Relevant bibliographies by topics / Newer Volcanic Province

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Academic literature on the topic 'Newer Volcanic Province'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Newer Volcanic Province"

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Gray, C. M., and I. McDougall. "K-Ar geochronology of basalt petrogenesis, Newer Volcanic Province, Victoria." Australian Journal of Earth Sciences 56, no. 2 (March 2009): 245–58. http://dx.doi.org/10.1080/08120090802547066.

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Cas, R. A. F., J. van Otterloo, T. N. Blaikie, and J. van den Hove. "The dynamics of a very large intra-plate continental basaltic volcanic province, the Newer Volcanics Province, SE Australia, and implications for other provinces." Geological Society, London, Special Publications 446, no. 1 (November 7, 2016): 123–72. http://dx.doi.org/10.1144/sp446.8.

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Ismail, Rafika, David Phillips, and William D. Birch. "40Ar/39Ar dating of alkali feldspar megacrysts from selected young volcanoes of the Newer Volcanic Province, Victoria." Proceedings of the Royal Society of Victoria 125, no. 2 (2013): 59. http://dx.doi.org/10.1071/rs13019.

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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.
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Aivazpourporgou, Sahereh, Stephan Thiel, Patrick Hayman, Louis Moresi, and Graham Heinson. "Results from long-period MT array in the Newer Volcanic Province, Western Victoria, Australia." ASEG Extended Abstracts 2013, no. 1 (December 2013): 1–3. http://dx.doi.org/10.1071/aseg2013ab370.

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5

Vogel, Derek C., and Reid R. Keays. "The petrogenesis and platinum-group element geochemistry of the Newer Volcanic Province, Victoria, Australia." Chemical Geology 136, no. 3-4 (April 1997): 181–204. http://dx.doi.org/10.1016/s0009-2541(96)00142-8.

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Graeber, Frank M., Gregory A. Houseman, and Stewart A. Greenhalgh. "Regional teleseismic tomography of the western Lachlan Orogen and the Newer Volcanic Province, southeast Australia." Geophysical Journal International 149, no. 2 (May 2002): 249–66. http://dx.doi.org/10.1046/j.1365-246x.2002.01598.x.

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7

Phillips, David. "40Ar/39Ar geochronology of feldspar megacrysts from Late Pleistocene volcanoes, Newer Volcanic Province, southeast Australia." Quaternary International 279-280 (November 2012): 379–80. http://dx.doi.org/10.1016/j.quaint.2012.08.1176.

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8

Blaikie, T. N., L. Ailleres, P. G. Betts, and R. A. F. Cas. "Interpreting subsurface volcanic structures using geologically constrained 3-D gravity inversions: Examples of maar-diatremes, Newer Volcanics Province, southeastern Australia." Journal of Geophysical Research: Solid Earth 119, no. 4 (April 2014): 3857–78. http://dx.doi.org/10.1002/2013jb010751.

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9

Oostingh, K. F., F. Jourdan, E. L. Matchan, and D. Phillips. "40Ar/39Ar geochronology reveals rapid change from plume-assisted to stress-dependent volcanism in the Newer Volcanic Province, SE Australia." Geochemistry, Geophysics, Geosystems 18, no. 3 (March 2017): 1065–89. http://dx.doi.org/10.1002/2016gc006601.

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10

Van Otterloo, J., M. Raveggi, R. A. F. Cas, and R. Maas. "Polymagmatic Activity at the Monogenetic Mt Gambier Volcanic Complex in the Newer Volcanics Province, SE Australia: New Insights into the Occurrence of Intraplate Volcanic Activity in Australia." Journal of Petrology 55, no. 7 (June 13, 2014): 1317–51. http://dx.doi.org/10.1093/petrology/egu026.

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Dissertations / Theses on the topic "Newer Volcanic Province"

1

Hare, Alison (Alison Grace) 1976. "The stratigraphy and evolution of the late Cenozoic, intra-plate Werribee Plains basaltic lava flow-field, Newer Volcanic Province, Victoria, Australia." Monash University, School of Geosciences, 2002. http://arrow.monash.edu.au/hdl/1959.1/7586.

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2

Oostingh, Kornelia Fieneke. "Ultra-Precise 40Ar/39Ar Geochronology: Development of 38Ar cosmogenic exposure and olivine (U-Th)/He dating techniques; and deciphering the geochemical evolution of the Newer Volcanic Province, SE Australia." Thesis, Curtin University, 2017. http://hdl.handle.net/20.500.11937/53004.

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In this study, existing (40Ar/39Ar) and underdeveloped (terrestrial cosmogenic 38Ar exposure dating and olivine (U-Th)/He dating) geochronology techniques are used and improved to better understand the igneous geology and landscape evolution of Australia. It is shown that an integral approach of geochemistry and ultra-precise geochronology, using the new generation multi-collector mass spectrometers, is of paramount importance to decipher the volcanic history of the small, intraplate Newer Volcanic Province in SE Australia.
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Launder, J. D. G. "Geochemical fingerprinting of Australia’s youngest volcanoes: The Newer Volcanic Province, South Australia and Victoria." Thesis, 2017. http://hdl.handle.net/2440/128255.

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Traces of volcanic tephra, known as cryptotephra can provide an important isochronous marker that allows sedimentary archives to be aligned in space and time. However, this use of cryptotephra requires an understanding of the unique chemical fingerprint of the glass shards that originate from a particular volcano. Subsequently, this study investigates how the geochemical composition of volcanic centres varies between volcanic centres using collected samples from 9 volcanoes within the NVP, SA and Victoria. Analysis of geochemical data was obtained through laser ablation ICP-MS, to augment previously analysed electron microprobe data for 7 of the 9 sites. This study also investigates the viability of trace element analysis of cryptotephra grains through laser ablation as a useful addition to the major oxide analysis that can be carried out by electron microprobe. Statistical models of linear regression analysis, regression trees and KS-tests, were employed to identify the degree to which the volcanoes studied can be discriminated according to their elemental composition, on the basis of their major oxides and trace elements. The experimental results indicate that a quantifiable difference in major and trace elemental composition can be determined for all volcanic centres analysed except samples obtained from Warrnambool. Subsequently, this study has successfully identified 8 volcanoes with tephra and crypyotephra that possess specific geochemical fingerprints.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2017
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