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Journal articles on the topic 'Geochemistry – Western Australia – Eastern Goldfields'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

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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2

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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3

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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4

Krapež, Bryan, Mark E. Barley, and Stuart J. A. Brown. "Late Archaean synorogenic basins of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia." Precambrian Research 161, no. 1-2 (February 2008): 135–53. http://dx.doi.org/10.1016/j.precamres.2007.06.016.

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5

Krapež, Bryan, Jon G. Standing, Stuart J. A. Brown, and Mark E. Barley. "Late Archaean synorogenic basins of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia." Precambrian Research 161, no. 1-2 (February 2008): 154–82. http://dx.doi.org/10.1016/j.precamres.2007.06.017.

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6

Krapež, Bryan, and Mark E. Barley. "Late Archaean synorogenic basins of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia." Precambrian Research 161, no. 1-2 (February 2008): 183–99. http://dx.doi.org/10.1016/j.precamres.2007.06.020.

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7

Holzschuh, Josef. "Low‐cost geophysical investigations of a paleochannel aquifer in the Eastern Goldfields, Western Australia." GEOPHYSICS 67, no. 3 (May 2002): 690–700. http://dx.doi.org/10.1190/1.1484512.

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Compressional (P) wave and shear (S) wave seismic reflection techniques were used to delineate the sand and gravel aquifer within a highly saline clay‐filled paleochannel in the Eastern Goldfields of Western Australia. The seismic refraction and gravity methods were also used to investigate the paleochannel. The unsaturated loose fine‐grained sand up to 10 m in depth at the surface is a major factor in degrading subsurface imaging. The seismic processing needed to be precise, with accurate static corrections and normal moveout corrections. Deconvolution enhanced the aquifer and other paleochannel reflectors. P‐wave reflection and refraction layer depths had good correlation and showed a total of six boundaries: (1) water table, (2) change in velocity (compaction) in the paleochannel sediments, (3) sand and gravel aquifer, (4) red‐brown saprolite and green saprolite boundary, (5) weathered bedrock, and (6) unweathered bedrock. P‐wave explosive and hammer sources were found to have similar signal characteristics, and the aquifer and bedrock were both imaged using the hammer source. The deep shots below the water table have the most broadband frequency response for reflections, but stacking clear reflections was difficult. The S‐wave reflection results showed high lateral and vertical resolution of the basal saprolite clay, the sand and gravel aquifer, and very shallow clays above the aquifer. The S‐wave reflection stacking velocities were 10–20% of the P‐waves, increasing the resolution of the S‐wave section. The gravity data were modelled to fit the known drilling and P‐wave seismic reflection depths. The refraction results did not identify the top of bedrock, so refraction depths were not used for the gravity modeling in this highly weathered environment. The final gravity model mapped the bedrock topography beyond the lateral extent of the seismic and drilling data.

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8

Brown, Suzanne M., David I. Groves, and Philip G. Newton. "Geological setting and mineralization model for the Cleo gold deposit, Eastern Goldfields Province, Western Australia." Mineralium Deposita 37, no. 8 (March 5, 2002): 704–21. http://dx.doi.org/10.1007/s00126-002-0255-x.

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9

Morris, P. A., and W. K. Witt. "Geochemistry and tectonic setting of two contrasting Archaean felsic volcanic associations in the Eastern Goldfields, Western Australia." Precambrian Research 83, no. 1-3 (May 1997): 83–107. http://dx.doi.org/10.1016/s0301-9268(97)00006-5.

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10

Krapež, Bryan, and April L. Pickard. "Detrital-zircon age-spectra for Late Archaean synorogenic basins of the Eastern Goldfields Superterrane, Western Australia." Precambrian Research 178, no. 1-4 (April 2010): 91–118. http://dx.doi.org/10.1016/j.precamres.2010.01.014.

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11

Scott, K. M., and R. W. Howard. "Hydrothermal alteration and geochemical dispersion in the regolith at Panglo, Eastern Goldfields, Western Australia." Geochemistry: Exploration, Environment, Analysis 1, no. 4 (November 2001): 313–22. http://dx.doi.org/10.1144/geochem.1.4.313.

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12

Barley, Mark E., Stuart J. A. Brown, Bryan Krapež, and Natalie Kositcin. "Physical volcanology and geochemistry of a Late Archaean volcanic arc: Kurnalpi and Gindalbie Terranes, Eastern Goldfields Superterrane, Western Australia." Precambrian Research 161, no. 1-2 (February 2008): 53–76. http://dx.doi.org/10.1016/j.precamres.2007.06.019.

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13

Brown, S. J. A., M. E. Barley, B. Krapež, and R. A. F. Cas. "The Late Archaean Melita Complex, Eastern Goldfields, Western Australia: shallow submarine bimodal volcanism in a rifted arc environment." Journal of Volcanology and Geothermal Research 115, no. 3-4 (June 2002): 303–27. http://dx.doi.org/10.1016/s0377-0273(01)00314-6.

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14

Blewett, Richard S., Kevin F. Cassidy, David C. Champion, Paul A. Henson, Bruce S. Goleby, Leonie Jones, and P. Bruce Groenewald. "The Wangkathaa Orogeny: an example of episodic regional ‘D2’ in the late Archaean Eastern Goldfields Province, Western Australia." Precambrian Research 130, no. 1-4 (April 2004): 139–59. http://dx.doi.org/10.1016/j.precamres.2003.11.001.

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15

Hodkiewicz, P. F., D. I. Groves, G. J. Davidson, R. F. Weinberg, and S. G. Hagemann. "Influence of structural setting on sulphur isotopes in Archean orogenic gold deposits, Eastern Goldfields Province, Yilgarn, Western Australia." Mineralium Deposita 44, no. 2 (October 14, 2008): 129–50. http://dx.doi.org/10.1007/s00126-008-0211-5.

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16

Jones, Sarah, David Doutch, and Tim Lutter. "The Invincible deposit: Early gold mineralisation truncated by unaltered c. 2665 Ma conglomerate, St Ives, Eastern Goldfields, Western Australia." Ore Geology Reviews 109 (June 2019): 303–21. http://dx.doi.org/10.1016/j.oregeorev.2019.04.016.

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17

Sung, Y. H., J. Brugger, C. L. Ciobanu, A. Pring, W. Skinner, L. V. Danyushevsky, and M. Nugus. "Invisible gold in arsenian pyrite and arsenopyrite from a multistage Archaean gold deposit: Sunrise Dam, Eastern Goldfields Province, Western Australia." Mineralium Deposita 44, no. 7 (July 16, 2009): 793. http://dx.doi.org/10.1007/s00126-009-0251-5.

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18

Witt, W. K., and R. Davy. "Geology and geochemistry of Archaean granites in the Kalgoorlie region of the Eastern Goldfields, Western Australia: a syn-collisional tectonic setting?" Precambrian Research 83, no. 1-3 (May 1997): 133–83. http://dx.doi.org/10.1016/s0301-9268(97)00008-9.

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19

Steadman, Jeffrey A., Ross R. Large, Sebastien Meffre, and Stuart W. Bull. "Age, origin and significance of nodular sulfides in 2680Ma carbonaceous black shale of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia." Precambrian Research 230 (June 2013): 227–47. http://dx.doi.org/10.1016/j.precamres.2013.02.013.

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20

Trofimovs, J., B. K. Davis, and R. A. F. Cas. "Contemporaneous ultramafic and felsic intrusive and extrusive magmatism in the Archaean Boorara Domain, Eastern Goldfields Superterrane, Western Australia, and its implications." Precambrian Research 131, no. 3-4 (June 2004): 283–304. http://dx.doi.org/10.1016/j.precamres.2003.12.012.

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21

Holzschuh, Josepf. "To “Low‐cost geophysical investigations of a paleochannel aquifer in the Eastern Goldfields, Western Australia” (Josef Holzschuh, GEOPHYSICS, 67, 690–700)." GEOPHYSICS 68, no. 1 (January 2003): 409. http://dx.doi.org/10.1190/1.1552008.

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22

Morris, Paul A., and Andrew J. Sanders. "The effect of sample medium on regolith chemistry over greenstone belts in the northern Eastern Goldfields of Western Australia." Geochemistry: Exploration, Environment, Analysis 1, no. 3 (August 2001): 201–10. http://dx.doi.org/10.1144/geochem.1.3.201.

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23

Blewett, R. S., R. Squire, J. M. Miller, P. A. Henson, and D. C. Champion. "Architecture and geodynamic evolution of the St Ives Goldfield, eastern Yilgarn Craton, Western Australia." Precambrian Research 183, no. 2 (November 2010): 275–91. http://dx.doi.org/10.1016/j.precamres.2010.07.017.

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24

Krapež, Bryan, and Jason L. Hand. "Late Archaean deep-marine volcaniclastic sedimentation in an arc-related basin: The Kalgoorlie Sequence of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia." Precambrian Research 161, no. 1-2 (February 2008): 89–113. http://dx.doi.org/10.1016/j.precamres.2007.06.014.

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25

Morey, Anthony A., Roberto F. Weinberg, and Frank P. Bierlein. "The structural controls of gold mineralisation within the Bardoc Tectonic Zone, Eastern Goldfields Province, Western Australia: implications for gold endowment in shear systems." Mineralium Deposita 42, no. 6 (March 1, 2007): 583–600. http://dx.doi.org/10.1007/s00126-007-0125-7.

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26

Kuhn, Stephen, Matthew J. Cracknell, and Anya M. Reading. "Lithologic mapping using Random Forests applied to geophysical and remote-sensing data: A demonstration study from the Eastern Goldfields of Australia." GEOPHYSICS 83, no. 4 (July 1, 2018): B183—B193. http://dx.doi.org/10.1190/geo2017-0590.1.

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The Eastern Goldfields of Western Australia is one of the world’s premier gold-producing regions; however, large areas of prospective bedrock are under cover and lack detailed lithologic mapping. Away from the near-mine environment, exploration for new gold prospects requires mapping geology using the limited data available with robust estimates of uncertainty. We used the machine learning algorithm Random Forests (RF) to classify the lithology of an underexplored area adjacent to the historically significant Junction gold mine, using geophysical and remote-sensing data, with no geochemical sampling available at this reconnaissance stage. Using a sparse training sample, 1.6% of the total ground area, we produce a refined lithologic map. The classification is stable, despite including parts of the study area with later intrusions and variable cover depth, and it preserves the stratigraphic units defined in the training data. We assess the uncertainty associated with this new RF classification using information entropy, identifying those areas of the refined map that are most likely to be incorrectly classified. We find that information entropy correlates well with inaccuracy, providing a mechanism for explorers to direct future expenditure toward areas most likely to be incorrectly mapped or geologically complex. We conclude that the method can be an effective additional tool available to geoscientists in a greenfield, orogenic gold setting when confronted with limited data. We determine that the method could be used either to substantially improve an existing map, or produce a new map, taking sparse observations as a starting point. It can be implemented in similar situations (with limited outcrop information and no geochemical data) as an objective, data-driven alternative to conventional interpretation with the additional value of quantifying uncertainty.

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27

Dominy, S. C., and S. P. Hunt. "Evaluation of gold deposits—Part 2: results of a survey of estimation methodologies applied in the Eastern Goldfields of Western Australia." Applied Earth Science 110, no. 3 (December 2001): 167–75. http://dx.doi.org/10.1179/aes.2001.110.3.167.

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28

Barnes, S. J., C. M. Lesher, and R. A. Sproule. "Geochemistry of komatiites in the Eastern Goldfields Superterrane, Western Australia and the Abitibi Greenstone Belt, Canada, and implications for the distribution of associated Ni–Cu–PGE deposits." Applied Earth Science 116, no. 4 (December 2007): 167–87. http://dx.doi.org/10.1179/174327507x271996.

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29

Rasmussen, Birger, Andreas G. Mueller, and Ian R. Fletcher. "Zirconolite and xenotime U–Pb age constraints on the emplacement of the Golden Mile Dolerite sill and gold mineralization at the Mt Charlotte mine, Eastern Goldfields Province, Yilgarn Craton, Western Australia." Contributions to Mineralogy and Petrology 157, no. 5 (November 6, 2008): 559–72. http://dx.doi.org/10.1007/s00410-008-0352-7.

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30

Ross, A. A., M. E. Barley, S. J. A. Brown, N. J. McNaughton, J. R. Ridley, and I. R. Fletcher. "Young porphyries, old zircons: new constraints on the timing of deformation and gold mineralisation in the Eastern Goldfields from SHRIMP U–Pb zircon dating at the Kanowna Belle Gold Mine, Western Australia." Precambrian Research 128, no. 1-2 (January 2004): 105–42. http://dx.doi.org/10.1016/j.precamres.2003.08.013.

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31

Drummond, Barry J., Bruce R. Goleby, A. J. Owen, A. N. Yeates, C. Swager, Y. Zhang, and J. K. Jackson. "Seismic reflection imaging of mineral systems: Three case histories." GEOPHYSICS 65, no. 6 (November 2000): 1852–61. http://dx.doi.org/10.1190/1.1444869.

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Mineral deposits can be described in terms of their mineral systems, i.e., fluid source, migration pathway, and trap. Source regions are difficult to recognize in seismic images. Many orebodies lie on or adjacent to major fault systems, suggesting that the faults acted as fluid migration pathways through the crust. Large faults often have broad internal zones of deformation fabric, which is anisotropic. This, coupled with the metasomatic effects of fluids moving along faults while they are active, can make the faults seismically reflective. For example, major gold deposits in the Archaean Eastern Goldfields province of Western Australia lie in the hanging‐wall block of regional‐scale faults that differ from other nearby faults by being highly reflective and penetrating to greater depths in the lower crust. Coupled thermal, mechanical, and fluid‐flow modeling supports the theory that these faults were fluid migration pathways from the lower to the upper crust. Strong reflections are also recorded from two deeply penetrating faults in the Proterozoic Mt. Isa province in northeastern Australia. Both are closely related spatially to copper and copper‐gold deposits. One, the Adelheid fault, is also adjacent to the large Mt. Isa silver‐lead‐zinc deposit. In contrast, other deeply penetrating faults that are not intrinsically reflective but are mapped in the seismic section on the basis of truncating reflections have no known mineralization. Regional seismic profiles can therefore be applied in the precompetitive area selection stage of exploration. Applying seismic techniques at the orebody scale can be difficult. Orebodies often have complex shapes and reflecting surfaces that are small compared to the diameter of the Fresnel zone for practical seismic frequencies. However, if the structures and alteration haloes around the orebodies themselves, seismic techniques may be more successful. Strong bedding‐parallel reflections were observed from the region of alteration around the Mt. Isa silver‐lead‐zinc orebodies using high‐resolution profiling. In addition, a profile in Tasmania imaged an internally nonreflective bulge within the Que Hellyer volcanics, suggesting a good location to explore for a volcanic hosted massive sulfide deposit. These case studies provide a pointer to how seismic techniques could be applied during mineral exploration, especially at depths greater than those being explored with other techniques.

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32

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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33

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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34

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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35

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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36

Howard, David. "Geological Survey of Western Australia: Data released from Eastern Goldfields 2019 seismic survey." Preview 2019, no. 202 (September 3, 2019): 18. http://dx.doi.org/10.1080/14432471.2019.1669282.

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37

Fox, J. E. D., J. R. Neilsen, and J. M. Osborne. "Eucalyptus seedling growth and salt tolerance from the north-eastern goldfields of Western Australia." Journal of Arid Environments 19, no. 1 (July 1990): 45–53. http://dx.doi.org/10.1016/s0140-1963(18)30828-0.

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38

Swager, C. P. "Tectono-stratigraphy of late Archaean greenstone terranes in the southern Eastern Goldfields, Western Australia." Precambrian Research 83, no. 1-3 (May 1997): 11–42. http://dx.doi.org/10.1016/s0301-9268(97)00003-x.

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39

Wyche, Stephen, Marco L. Fiorentini, John L. Miller, and T. Campbell McCuaig. "Geology and controls on mineralisation in the Eastern Goldfields region, Yilgarn Craton, Western Australia." Episodes 35, no. 1 (March 1, 2012): 273–82. http://dx.doi.org/10.18814/epiiugs/2012/v35i1/027.

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40

McIntyre, J. R., and J. E. Martyn. "Early extension in the Late Archaean northeastern Eastern Goldfields Province, Yilgarn Craton, Western Australia." Australian Journal of Earth Sciences 52, no. 6 (December 2005): 975–92. http://dx.doi.org/10.1080/08120090500302319.

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41

Fergusson, B., and AJ Graham. "A Quantitative Study of Soil-Plant Relations in the Eastern Goldfields of Western Australia." Rangeland Journal 20, no. 1 (1998): 119. http://dx.doi.org/10.1071/rj9980119.

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The soil and plants at a 27.4 ha field site near Kalgoorlie, Western Australia, were surveyed and analysed with multivariate statistics. Cluster analysis identified four distinct plant communities at the study site. These were: Acacia acuminata shrubland Eucalyptus gvfithsii woodland Eucalyptus salrnonophloia woodland 'Ground Covers' - areas characterised by the presence of generalist herbs, low shrubs and weeds, and the absence of dominant upper storey species. Discriminant function analysis identified site elevation and soil exchangeable Ca as the primary environmental discriminants between the plant communities. Using these two variables, sample points were classified into one of the four plant communities. The two methods of classification matched well, with classification based on the two environmental variables providing an indication of which plant community would be most likely to establish in disturbed areas. This type of information can be important to revegetation programs in the region, guiding the use of appropriate plant species under different rehabilitation conditions. Key wcrds: environmental variables, plant communities, multivariate analysis, classification, revegetation

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42

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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43

Cohalan, Louis, Roberto F. Weinberg, Rick J. Squire, and Charlotte M. Allen. "Early deformation in the Eastern Goldfields, Yilgarn Craton, Western Australia: A record of early thrusting?" Precambrian Research 266 (September 2015): 212–26. http://dx.doi.org/10.1016/j.precamres.2015.05.013.

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44

Witt, W. K., D. R. Mason, and D. P. Hammond. "Archean Karari gold deposit, Eastern Goldfields Province, Western Australia: a monzonite-associated disseminated gold deposit." Australian Journal of Earth Sciences 56, no. 8 (December 2009): 1061–86. http://dx.doi.org/10.1080/08120090903246188.

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45

Watson, David S., and Michele Clapin. "Ear health of Aboriginal primary school children in the Eastern Goldfields Region of Western Australia." Australian Journal of Public Health 16, no. 1 (February 12, 2010): 26–30. http://dx.doi.org/10.1111/j.1753-6405.1992.tb00020.x.

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46

Williams, P. R., and A. J. Whitaker. "Gneiss domes and extensional deformation in the highly mineralised Archaean Eastern Goldfields Province, Western Australia." Ore Geology Reviews 8, no. 1-2 (April 1993): 141–62. http://dx.doi.org/10.1016/0169-1368(93)90032-t.

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47

Swager, Cees, and Timothy J. Griffin. "An early thrust duplex in the Kalgoorlie-Kambalda greenstone belt, Eastern Goldfields Province, Western Australia." Precambrian Research 48, no. 1-2 (August 1990): 63–73. http://dx.doi.org/10.1016/0301-9268(90)90057-w.

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48

Williams, P. R., B. W. Nisbet, and M. A. Etheridge. "Shear zones, gold mineralization and structural history in the Leonora district, Eastern Goldfields Province, Western Australia." Australian Journal of Earth Sciences 36, no. 3 (September 1989): 383–403. http://dx.doi.org/10.1080/08120098908729496.

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49

Drummond, B. J., and B. R. Goleby. "Seismic Reflection Images of the Major Ore-Controlling Structures in the Eastern Goldfields Province, Western Australia." Exploration Geophysics 24, no. 3-4 (September 1993): 473–78. http://dx.doi.org/10.1071/eg993473.

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50

Trench, A., J. A. Withers, M. House, B. Goleby, D. R. Miller, and B. J. Drummond. "On the Gravity Signature of Archaean Greenstones in the Widgiemooltha-Tramways Area, Eastern Goldfields, Western Australia." Exploration Geophysics 24, no. 3-4 (September 1993): 811–18. http://dx.doi.org/10.1071/eg993811.

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