PHILLIPS
School of Earth Sciences, The University of Melbourne, VIC 3010, Australia.
*Corresponding author: ematchan@unimelb.edu.au
SUPPLEMENTARY PAPERS
Australian Journal of Earth Sciences (2016) 63,
http://dx.doi.org/10.1080/08120099.2016.1156576
----------------------------------------------------------------------------------------------------------------
Copies of Supplementary Papers may be obtained from the Geological Society of
Australia's website (www.gsa.org.au), the Australian Journal of Earth Sciences
website (www.ajes.com.au) or from the National Library of Australia's Pandora
archive (http://nla.gov.au/nla.arc-25194).
----------------------------------------------------------------------------------------------------------------
SUPPLEMENTARY PAPERS
Table A1. ARGUSVI
40
Ar/
39
Ar laser step-heating analytical results for NVP26
groundmass.
Table A2.
40
Ar/
39
Ar ARGUSVI data and blank values for laser step-heating analysis
of sample NVP26 excluding interference corrections.
Figure A1.
40
Ar/
39
Ar age spectra and inverse isochron diagrams for individual NVP26
groundmass aliquants. Errors symbols are 1σ. Grey symbols are excluded from
age calculation results. In inverse isochron diagrams, solid lines represent
preferred isochron results and dashed lines indicate position of inverse
isochrons constructed from all data points. Step numbers are indicated.
Appendix B Supplementary information related to the contact between lava flows
from Mount Widderin and Mount Elephant.
Matchan et al. 2016 Australian Journal of Earth Sciences 63/2 Supplementary Papers http://dx.doi.org/10.1080/08120099.2016.1156576
1

Table A1. ARGUSVI
40
Ar/
39
Ar laser step-heating analytical results for NVP26 groundmass.
a,b,c,d
Sample
Step Laser
40
Ar ±1σ
39
Ar ±1σ
38
Ar ±1σ
37
Ar ±1σ
36
Ar ±1σ
39
Ar Cum.% Apparent
ID
No Power (x10
-14 39
Ar Age (ka)
mol)
d
NVP26-1 101.3 mg
NVP26-1a 1 4% 345.50 0.08 63.788 0.045 0.1344 0.0006 99.1 2.9 0.7128 0.0031 0.2264 2.719 0.081 38.41 2.080 0.015 17.98 401.604 2.8 0.7
NVP26-1b 2 6% 501.14 0.22 105.177 0.043 0.1812 0.0008 132.7 3.0 0.9615 0.0043 0.3734 2.208 0.050 42.72 2.035 0.012 47.63 392.884 2.4 0.6
NVP26-1c 3 9% 530.49 0.13 104.603 0.076 0.2008 0.0006 138.7 4.1 1.0655 0.0029 0.3713 2.320 0.068 40.03 2.030 0.009 77.12 391.926 1.7 0.4
NVP26-1d 4 12% 316.81 0.07 52.986 0.037 0.1329 0.0004 88.9 3.1 0.7050 0.0022 0.1881 2.937 0.104 33.56 2.007 0.013 92.06 387.339 2.4 0.6
NVP26-1e 5 18% 279.59 0.07 28.168 0.046 0.1422 0.0003 110.9 1.8 0.7542 0.0016 0.1000 6.888 0.110 19.46 1.932 0.017 100.00 372.937 3.4 0.9
Total gas age: 391.8 ± 4.7 (2σ)
NVP26-2 71.5 mg
NVP26-2a 1 4% 645.08 0.34 106.061 0.078 0.2676 0.0006 173.3 2.5 1.4197 0.0031 0.3765 2.859 0.041 34.29 2.086 0.009 18.78 402.608 1.8 0.5
NVP26-2b 2 6% 702.98 0.29 144.297 0.108 0.2572 0.0004 191.8 2.0 1.3645 0.0023 0.5123 2.327 0.025 42.05 2.049 0.005 44.33 395.444 1.0 0.3
NVP26-2c 3 8% 563.02 0.16 117.904 0.060 0.2037 0.0006 142.5 2.3 1.0804 0.0031 0.4186 2.115 0.034 42.71 2.039 0.008 65.20 393.696 1.6 0.4
NVP26-2d 4 10% 450.09 0.10 86.882 0.030 0.1731 0.0006 113.1 4.0 0.9182 0.0032 0.3084 2.278 0.081 39.09 2.025 0.011 80.59 390.944 2.2 0.6
NVP26-2e 5 14% 447.18 0.12 65.464 0.035 0.1992 0.0004 133.7 2.3 1.0570 0.0021 0.2324 3.575 0.061 29.43 2.010 0.010 92.18 388.052 1.9 0.5
NVP26-2f 6 20% 341.33 0.09 30.637 0.042 0.1757 0.0005 139.1 2.6 0.9319 0.0027 0.1088 7.948 0.146 18.49 2.060 0.026 97.60 397.680 5.1 1.3
NVP26-2g 7 30% 199.01 0.06 13.555 0.032 0.1060 0.0004 99.1 2.3 0.5625 0.0019 0.0481 12.794 0.302 15.61 2.292 0.043 100.00 442.346 8.3 1.9
Total gas age: 396.1 ± 4.0 (2σ)
NVP26-3 76.0 mg
NVP26-3a 1 4% 399.93 0.13 68.267 0.040 0.1644 0.0004 101.9 2.4 0.8724 0.0021 0.2423 2.613 0.063 34.87 2.043 0.009 16.45 394.387 1.8 0.5
NVP26-3b 2 6% 516.57 0.33 103.661 0.042 0.1942 0.0005 136.2 2.1 1.0303 0.0025 0.3680 2.299 0.036 40.45 2.016 0.008 41.42 389.151 1.5 0.4
NVP26-3c 3 8% 430.47 0.18 89.732 0.060 0.1588 0.0005 109.2 2.2 0.8426 0.0027 0.3185 2.130 0.044 41.56 1.994 0.009 63.04 384.867 1.8 0.5
NVP26-3d 4 10% 325.98 0.08 64.475 0.052 0.1243 0.0004 85.5 2.0 0.6592 0.0019 0.2289 2.322 0.054 39.62 2.003 0.009 78.57 386.710 1.7 0.4
NVP26-3e 5 14% 340.29 0.08 52.219 0.043 0.1488 0.0005 100.8 3.2 0.7895 0.0028 0.1854 3.377 0.108 30.73 2.002 0.016 91.15 386.548 3.1 0.8
NVP26-3f 6 30% 445.42 0.07 36.739 0.068 0.2361 0.0005 185.6 2.7 1.2523 0.0028 0.1304 8.842 0.128 16.06 1.947 0.023 100.00 375.808 4.5 1.2
Total gas age: 387.2 ± 4.3 (2σ)
NVP26-4
101.1 mg
NVP26-4a 1 4% 632.41 0.24 108.707 0.046 0.2586 0.0008 172.1 2.5 1.3720 0.0043 0.3859 2.771 0.040 35.23 2.050 0.012 19.72 395.637 2.3 0.6
NVP26-4b 2 6% 723.03 0.30 152.589 0.092 0.2607 0.0005 197.1 1.6 1.3828 0.0028 0.5417 2.260 0.019 42.90 2.033 0.006 47.40 392.419 1.1 0.3
NVP26-4c 3 8% 571.53 0.17 122.726 0.065 0.2054 0.0006 143.8 2.1 1.0895 0.0031 0.4357 2.051 0.030 43.09 2.007 0.008 69.67 387.349 1.5 0.4
NVP26-4d 4 10% 398.11 0.12 76.565 0.041 0.1559 0.0005 92.6 3.0 0.8271 0.0025 0.2718 2.116 0.070 37.97 1.974 0.010 83.56 381.126 1.9 0.5
NVP26-4e 5 14% 427.80 0.09 58.687 0.036 0.1977 0.0004 129.7 2.8 1.0487 0.0021 0.2083 3.868 0.084 26.82 1.955 0.011 94.21 377.346 2.1 0.6
NVP26-4f 6 30% 486.47 0.19 31.927 0.036 0.2690 0.0008 215.2 2.3 1.4270 0.0041 0.1133 11.798 0.128 12.42 1.892 0.039 100.00 365.248 7.5 2.0
Total gas age: 387.2 ± 4.1 (2σ)
NVP26-5
101.0 mg
NVP26-5a 1 4% 740.37 0.26 128.485 0.073 0.3001 0.0007 208.2 3.1 1.5920 0.0037 0.4561 2.836 0.042 35.80 2.063 0.009 22.89 398.219 1.7 0.4
NVP26-5b 2 6% 783.34 0.27 168.031 0.077 0.2798 0.0007 206.6 1.3 1.4843 0.0035 0.5965 2.152 0.013 43.43 2.025 0.007 52.83 390.826 1.3 0.3
NVP26-5c 3 8% 575.39 0.10 121.589 0.051 0.2090 0.0005 141.9 2.6 1.1088 0.0025 0.4316 2.043 0.037 42.47 2.010 0.006 74.50 387.942 1.2 0.3
NVP26-5d 4 10% 391.34 0.08 71.175 0.049 0.1575 0.0006 102.9 4.8 0.8358 0.0029 0.2527 2.529 0.118 36.24 1.992 0.012 87.18 384.597 2.4 0.6
NVP26-5e 5 14% 408.08 0.10 47.829 0.035 0.1968 0.0006 135.1 2.7 1.0439 0.0031 0.1698 4.944 0.098 23.63 2.016 0.019 95.70 389.134 3.7 1.0
NVP26-5f 6 30% 414.33 0.13 24.106 0.043 0.2322 0.0004 187.5 3.7 1.2321 0.0024 0.0856 13.612 0.270 11.22 1.928 0.030 100.00 372.221 5.8 1.6
Total gas age: 390.2 ± 3.8 (2σ)
b
Interference corrections: (
36
Ar/
37
Ar)
Ca
= (2.5713 ± 0.0023) x 10
-4
; (
39
Ar/
37
Ar)
Ca
= (6.6200 ± 0.0801) x 10
-4
; (
40
Ar/
39
Ar)
K
= (1.00 ± 0.05) x 10
-10
; (
38
Ar/
39
Ar)
K
= (1.2136 ± 0.0016) x 10
-2
c
J-value is 0.0001070135 ± 0.0000000648 ( 0.061%;1σ), based on an age of 1.1811 ± 0.0006 Ma (1σ) for AC sanidine (Phillips et al., submitted)
d
Sensitivity = 3.55 x 10
-17
mol/fA
(fA)
(fA)
b
(fA)
(fA)
b
a
Data are corrected for mass spectrometer backgrounds, discrimination, radioactive decay and interference corrections (see Table A.2 for values excluding the interference correction). Errors are
one sigma uncertainties and exclude uncertainty in the J-value.
(fA)
Matchan et al. 2016 Australian Journal of Earth Sciences 63/2 Supplementary Papers http://dx.doi.org/10.1080/08120099.2016.1156576
2

Table A1. ARGUSVI
40
Ar/
39
Ar laser step-heating analytical results for NVP26 groundmass.
a,b,c,d
Sample
Step
ID
No
NVP26-1
101.3 mg
NVP26-1a 1
NVP26-1b 2
NVP26-1c 3
NVP26-1d 4
NVP26-1e 5
NVP26-2
NVP26-2a 1
NVP26-2b 2
NVP26-2c 3
NVP26-2d 4
NVP26-2e 5
NVP26-2f 6
NVP26-2g 7
NVP26-3
NVP26-3a 1
NVP26-3b 2
NVP26-3c 3
NVP26-3d 4
NVP26-3e 5
NVP26-3f 6
NVP26-4
NVP26-4a 1
NVP26-4b 2
NVP26-4c 3
NVP26-4d 4
NVP26-4e 5
NVP26-4f 6
NVP26-5
NVP26-5a 1
NVP26-5b 2
NVP26-5c 3
NVP26-5d 4
NVP26-5e 5
NVP26-5f 6
Background correction
Blank no.
40
Ar ±1σ
39
Ar ±1σ
38
Ar ±1σ
37
Ar ±1σ
36
Ar ±1σ
EXB#74 7.276 0.011 0.085 0.019 -0.121 0.043 0.020 0.027 0.03095 0.00053
EXB#75 7.787 0.024 0.056 0.017 -0.055 0.030 -0.002 0.032 0.03330 0.00021
EXB#75 7.787 0.024 0.056 0.017 -0.055 0.030 -0.002 0.032 0.03330 0.00021
EXB#76 7.792 0.013 0.086 0.022 -0.062 0.020 0.025 0.011 0.03381 0.00035
EXB#76 7.792 0.013 0.086 0.022 -0.062 0.020 0.025 0.011 0.03381 0.00035
EXB#82 3.336 0.016 0.060 0.018 -0.008 0.021 -0.014 0.015 0.01726 0.00011
EXB#82 3.336 0.016 0.060 0.018 -0.008 0.021 -0.014 0.015 0.01726 0.00011
EXB#83 3.393 0.019 0.092 0.017 -0.003 0.020 -0.009 0.015 0.01881 0.00014
EXB#83 3.393 0.019 0.092 0.017 -0.003 0.020 -0.009 0.015 0.01881 0.00014
EXB#83 3.393 0.019 0.092 0.017 -0.003 0.020 -0.009 0.015 0.01881 0.00014
EXB#84 3.429 0.010 0.102 0.022 -0.044 0.022 0.020 0.014 0.01812 0.00036
EXB#84 3.429 0.010 0.102 0.022 -0.044 0.022 0.020 0.014 0.01812 0.00036
EXB#89 2.515 0.025 0.081 0.008 -0.083 0.017 0.035 0.014 0.01532 0.00035
EXB#89 2.515 0.025 0.081 0.008 -0.083 0.017 0.035 0.014 0.01532 0.00035
EXB#89 2.515 0.025 0.081 0.008 -0.083 0.017 0.035 0.014 0.01532 0.00035
EXB#90 2.707 0.029 0.092 0.023 -0.093 0.012 0.012 0.012 0.01736 0.00047
EXB#90 2.707 0.029 0.092 0.023 -0.093 0.012 0.012 0.012 0.01736 0.00047
EXB#90 2.707 0.029 0.092 0.023 -0.093 0.012 0.012 0.012 0.01736 0.00047
EXB#91 3.219 0.017 0.088 0.022 -0.079 0.036 -0.012 0.013 0.01936 0.00012
EXB#91 3.219 0.017 0.088 0.022 -0.079 0.036 -0.012 0.013 0.01936 0.00012
EXB#91 3.219 0.017 0.088 0.022 -0.079 0.036 -0.012 0.013 0.01936 0.00012
EXB#92 3.523 0.014 0.081 0.004 -0.067 0.026 0.051 0.019 0.02015 0.00044
EXB#92 3.523 0.014 0.081 0.004 -0.067 0.026 0.051 0.019 0.02015 0.00044
EXB#92 3.523 0.014 0.081 0.004 -0.067 0.026 0.051 0.019 0.02015 0.00044
EXB#94 2.449 0.015 0.036 0.017 -0.051 0.013 -0.023 0.007 0.01431 0.00031
EXB#94 2.449 0.015 0.036 0.017 -0.051 0.013 -0.023 0.007 0.01431 0.00031
EXB#94 2.449 0.015 0.036 0.017 -0.051 0.013 -0.023 0.007 0.01431 0.00031
EXB#95 2.554 0.027 0.081 0.010 -0.040 0.011 0.018 0.020 0.01585 0.00021
EXB#95 2.554 0.027 0.081 0.010 -0.040 0.011 0.018 0.020 0.01585 0.00021
EXB#95 2.554 0.027 0.081 0.010 -0.040 0.011 0.018 0.020 0.01585 0.00021
(fA)
(fA)
(fA)
(fA)
(fA)
Matchan et al. 2016 Australian Journal of Earth Sciences 63/2 Supplementary Papers http://dx.doi.org/10.1080/08120099.2016.1156576
3

Table A2.
40
Ar/
39
Ar ARGUSVI data and blank values for laser step-heating analysis of sample NVP26 excluding interference corrections
a
Background correction
Sample Step Laser
40
Ar ±1σ
39
Ar ±1σ
38
Ar ±1σ
37
Ar ±1σ
36
Ar ±1σ
Blank no.
40
Ar ±1σ
39
Ar ±1σ
38
Ar ±1σ
37
Ar ±1σ
36
Ar ±1σ H1/Ax H1/L1 H1/L2 AX L1 L2 H1/CDD ±1σ
ID No
Power
[40] [40] [40] (1amu) (1amu) (1amu) (%)
NVP26-1 101.3 mg
NVP26-1a 1 4% 345.50 0.08 63.853 0.045 0.970 0.052 99.1 2.9 0.7383 0.0030
EXB#74
7.276 0.011 0.085 0.019 -0.121 0.043 0.020 0.027 0.03095 0.00053 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.402846 0.095942
NVP26-1b 2 6% 501.14 0.22 105.265 0.043 1.435 0.036 132.7 3.0 0.9957 0.0042
EXB#75
7.787 0.024 0.056 0.017 -0.055 0.030 -0.002 0.032 0.03330 0.00021 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.402846 0.095942
NVP26-1c 3 9% 530.49 0.13 104.695 0.076 1.491 0.035 138.7 4.1 1.1012 0.0027
EXB#75
7.787 0.024 0.056 0.017 -0.055 0.030 -0.002 0.032 0.03330 0.00021 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.402846 0.095942
NVP26-1d 4 12% 316.81 0.07 53.045 0.037 0.776 0.025 88.9 3.1 0.7279 0.0021
EXB#76
7.792 0.013 0.086 0.022 -0.062 0.020 0.025 0.011 0.03381 0.00035 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.402846 0.095942
NVP26-1e 5 18% 279.59 0.07 28.241 0.046 0.511 0.027 110. 9 1.8 0.7827 0.0015
EXB#76
7.792 0.013 0.086 0.022 -0.062 0.020 0.025 0.011 0.03381 0.00035 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.402846 0.095942
NVP26-2 71.5 mg
NVP26-2a 1 4% 645.08 0.34 106.176 0.078 1.561 0.029 173.3 2.5 1.4643 0.0030
EXB#82
3.336 0.016 0.060 0.018 -0.008 0.021 -0.014 0.015 0.01726 0.00011 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-2b 2 6% 702.98 0.29 144.424 0.108 2.006 0.032 191.8 2.0 1.4138 0.0022
EXB#82
3.336 0.016 0.060 0.018 -0.008 0.021 -0.014 0.015 0.01726 0.00011 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-2c 3 8% 563.02 0.16 117.998 0.060 1.653 0.030 142.5 2.3 1.1170 0.0031
EXB#83
3.393 0.019 0.092 0.017 -0.003 0.020 -0.009 0.015 0.01881 0.00014 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-2d 4 10% 450.09 0.10 86.957 0.030 1.186 0.023 113. 1 4.0 0.9472 0.0031
EXB#83
3.393 0.019 0.092 0.017 -0.003 0.020 -0.009 0.015 0.01881 0.00014 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-2e 5 14% 447.18 0.12 65.553 0.035 0.989 0.028 133.7 2.3 1.0914 0.0020
EXB#83
3.393 0.019 0.092 0.017 -0.003 0.020 -0.009 0.015 0.01881 0.00014 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-2f 6 20% 341.33 0.09 30.729 0.042 0.597 0.024 139.1 2.6 0.9677 0.0026
EXB#84
3.429 0.010 0.102 0.022 -0.044 0.022 0.020 0.014 0.01812 0.00036 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-2g 7 30% 199.01 0.06 13.620 0.032 0.299 0.027 99.1 2.3 0.5880 0.0018
EXB#84
3.429 0.010 0.102 0.022 -0.044 0.022 0.020 0.014 0.01812 0.00036 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-3 76.0 mg
NVP26-3a 1 4% 399.93 0.13 68.334 0.040 1.009 0.037 101.9 2.4 0.8986 0.0020
EXB#89
2.515 0.025 0.081 0.008 -0.083 0.017 0.035 0.014 0.01532 0.00035 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-3b 2 6% 516.57 0.33 103.752 0.042 1.533 0.024 136.2 2.1 1.0653 0.0024
EXB#89
2.515 0.025 0.081 0.008 -0.083 0.017 0.035 0.014 0.01532 0.00035 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-3c 3 8% 430.47 0.18 89.804 0.060 1.288 0.032 109.2 2.2 0.8707 0.0027
EXB#89
2.515 0.025 0.081 0.008 -0.083 0.017 0.035 0.014 0.01532 0.00035 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-3d 4 10% 325.98 0.08 64.531 0.052 1.037 0.016 85.5 2.0 0.6813 0.0018
EXB#90
2.707 0.029 0.092 0.023 -0.093 0.012 0.012 0.012 0.01736 0.00047 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-3e 5 14% 340.29 0.08 52.286 0.043 0.840 0.032 100.8 3.2 0.8155 0.0027
EXB#90
2.707 0.029 0.092 0.023 -0.093 0.012 0.012 0.012 0.01736 0.00047 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-3f 6 30% 445.42 0.07 36.862 0.068 0.778 0.028 185.6 2.7 1.3001 0.0027
EXB#90
2.707 0.029 0.092 0.023 -0.093 0.012 0.012 0.012 0.01736 0.00047 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-4 101.1 mg
NVP26-4a 1 4% 632.41 0.24 108.820 0.046 1.572 0.039 172.1 2.5 1.4162 0.0043
EXB#91
3.219 0.017 0.088 0.022 -0.079 0.036 -0.012 0.013 0.01936 0.00012 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-4b 2 6% 723.03 0.30 152.719 0.092 2.127 0.040 197.1 1.6 1.4335 0.0027
EXB#91
3.219 0.017 0.088 0.022 -0.079 0.036 -0.012 0.013 0.01936 0.00012 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-4c 3 8% 571.53 0.17 122.821 0.065 1.721 0.043 143.8 2.1 1.1265 0.0031
EXB#91
3.219 0.017 0.088 0.022 -0.079 0.036 -0.012 0.013 0.01936 0.00012 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-4d 4 10% 398.11 0.12 76.626 0.041 1.129 0.037 92.6 3.0 0.8510 0.0023
EXB#92
3.523 0.014 0.081 0.004 -0.067 0.026 0.051 0.019 0.02015 0.00044 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-4e 5 14% 427.80 0.09 58.773 0.036 0.971 0.026 129.7 2.8 1.0820 0.0020
EXB#92
3.523 0.014 0.081 0.004 -0.067 0.026 0.051 0.019 0.02015 0.00044 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-4f 6 30% 486.47 0.19 32.069 0.036 0.672 0.042 215.2 2.3 1.4824 0.0040
EXB#92
3.523 0.014 0.081 0.004 -0.067 0.026 0.051 0.019 0.02015 0.00044 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-5 101.0 mg
NVP26-5a 1 4% 740.37 0.26 128.622 0.073 1.943 0.075 208.2 3.1 1.6456 0.0036
EXB#94
2.449 0.015 0.036 0.017 -0.051 0.013 -0.023 0.007 0.01431 0.00031 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-5b 2 6% 783.34 0.27 168.168 0.077 2.360 0.016 206.6 1.3 1.5374 0.0035
EXB#94
2.449 0.015 0.036 0.017 -0.051 0.013 -0.023 0.007 0.01431 0.00031 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-5c 3 8% 575.39 0.10 121.683 0.051 1.692 0.021 141.9 2.6 1.1453 0.0024
EXB#94
2.449 0.015 0.036 0.017 -0.051 0.013 -0.023 0.007 0.01431 0.00031 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-5d 4 10% 391.34 0.08 71.243 0.049 0.999 0.043 102.9 4.8 0.8622 0.0027
EXB#95
2.554 0.027 0.081 0.010 -0.040 0.011 0.018 0.020 0.01585 0.00021 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-5e 5 14% 408.08 0.10 47.918 0.035 0.849 0.032 135.1 2.7 1.0787 0.0030
EXB#95
2.554 0.027 0.081 0.010 -0.040 0.011 0.018 0.020 0.01585 0.00021 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
NVP26-5f 6 30% 414.33 0.13 24.230 0.043 0.566 0.024 187.5 3.7 1.2803 0.0022
EXB#95
2.554 0.027 0.081 0.010 -0.040 0.011 0.018 0.020 0.01585 0.00021 1.001217 0.998905 0.993785 0.992794 0.990793 0.993521 320.505939 0.150435
(fA)
(fA)
(fA)
(fA)
(fA)
a
Data are corrected for mass spectrometer backgrounds, discrimination and radioactive decay.
Argus Sensitivity and Discrimination Corrections
(fA)
(fA)
(fA)
(fA)
(fA)
Matchan et al. 2016 Australian Journal of Earth Sciences 63/2 Supplementary Papers http://dx.doi.org/10.1080/08120099.2016.1156576
4

Figure'A1.'
40
Ar/
39
Ar(age(spectra(and(inverse(isochron(diagrams(for(individual(NVP26(groundmass(aliquants.(Errors(symbols(
are(1σ.(Grey(symbols(are(excluded(from(age(calculaHon(results.(In(inverse(isochron(diagrams,(solid(lines(represent(preferred(
isochron(results(and(dashed(lines(indicate(posiHon(of(inverse(isochrons(constructed(from(all(data(points.(Step(numbers(are(
indicated.(
300
320
340
360
380
400
420
440
460
480
500
Age (ka)
300
320
340
360
380
400
420
440
460
480
500
Age (ka)
Plateau steps are dark grey error symbols are 1σ
300
320
340
360
380
400
420
440
460
480
500
Age (ka)
300
320
340
360
380
400
420
440
460
480
500
0 20 40 60 80 100
Age (ka)
NVP26-1
Plateau age =391.1 ± 2.4 ka (2σ)
MSWD=1.6, p=0.2
Includes 74.1% of the
39
Ar
a
b
c
d
e
NVP26-2
Plateau age =394.4 ± 1.7 ka (2σ)
MSWD=1.9, p=0.2
Includes 61.8% of the
39
Ar
NVP26-3
Plateau age =387.1 ± 1.9 ka (2σ)
MSWD=1.1, p=0.3
Includes 74.7% of the
39
Ar
NVP26-4
f
g
h
1
2
3
4
5
0.0018
0.0020
0.0022
0.0024
0.0026
0.0028
0.0030
36
Ar/
40
Ar
39
Ar/
40
Ar
1
2
3
4
5
6
7
0.0018
0.0020
0.0022
0.0024
0.0026
0.0028
0.0030
1
2
3
4
5
6
0.0018
0.0020
0.0022
0.0024
0.0026
0.0028
0.0030
1
2
3
4
5
6
0.0018
0.0020
0.0022
0.0024
0.0026
0.0028
0.0030
0.04 0.08 0.12 0.16 0.20
error symbols are 1σ
36
Ar/
40
Ar
36
Ar/
40
Ar
36
Ar/
40
Ar
Cumulative %
39
Ar
NVP26-1
age = 403.3 ± 5.6 ka (2σ)
40
Ar/
36
Ar
i
= 292.7 ± 2.1 (2σ)
MSWD = 0.1
n = 4 of 5
NVP26-2
age = 393 ± 17 ka (95% CI)
40
Ar/
36
Ar
i
= 298.6 ± 5.2 (95% CI)
MSWD = 4
n = 5 of 7
NVP26-3
age = 391.6 ± 4.4 ka (2σ)
40
Ar/
36
Ar
i
= 296.3 ± 1.8 (2σ)
MSWD = 1.4
n = 5 of 6
NVP26-4
age = 395 ± 15 ka (95% CI)
40
Ar/
36
Ar
i
= 294.6 ± 5.9 (95% CI)
MSWD = 8.7
n =5 of 6
Matchan et al. 2016 Australian Journal of Earth Sciences 63/2 Supplementary Papers http://dx.doi.org/10.1080/08120099.2016.1156576
5

Citations
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Journal ArticleDOI
TL;DR: The Newer Volcanics Province of SE Australia is a very large continental basaltic province, with an area of >23 000 km2, a dense rock equivalent volume of <900 km3 and >400 monogenetic volcanoes; it has been active since c. 8 Ma.
Abstract: Abstract The Newer Volcanics Province of SE Australia is a very large continental basaltic province, with an area of >23 000 km2, a dense rock equivalent volume of <900 km3 and >400 monogenetic volcanoes; it has been active since c. 8 Ma. Lava fields, shields, scoria cones are common, and there are >40 maars and volcanic complexes. Maars occur dominantly in the south where magmas erupted through Tertiary sedimentary aquifers, whereas in the north, over Palaeozoic crust, there are few. Complex interactions of the magma volatile content, magma ascent rates, conduit characteristics and the availability and depth of aquifers caused diverse eruption styles. Volcanoes commonly occur close to major crustal faults, which acted as magma conduits. There is no simple age pattern of volcanism across the province. Volcanism was probably triggered by transtensional decompression in the crust where fault sets intersect, affecting hot, hydrated mantle that had welled up through edge-driven convection where the base of the lithosphere thins abruptly at the edge of the continent. Rock compositions range from picritic to basaltic andesitic. Some volcanoes are polymagmatic. Regional geophysical datasets have clarified the regional characteristics of the province, whereas detailed ground magnetic and gravity surveys resulted in new insights into the subsurface structure of maar-diatremes.

30 citations


Cites background from "A new 40Ar/39Ar eruption age for th..."

  • ...…(McDougall et al. 1966; Aziz-ur-Rahman & McDougall 1972; Gray & McDougall 2009; Gouramanis et al. 2010; Matchan & Phillips 2011; Ismail et al. 2013; Matchan et al. 2016), and possibly as early as 7.8 Ma (Edwards et al. 2004), to about 5 ka (McDougall & Gill 1975; Blackburn 1966; Blackburn et al.…...

    [...]

Journal ArticleDOI
TL;DR: In this paper, the authors present 40Ar/39Ar ages of volcanic features in the Cenozoic intraplate Newer Volcanic Province in southeast Australia, and suggest that magmatism is related to the complex interplay of upwelling due to edge-driven convection and the Cosgrove track mantle plume located in the northeast of the province at 6.5-5 Ma.
Abstract: Here we present 40Ar/39Ar ages of volcanic features in the Cenozoic intraplate Newer Volcanic Province in southeast Australia. The <5 Ma volcanic products in the Newer Volcanic Province can be subdivided into tholeiitic, valley-filling Newer Plains basalts, and alkaline scoria cones, lava shields, and maars of the Newer Cones series. Plateau ages range from 3.76 ± 0.01 to 4.32 ± 0.03 Ma (2σ; all sources of uncertainties included) for the Newer Plains series, with production rates of volcanism decreasing post 4 Ma. We suggest that magmatism is related to the complex interplay of magma upwelling due to edge-driven convection and the Cosgrove track mantle plume located in the northeast of the province at 6.5–5 Ma. Plateau ages range from 1290 ± 20 to 41.1 ± 2.2 ka (2σ) for the Newer Cones series, with a diffuse age progression in the onset of volcanism for these features from east to west. Analyses of the distribution and geomorphology of these volcanic features indicates a strong control of basement faults on volcanism, reflected in alignment of volcanic features along Paleozoic north-south oriented basement faults in the east and Cretaceous northwest-southeast oriented extensional features in the west. This age progression can be explained by a westerly migration of stress derived from the left-lateral strike-slip Tasman Fracture Zone. This suggests that the general mechanism of volcanism changed from upwelling due to plume-assisted edge-driven convection prior to ∼4 Ma to stress-dependent upwelling at around 1.3 Ma.

24 citations

Journal ArticleDOI
TL;DR: In this article, entrained anorthoclase megacrysts were used to yield 40Ar/39Ar ages for scoria cones and maars from the Pliocene-Holocene Newer Volcanic Province (NVP) of south-eastern Australia.

10 citations

Journal ArticleDOI
TL;DR: In this paper, a holistic approach to lava flow mapping is employed to unravel the complex network, incorporating diagnostic petrography, geochemistry and precise 40Ar/39Ar geochronology.

4 citations

References
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Journal ArticleDOI
TL;DR: The West Victorian Uplands is a region of low relief, gentle gradients, young volcanicity and local domal uplift as mentioned in this paper, which distinguishes it from the rest of the Eastern Highlands of Australia.
Abstract: The West Victorian Uplands is a region of low relief, gentle gradients, young volcanicity and local domal uplift These characteristics distinguish it from the rest of the Eastern Highlands of Australia The origin of the West Victorian Uplands dates back to uplift in the Cretaceous, but elevation and relief have always remained low Further uplift, extending westwards from central Victoria, may have begun raising the West Victorian Uplands in Middle Tertiary times Doming, fault activity, earthquakes and volcanism are extending progressively westwards Not only may the Eastern Highlands of Victoria have grown in this way in the past, but the area may also provide a view of the early evolution of the Eastern Highlands of Australia

11 citations


"A new 40Ar/39Ar eruption age for th..." refers background in this paper

  • ...In the Central Highlands subprovince, volcanoes erupted within an already uplifted and dissected terrain (Boyce, 2013; Holdgate et al., 2006; Joyce, 1992, 1999)....

    [...]

Journal ArticleDOI
TL;DR: The Streatham Deep-Lead System covers >2500 km2 between the West Victorian Uplands and the Otway Basin, from which it is separated by a subsurface granite ridge.
Abstract: The mainly sub-basaltic paleodrainage of the Streatham Deep-Lead System covers >2500 km2 between the West Victorian Uplands and the Otway Basin, from which it is separated by a subsurface granite ridge. Five main tributaries flowed southwards into a series of grabens that host up to 140 m of fluvial coal-bearing sediments (Yaloak/Calivil Formation). The grabens were probably initially connected to the ocean (Otway Basin) through a western outlet; in the Eocene, the outlet shifted eastwards. Accumulation of the deep-lead sediments in the central grabens was controlled by synsedimentary subsidence along reactivated north-northwest Paleozoic and east-northeast Cretaceous faults. Fault movement occurred in the mid-Late Paleocene in the western depocentre, and Eocene in the central and eastern depocentres, and correlates well with tectonic activity in the eastern part of the Otway Basin. Following an Early Oligocene hiatus, fluvial sedimentation and syndepositional faulting recommenced from the Late Oligocene ...

10 citations


"A new 40Ar/39Ar eruption age for th..." refers background in this paper

  • ...Furthermore, as NVP basalts significantly modified regional drainage patterns (e.g. Raiber & Webb, 2008; Taylor & Gentle, 2002), determining well-constrained eruption ages for key flows may provide useful stratigraphic markers for changes in paleo-environment (e.g. Baker, 2008)....

    [...]

Journal ArticleDOI
01 Jan 2013
TL;DR: In this article, the authors used seven alkali feldspar samples, mostly anorthoclase megacrysts, from volcanic centres in the Newer Volcanic Province (NVP) in Victoria, with extension into south-eastern South Australia, for 40Ar/39Ar dating in the present study.
Abstract: The Newer Volcanic Province (NVP) in Victoria, with extension into south-eastern South Australia, represents the youngest chapter of Cenozoic volcanism in south-eastern Australia. However, most ages have been determined by the potassium–argon (K–Ar) method, and the age data are not comprehensive. In addition, few ages exist for the array of scoria cone volcanoes in the NVP. Seven alkali feldspar samples, mostly anorthoclase megacrysts, from volcanic centres in the NVP were used for 40Ar/39Ar dating in the present study. In geochronological order, with ages quoting 95% confidence limits, locations are Mount Franklin near Daylesford (0.110 ± 0.014 Ma), Red Rock near Alvie (0.116 ± 0.048 Ma), Lake Bullenmerri at Camperdown (0.116 ± 0.019 Ma), Ridge Road Quarry near Daylesford (2.01 ± 0.11 Ma) and Mount Kororoit near Diggers Rest (3.74 ± 0.26 Ma). Two samples from The Anakies, near Bacchus Marsh, produced discordant results suggesting a maximum age of ca. 1.9 Ma. The analyses and reported ages in the present study not only provide new geochronological data for the province, but also elucidate the difficulties in dating very young basalts using the 40Ar/39Ar dating method. These results are consistent with the erosion levels of the scoria volcanoes sampled, and indicate a major episode of explosive volcanic activity at ca. 100 ka. In contrast, the more eroded Mount Kororoit is considered to be ca. 3.7 Ma in age. The age of The Anakies is more equivocal owing to the indicated presence of excess argon and a maximum age of ca. 1.9 Ma is suggested for this locality. Given the latter results and lack of precision obtainable from the younger samples, the possibility remains that other samples contained extraneous argon and that the ages generated are thus maximum eruption ages. Analyses of additional samples from these and other localities will be required to further resolve this issue.

6 citations


"A new 40Ar/39Ar eruption age for th..." refers background in this paper

  • ...…low to high temperature observed for all other step-heating experiments is characteristic of fine-grained samples that have experienced irradiation-induced recoil of 39Ar and 37Ar between phases with differing K- and Ca-contents (e.g. Jourdan & Renne, 2014; Koppers, Staudigel, & Wijbrans, 2000)....

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  • ...Assuming that all 39Ar and 37Ar have been retained in the sample, but redistributed between phases (i.e. no net loss), the total gas age should approximate the groundmass crystallisation age (e.g. Jourdan & Renne, 2014)....

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  • ...Although these distances are small, the recoil loss/redistribution of 39ArK and 37ArCa in fine-grained samples can have a significant effect on 40Ar/39Ar apparent ages, especially in the case of Ca-rich samples (e.g. Jourdan & Renne, 2014; Koppers et al., 2000)....

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