Journal articles: 'Australian goldfields'

1

Robbins, W. M., and Alan Mayne. "Hill End: An Australian Goldfields Landscape." Labour History, no. 93 (2007): 243. http://dx.doi.org/10.2307/27516253.

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TIMMS, BRIAN V. "Six new species of the brine shrimp Parartemia Sayce 1903 (Crustacea: Anostraca: Artemiina) in Western Australia." Zootaxa 2715, no. 1 (January 22, 2019): 1. http://dx.doi.org/10.11646/zootaxa.2715.1.1.

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The Australian anostracan fauna is generically depauperate, but species-rich due to radiation within Branchinella and also Parartemia. Most Parartemia, including the six new species, occur in Western Australia, with P. boomeranga sp. nov. in the inner Wheatbelt, P. mouritzi sp. nov. in the eastern Wheatbelt, P. purpurea sp. nov. in the Esperance hinterland, P. veronicae sp. nov. in the Goldfields, P. bicorna sp. nov. in Lake Carey in the northern Goldfields and P. laticaudata sp. nov. in the far north and the Northern Territory. All species use lock and key amplexus meaning that the second antennae of males are highly differentiated and in females the last few thoracomeres are variously modified and the 10th, and especially 11th, thoracopods much reduced. Although many of the new species occur in remote salinas, some are endangered due to anthropogenic salinisation.

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Jorgensen, Darren. "Flags and landscapes: border art from the Australian goldfields." World Art 8, no. 2 (July 3, 2018): 207–24. http://dx.doi.org/10.1080/21500894.2018.1522370.

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4

Prangnell, Jonathan, and Kate Quirk. "Children in Paradise: Growing Up on the Australian Goldfields." Historical Archaeology 43, no. 3 (September 2009): 38–49. http://dx.doi.org/10.1007/bf03376759.

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Murray, B. R., C. R. Dickman, C. H. S. Watts, and S. R. Morton. "The dietary ecology of Australian rodents." Wildlife Research 26, no. 6 (1999): 857. http://dx.doi.org/10.1071/wr97046_co.

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Very little systematic information has been collected on the diets of Australian rodents in arid and semiarid regions. The information that is available is restricted generally to short periods of sampling and small sample sizes. Here we review the diets of 15 extant and one extinct species of Australian desert rodents, and provide new results of dietary analyses for (1) Leggadina forresti, Pseudomys desertorand Rattus villosissimus from the Simpson Desert, south-western Queensland, (2) P. albocinereus and P. bolami from the western goldfields of Western Australia, and (3) Notomys alexis, P. desertor and P. hermannsburgensis from the Tanami Desert, Northern Territory. Overwhelmingly, omnivory is the predominant dietary strategy, with most species (11) taking substantial amounts of invertebrate, seed and green plant material. Of the other five species, four can be considered herbivores and one a granivore. Of the four herbivores, however, one is extinct (Leporillus apicalis), one is restricted to an offshore island (Lep. conditor), while another (P. fieldi) is classified as a herbivore from a diet sample of four individuals only. Similarly, P. occidentalis is classified as a granivore on the basis of dietary sampling of two individuals alone. These findings indicate that omnivory, over and above any other dietary strategy including granivory, is predominant among rodents inhabiting Australian deserts.

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Murray, B. R., C. R. Dickman, C. H. S. Watts, and S. R. Morton. "The dietary ecology of Australian desert rodents." Wildlife Research 26, no. 4 (1999): 421. http://dx.doi.org/10.1071/wr97046.

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Very little systematic information has been collected on the diets of Australian rodents in arid and semiarid regions. The information that is available is restricted generally to short periods of sampling and small sample sizes. Here we review the diets of 15 extant and one extinct species of Australian desert rodents, and provide new results of dietary analyses for (1) Leggadina forresti, Pseudomys desertorand Rattus villosissimus from the Simpson Desert, south-western Queensland, (2) P. albocinereus and P. bolami from the western goldfields of Western Australia, and (3) Notomys alexis, P. desertor and P. hermannsburgensis from the Tanami Desert, Northern Territory. Overwhelmingly, omnivory is the predominant dietary strategy, with most species (11) taking substantial amounts of invertebrate, seed and green plant material. Of the other five species, four can be considered herbivores and one a granivore. Of the four herbivores, however, one is extinct (Leporillus apicalis), one is restricted to an offshore island (Lep. conditor), while another (P. fieldi) is classified as a herbivore from a diet sample of four individuals only. Similarly, P. occidentalis is classified as a granivore on the basis of dietary sampling of two individuals alone. These findings indicate that omnivory, over and above any other dietary strategy including granivory, is predominant among rodents inhabiting Australian deserts.

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Brennan, G. K., and P. Newby. "Potential of Western Australian Eastern Goldfields timbers for high quality wood products." Australian Forestry 55, no. 1-4 (January 1992): 74–79. http://dx.doi.org/10.1080/00049158.1992.10676100.

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8

Stafford, RA. "Preventing the 'Curse of California': Advice for English Emigrants to the Australian Goldfields." Historical Records of Australian Science 7, no. 3 (1987): 215. http://dx.doi.org/10.1071/hr9880730215.

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9

Hartley, Richard. "Bewick Moreing in Western Australian Gold Mining 1897-1904: Management Policies & Goldfields Responses." Labour History, no. 65 (1993): 1. http://dx.doi.org/10.2307/27509195.

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10

Oliver, Bobbie, and Richard G. Hartley. "River of Steel: A History of the Western Australian Goldfields and Agricultural Water Supply." Labour History, no. 95 (2008): 263. http://dx.doi.org/10.2307/27516329.

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11

TONTS, MATTHEW. "Labour Market Dynamics in Resource Dependent Regions: an Examination of the Western Australian Goldfields." Geographical Research 48, no. 2 (November 2, 2009): 148–65. http://dx.doi.org/10.1111/j.1745-5871.2009.00624.x.

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12

Flanigan, J. E., P. C. Withers, C. J. Fuery, and M. Guppy. "Metabolic depression and Na+/K+ gradients in the aestivating Australian goldfields frog, Neobatrachus wilsmorei." Journal of Comparative Physiology B 163, no. 7 (December 1993): 587–93. http://dx.doi.org/10.1007/bf00302118.

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13

Sinclair, Craig, Peter Keelan, Samuel Stokes, Annette Stokes, and Christine Jeffries-Stokes. "Participatory video making for research and health promotion in remote Australian Aboriginal communities." International Journal of Critical Indigenous Studies 8, no. 1 (January 1, 2015): 2–16. http://dx.doi.org/10.5204/ijcis.v8i1.129.

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This paper describes the participatory video (PV) method as a means of engaging children in remote Aboriginal communities as participants in health research. The PV method was piloted in two remote communities in the Goldfields region of Western Australia. There was widespread community acceptance of this approach and preliminary findings are discussed with reference to the key themes of perspectives on health, benefits to participants and benefits to communities. The PV method has a number of strengths, including flexibility to respond to community priorities, a lack of dependence on verbal or written data collection and the capacity to generate immediate benefits for participants. While not without methodological problems, these pilot projects suggest that the PV method is well suited to the remote Aboriginal communities who participated. The ethical implications of the PV method are discussed with specific reference to published ethical guidelines.

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14

Bedka, Kristopher M., John T. Allen, Heinz Jurgen Punge, Michael Kunz, and Denis Simanovic. "A Long-Term Overshooting Convective Cloud-Top Detection Database over Australia Derived from MTSAT Japanese Advanced Meteorological Imager Observations." Journal of Applied Meteorology and Climatology 57, no. 4 (April 2018): 937–51. http://dx.doi.org/10.1175/jamc-d-17-0056.1.

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ABSTRACTA 10-yr geostationary (GEO) overshooting cloud-top (OT) detection database using Multifunction Transport Satellite (MTSAT) Japanese Advanced Meteorological Imager (JAMI) observations has been developed over the Australian region. GEO satellite imagers collect spatially and temporally detailed observations of deep convection, providing insight into the development and evolution of hazardous storms, particularly where surface observations of hazardous storms and deep convection are sparse and ground-based radar or lightning sensor networks are limited. Hazardous storms often produce one or more OTs that indicate the location of strong updrafts where weather hazards are typically concentrated, which can cause substantial impacts on the ground such as hail, damaging winds, tornadoes, and lightning and to aviation such as turbulence and in-flight icing. The 10-yr OT database produced using an automated OT detection algorithm is demonstrated for analysis of storm frequency, diurnally, spatially, and seasonally relative to known features such as the Australian monsoon, expected regions of hazardous storms along the southeastern coastal regions of southern Queensland and New South Wales, and the preferential extratropical cyclone track along the Indian Ocean and southern Australian coast. A filter based on atmospheric instability, deep-layer wind shear, and freezing level was used to identify OTs that could have produced hail. The filtered OT database is used to generate a hail frequency estimate that identifies a region extending from north of Brisbane to Sydney and the Goldfields–Esperance region of eastern Western Australia as the most hail-prone regions.

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15

Giachino, Pier Mauro, Stefan Eberhard, and Giulia Perina. "A rich fauna of subterranean short-range endemic Anillini (Coleoptera, Carabidae, Trechinae) from semi-arid regions of Western Australia." ZooKeys 1044 (June 16, 2021): 269–337. http://dx.doi.org/10.3897/zookeys.1044.58844.

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Globally, the great majority of Anillini species are endogean, adapted to live in the interstices of soil and leaf litter, while the extremely low vagility of these minute ground beetles gives rise to numerous shortrange endemic species. Until recently the Australian Anillini fauna was known only from leaf litter in rain forests and eucalypt forests in the wetter, forested regions of eastern and south eastern Australia, as well as Lord Howe and Norfolk islands. The first hypogean Anillini in Australia (17 species in six genera) were described in 2016 from mineral exploration drill holes in iron-ore bearing rocks of the Pilbara region in Western Australia, representing the first finding of the tribe deep underground in a semi-arid climate region. A further eight new genera and 20 new species are described herein, mostly from the Pilbara region as well as the semi-arid Kimberley and Goldfields regions; all were collected in mineral exploration drill holes. The following new genera are described: Erwinanillusgen. nov., Gregorydytesgen. nov., Pilbaraphanusgen. nov., Neoillaphanusgen. nov., Kimberleytyphlusgen. nov., Gilesdytesgen. nov., Pilbaradytesgen. nov., and Bylibaraphanusgen. nov. The following new species are described: Erwinanillus baehrisp. nov.; Gracilanillus hirsutussp. nov., G. pannawonicanussp. nov.; Gregorydytes ophthalmianussp. nov.; Pilbaraphanus chichesterianussp. nov., P. bilybarianussp. nov.; Magnanillus firetalianussp. nov., M. sabaesp. nov., M. salomonissp. nov., M. regalissp. nov., M. serenitatissp. nov.; Neoillaphanus callawanussp. nov.; Kimberleytyphlus carrboydianussp. nov.; Austranillus jinayrianussp. nov.; Gilesdytes pardooanussp. nov., G. ethelianussp. nov.; Pilbaradytes abydosianussp. nov., P. webberianussp. nov.; Bylibaraphanus cundalinianussp. nov.; and Angustanillus armatussp. nov. Identification keys are provided for all Australian anilline genera, and Western Australian species. All the described species are known from a single locality and qualify as short-range endemics. The Anillini are recognised as a significant and diverse element making up part of Western Australia’s remarkable subterranean fauna, and whose conservation may potentially be impacted by mining developments.

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16

Tutchener, D., S. Aird, M. Boulden, and A. Cooper. "The ‘taphonomy’ of the Australian great bowerbird within the Wenlock Goldfields, Cape York Peninsula Queensland." Australian Archaeology 83, no. 1-2 (May 4, 2017): 71–74. http://dx.doi.org/10.1080/03122417.2017.1351684.

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17

Jones, Jennifer. "Faith and Failure on the Australian Goldfields: Gendered Interpretations of Piety and the “Good Death”." Journal of Religious History 43, no. 4 (November 21, 2019): 460–77. http://dx.doi.org/10.1111/1467-9809.12627.

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18

Reeves, Andrew, Tom Savage, A. W. Jenkinson, and J. B. Scott. "Yours 'Til the War of Classes is Ended': Obu Organisers on Western Australian Eastern Goldfields." Labour History, no. 65 (1993): 19. http://dx.doi.org/10.2307/27509196.

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19

Laurent, John. "Mechanics’ institutes and the labor movement: A case study of the west Australian goldfields, 1895–1917." Melbourne Studies in Education 29, no. 1 (January 1987): 81–98. http://dx.doi.org/10.1080/17508488709556223.

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20

Tonts, Matthew, Kirsten Martinus, and Paul Plummer. "Regional development, redistribution and the extraction of mineral resources: The Western Australian Goldfields as a resource bank." Applied Geography 45 (December 2013): 365–74. http://dx.doi.org/10.1016/j.apgeog.2013.03.004.

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21

Friedel, Margaret, Don Burnside, and Alec Holm. "Developing Land Use Policy for Environmental Objectives: Some Perspectives from the Rangeways Project in the Western Australian Goldfields." Australasian Journal of Environmental Management 9, no. 1 (January 2002): 12–26. http://dx.doi.org/10.1080/14486563.2002.10648539.

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22

Yeates, Anthony. "Not a Poor Man's Field: the New Guinea goldfields to 1942 — an Australian colonial history. By Michael Waterhouse." Journal of Pacific History 46, no. 1 (June 2011): 142–43. http://dx.doi.org/10.1080/00223344.2011.573649.

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23

Spry, Caroline, Rebekah Kurpiel, Elizabeth Foley, Jodi Turnbull, and Paul Penzo-Kajewski. "Disentangling activity traces on Australian goldfields: An experimental study of quartz assemblages derived from knapping and gold prospecting." Australian Archaeology 87, no. 1 (January 2, 2021): 49–62. http://dx.doi.org/10.1080/03122417.2021.1885109.

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24

J. Yates, Colin, Richard J. Hobbs, and Richard W. Bell. "Landscape-scale disturbances and regeneration in semi-arid woodlands of southwestern Australia." Pacific Conservation Biology 1, no. 3 (1994): 214. http://dx.doi.org/10.1071/pc940214.

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Woodlands dominated by Eucalyptus salmonophloia occur both in the fragmented landscapes of the Western Australian wheatbelt and in the adjacent unfragmented goldfields area. We examined the responses of the unfragmented woodlands to landscape-scale disturbances caused by fire, floods, windstorms and drought. Sites known to have experienced disturbances of these types over the past 50 years all had cohorts of sapling-stage E. salmonophloia and other dominant Eucalyptus species. Sites disturbed either by fire, flood or storm during 1991-92 displayed adult tree mortality and extensive seedling establishment, although rates of establishment and survival varied between sites. No regeneration was observed at equivalent undisturbed sites. These results indicate that landscape-scale disturbances of several types are important drivers of the dynamics of these semi-arid woodlands. Lack of regeneration of fragmented woodlands in the wheatbelt is likely to be due to changed disturbance regimes coupled with altered physical and biotic conditions within remnants. We argue that it may be difficult to identify processes which are important for the long-term persistence of natural ecosystems in fragmented landscapes without reference to equivalent unfragmented areas.

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Heath, Christopher J., and Ian H. Campbell. "A New Geochemical Technique for Gold Exploration: Alkali Element Mobility Associated with Gold Mineralization in the West Australian Goldfields." Economic Geology 99, no. 2 (March 2004): 313–24. http://dx.doi.org/10.2113/gsecongeo.99.2.313.

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26

Rice, Clive M., Mark D. Welch, John W. Still, Alan J. Criddle, and Chris J. Stanley. "Honeaite, a new gold-thallium-telluride from the Eastern Goldfields, Yilgarn Craton, Western Australia." European Journal of Mineralogy 28, no. 5 (January 24, 2016): 979–90. http://dx.doi.org/10.1127/ejm/2016/0028-2559.

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27

Chrimes, M. "Book reviewRIVER OF STEEL: A HISTORY OF THE WESTERN AUSTRALIAN GOLDFIELDS AND AGRICULTURAL WATER SUPPLY 1895–2003 HartleyR. G. Access Press, Perth, 2007, ISBN 9780864451965, AUS $50, 522 pp." Proceedings of the Institution of Civil Engineers - Engineering History and Heritage 162, no. 3 (August 2009): 168. http://dx.doi.org/10.1680/ehah.2009.162.3.168.

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Grguric, B. A., I. C. Madsen, and A. Pring. "Woodallite, a new chromium analogue of iowaite from the Mount Keith nickel deposit, Western Australia." Mineralogical Magazine 65, no. 3 (June 2001): 427–35. http://dx.doi.org/10.1180/002646101300119501.

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AbstractWoodallite is a new Cr-rich member of the hydrotalcite group from the large, low-grade Mount Keith nickel deposit, in the northeastern Goldfields district of Western Australia. Woodallite occurs as whorls and clusters of minute platelets up to 6 mm across in lizardite+brucite-altered dunite. Individual platelets are typically 10–100 µm in maximum dimension and are often curved. Associated minerals include chromite, lizardite, iowaite, pentlandite, magnetite, tochilinite and brucite. Electron microprobe analysis gave: Mg 25.90 wt.%; Cr 10.81; Fe 4.86; Al 0.68; Cl 9.89; S 0.03; Si 0.01; Ni 0.01; Na 0.01, yielding (after correction for loss of volatiles) an empirical formula of Mg6.19(Cr1.21Fe0.51Al0.15)∑1.87(OH)16[Cl1.62(CO3)0.17(SO4)0.01]·4H2O, by analogy with the hydrotalcite group. The simplified formula is Mg6Cr2(OH)16Cl2·4H2O. Combined thermogravimetric analysis and mass spectroscopy showed a two-stage weight loss of 12.7% and 27.3% occurring over the ranges 25–300°C and 300–660°C, respectively. The first weight loss is attributed to loss of interlayer water, chlorine-bearing species (e.g. HCl) and some CO2, the second to loss of hydroxide water, remaining CO2 and Cl species. The mineral is deep magenta to purple in colour, transparent, with a resinous to waxy lustre, and a perfect basal {0001} cleavage. Woodallite has a Mohs hardness of 1.5–2, and a pale-pink to white streak. The strongest lines in the X-ray powder pattern are [dobs (Iobs) (hkl)] 8.037 (100) (003); 4.021 (48) (006); 2.679 (1) (009); 2.624 (3) (012); 2.349 (5) (015); 2.007 (6) (0,0,12); 1.698 (2) (0,1,11); 1.524 (2) (21̄3). These lines were indexed on a hexagonal cell with a = 3.103(2), c = 24.111(24)Å, V = 201.14 Å3 and Z = 3/8. The new mineral is isostructural with the hydrotalcite group and has space group R3̄m. The measured density is 2.062 gm/cm3. Woodallite is uniaxial negative with ω = 1.555 and ε = 1.535 (white light); pleochroism is distinct from violet to pinkish lilac. Woodallite forms as a result of hydrothermal alteration of primary magmatic chromite by Clrich solutions at temperatures <320°C. Relict chromite fragments are frequently present in the whorls, and associated magnetite is altered extensively to iowaite. The mineral is named after Roy Woodall, eminent Australian industry geologist.

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29

Sedgwick, Laura. "Rushing for Gold: Life and Commerce on the Goldfields of New Zealand and Australia, Lloyd Carpenter and Lyndon Fraser (eds) (2016)." Journal of New Zealand & Pacific Studies 9, no. 1 (June 1, 2021): 104–6. http://dx.doi.org/10.1386/nzps_00053_5.

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Review of: Rushing for Gold: Life and Commerce on the Goldfields of New Zealand and Australia, Lloyd Carpenter and Lyndon Fraser (eds) (2016) Dunedin: Otago University Press, 344 pp., ISBN 978 1 87757 854 0 (pbk), NZ$45

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30

Davies, Peter, Susan Lawrence, Jodi Turnbull, Ian Rutherfurd, Ewen Silvester, James Grove, and Mark G. Macklin. "Groundwater extraction on the goldfields of Victoria, Australia." Hydrogeology Journal 28, no. 7 (June 24, 2020): 2587–600. http://dx.doi.org/10.1007/s10040-020-02196-w.

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31

Street, G. J. "MMR surveys for the location of palaeochannels in the Eastern Goldfields, Western Australia." Exploration Geophysics 20, no. 2 (1989): 123. http://dx.doi.org/10.1071/eg989123.

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The magnetometric resistivity (MMR) method was used to locate palaeodrainage channels in the Eastern Goldfields of Western Australia. Drilling results showed the method does not distinguish between the palaeochannel and porous weathered basement containing saline water. This distinction however was not essential to the success of the program as the weathered basement was generally symmetrical around the channel.

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32

Hartley, R. G. "Lessons from Western Australia's goldfields water supply scheme." Proceedings of the Institution of Civil Engineers - Engineering History and Heritage 163, no. 3 (August 2010): 179–87. http://dx.doi.org/10.1680/ehah.2010.163.3.179.

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33

Davies, Peter, and Susan Lawrence. "Flows of water on a nineteenth-century Australian goldfield." Water History 5, no. 3 (July 25, 2013): 331–47. http://dx.doi.org/10.1007/s12685-013-0082-2.

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34

Gibbs, Leah M. "Decolonising, Multiplicities and Mining in the Eastern Goldfields, Western Australia." Australian Geographical Studies 41, no. 1 (March 2003): 17–28. http://dx.doi.org/10.1111/1467-8470.00189.

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35

Glasson, M. J., R. W. Lehne, and F. W. Wellmer. "Gold exploration in the callion area, eastern goldfields, western Australia." Journal of Geochemical Exploration 31, no. 1 (December 1988): 1–19. http://dx.doi.org/10.1016/0375-6742(88)90034-9.

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36

Arne, D. C., J. E. Stott, and H. M. Waldron. "Biogeochemistry of the Ballarat East goldfield, Victoria, Australia." Journal of Geochemical Exploration 67, no. 1-3 (December 1999): 1–14. http://dx.doi.org/10.1016/s0375-6742(99)00061-8.

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McMickan, Peter J., Paul C. C. Sauter, and Kim F. Frankcombe. "Geophysical Investigations of the Kalgoorlie Goldfield, Western Australia." Exploration Geophysics 25, no. 3 (September 1994): 167. http://dx.doi.org/10.1071/eg994167a.

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38

Ride, B. M. "THE GOLDFIELDS GAS PIPELINE: 'OPENING A NEW FRONTIER'." APPEA Journal 36, no. 1 (1996): 599. http://dx.doi.org/10.1071/aj95039.

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Gas exploration and development in the northwest Pilbara in WA has increased due to the commitment of the Goldfields Gas Transmission Joint Venture to a 1,380 km gas pipeline linking the north west Pilbara to the east Pilbara iron ore region and the northern and central Goldfields. Construction of the GGT pipeline was approved in January 1995 and it is expected the pipeline will be servicing major mining operations in Newman, Mt Keith, Leinster and Kalgoorlie by August 1996. Other existing mining operations located near the pipeline are expected to convert from distillate for power station fuel to gas in 1996-97. Major new mining prospects in these highly prospective minerals provinces also offer potential for increased gas demand and GGT Pipeline throughput.The commercial arrangements for GGT Pipeline services are the first in Australia to be offered under the open access arrangements espoused by the Federal and WA Governments, and have set a benchmark for other pipelines in Australia. The innovative distance related pipeline tariff arrangements offer prospective gas shippers a simple method for evaluating use of the GGT pipeline and securing gas transmission services.The GGT Pipeline has had and will continue to have a major effect on the WA gas scene, stimulating gas exploration by capturing an established base load energy market currently dependent on liquid fuels and stimulating further WA gas demand growth.

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Davies, Peter, Jodi Turnbull, and Susan Lawrence. "Remote sensing landscapes of water management on the Victorian goldfields, Australia." Journal of Archaeological Science 76 (December 2016): 48–55. http://dx.doi.org/10.1016/j.jas.2016.10.009.

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40

Cramer, Lorinda. "Diggers’ Dress and Identity on the Victorian Goldfields, Australia, 1851‒1870." Fashion Theory 22, no. 1 (January 16, 2017): 85–108. http://dx.doi.org/10.1080/1362704x.2016.1266833.

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41

McMickan, Peter J., Paul C. C. Sauter, and Kim F. Frankcombe. "GOLD: Geophysical Investigations of the Kalgoorlie Goldfield, Western Australia." ASEG Extended Abstracts 1994, no. 1 (December 1994): 267–75. http://dx.doi.org/10.1071/asegspec07_18.

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42

Birch, William D., and Thomas A. Darragh. "George Henry Frederick Ulrich (1830–1900): pioneer mineralogist and geologist in Victoria." Proceedings of the Royal Society of Victoria 127, no. 1 (2015): 17. http://dx.doi.org/10.1071/rs15002.

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George Henry Frederick Ulrich (1830–1900) was educated at the Clausthal Mining School in Germany and arrived in Victoria in 1853. After a short period on the goldfields, he was employed on the Mining Commission and then on the Geological Survey of Victoria until its closure in 1868. In 1870 he was appointed Curator and Lecturer at the newly established Industrial and Technological Museum of Victoria. In 1878 he was appointed inaugural Director of the Otago School of Mines, New Zealand, a position he held until his death in 1900. His legacy includes detailed original maps of central Victorian goldfields, the foundation of the state’s geological collections, and among the first accounts of Victorian geology published in German periodicals, until now little known. As the only scientist of his times in Victoria with the qualifications and expertise to accurately identify and properly describe minerals, he provided the first comprehensive accounts of Victorian mineralogy, including the identification of the first new mineral in Australia, which he named maldonite. His contribution to mineralogy is recognised by the species ulrichite. Ulrich was universally respected for his scientific achievements and highly regarded for his personal qualities.

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43

Craig, Michael, Philip Withers, and S. Don Bradshaw. "Diet ofCtenotus xenopleura(Reptilia: Scincidae) in the southern Goldfields of Western Australia." Australian Zoologist 34, no. 1 (August 2007): 89–91. http://dx.doi.org/10.7882/az.2007.006.

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44

Myers, J. S. "Preface: Archaean geology of the Eastern Goldfields of Western Australia — regional overview." Precambrian Research 83, no. 1-3 (May 1997): 1–10. http://dx.doi.org/10.1016/s0301-9268(97)00002-8.

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45

Messenger, P. R. "Geochemistry of the Yandal belt metavolcanic rocks, Eastern Goldfields Province, Western Australia." Australian Journal of Earth Sciences 47, no. 6 (December 2000): 1015–28. http://dx.doi.org/10.1046/j.1440-0952.2000.00828.x.

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46

Davies, Peter, Susan Lawrence, Jodi Turnbull, Ian Rutherfurd, James Grove, Ewen Silvester, Darren Baldwin, and Mark Macklin. "Reconstruction of historical riverine sediment production on the goldfields of Victoria, Australia." Anthropocene 21 (March 2018): 1–15. http://dx.doi.org/10.1016/j.ancene.2017.11.005.

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Redman, B. A., and Reid R. Keays. "Archaean basic volcanism in the Eastern Goldfields Province, Yilgarn Block, Western Australia." Precambrian Research 30, no. 2 (September 1985): 113–52. http://dx.doi.org/10.1016/0301-9268(85)90048-8.

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Hough, M. A., F. P. Bierlein, L. Ailleres, and S. McKnight. "Nature of gold mineralisation in the Walhalla Goldfield, southeast Australia." Australian Journal of Earth Sciences 57, no. 7 (October 2010): 969–92. http://dx.doi.org/10.1080/08120099.2010.511262.

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Zhou, T., G. N. Phillips, S. Denn, and S. Burke. "Woodcutters goldfield: Gold in an Archaean granite, Kalgoorlie, Western Australia." Australian Journal of Earth Sciences 50, no. 4 (August 2003): 553–69. http://dx.doi.org/10.1046/j.1440-0952.2003.01012.x.

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DOUGHTY, PAUL, and PAUL M. OLIVER. "A new species of Underwoodisaurus (Squamata: Gekkota: Carphodactylidae) from the Pilbara region of Western Australia." Zootaxa 3010, no. 1 (August 31, 2011): 20. http://dx.doi.org/10.11646/zootaxa.3010.1.2.

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Abstract:

Ongoing surveys and systematic work focused on the Pilbara region in Western Australia have revealed the existence of numerous unrecognized species of reptiles. Here we describe Underwoodisaurus seorsus sp. nov., a new species similar to U. milii, but differing in its relatively plain dorsal and head patterns with only sparsely scattered pale tubercles, a much more gracile build, including longer snout, limbs and digits, smaller and more numerous fine scales on the dorsum, and the enlarged tubercles on the tail tending not to form transverse rows. The new species is known from few specimens and has only been encountered at mid elevations in the Hamersley Ranges, widely separated from the closest populations of U. milii in the northern Goldfields and Shark Bay in Western Australia. Given its rarity and small (potentially relictual) distribution this species may be of conservation concern.

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Journal articles on the topic 'Australian goldfields'

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