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Journal articles on the topic 'Kimberlite Australia'

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Published: 10 December 2022

Last updated: 28 January 2023

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1

Tukiainen, Tapani, and Leif Thorning. "Detection of kimberlitic rocks in West Greenland using airborne hyperspectral data: the HyperGreen 2002 project." Geological Survey of Denmark and Greenland (GEUS) Bulletin 7 (July 29, 2005): 69–72. http://dx.doi.org/10.34194/geusb.v7.4845.

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Previous investigations by the Geological Survey of Denmark and Greenland (GEUS) and exploration companies have demonstrated that some of the kimberlites in West Greenland are diamond bearing, making the region an important target for diamond prospecting. High-resolution hyperspectral (HS) remote sensing data have been successfully used for the location of kimberlitic rocks, e.g. in Australia and Africa. However, its potential as a viable method for the mapping of kimberlite occurrences in Arctic glaciated terrain with high relief was previously unknown. In July–August 2002, GEUS conducted an airborne hyperspectral survey in central West Greenland (Fig. 1) using the commercially available HyMap hyperspectral scanner operated by HyVista Corporation, Australia. Data were processed in 2003, and in 2004 follow-up field work was carried out in the Kangerlussuaq region to test possible kimberlites indicated by the HS data (Fig. 1). The project wasfinanced by the Bureau of Minerals and Petroleum, Government of Greenland.

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2

Urosevic, M., and B. J. Evans. "Surface and borehole seismic methods to delineate kimberlite pipes in Australia." Leading Edge 19, no. 7 (July 2000): 756–58. http://dx.doi.org/10.1190/1.1438712.

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3

Downes, Peter J., Dale Ferguson, and Brendan J. Griffin. "Volcanology of the Aries micaceous kimberlite, central Kimberley Basin, Western Australia." Journal of Volcanology and Geothermal Research 159, no. 1-3 (January 2007): 85–107. http://dx.doi.org/10.1016/j.jvolgeores.2006.06.004.

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4

EDWARDS, D., N. M. S. ROCK, W. R. TAYLOR, B. J. GRIFFIN, and R. R. RAMSAY. "Mineralogy and Petrology of the Aries Diamondiferous Kimberlite Pipe, Central Kimberley Block, Western Australia." Journal of Petrology 33, no. 5 (October 1, 1992): 1157–91. http://dx.doi.org/10.1093/petrology/33.5.1157.

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5

Singh, Balbir, and Matthias Cornelius. "Geochemistry and mineralogy of the regolith profile over the Aries kimberlite pipe, Western Australia." Geochemistry: Exploration, Environment, Analysis 6, no. 4 (October 24, 2006): 311–23. http://dx.doi.org/10.1144/1467-7873/06-113.

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6

McInnes, Brent I. A., Noreen J. Evans, Brad J. McDonald, Peter D. Kinny, and Janusz Jakimowicz. "Zircon U–Th–Pb–He double dating of the Merlin kimberlite field, Northern Territory, Australia." Lithos 112 (November 2009): 592–99. http://dx.doi.org/10.1016/j.lithos.2009.05.006.

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7

Griffin, W. L., and S. Y. O'Reilly. "Mantle-derived sapphirine." Mineralogical Magazine 50, no. 358 (December 1986): 635–40. http://dx.doi.org/10.1180/minmag.1986.050.358.08.

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AbstractA xenolith from the Delegate breccia pipe (New South Wales, Australia) contains sapphirine in equilibrium with aluminous clinopyroxene, garnet, and plagioclase (An48). This unusual assemblage probably developed from a clinopyroxene (±spinel ± plagioclase) cumulate during cooling from > 1400°C to c. 1000°C at pressures near 15 kbar. The sapphirine is close to the 7:9:3 composition, suggesting that bulk composition is more important than P-T conditions in determining the stoichiometry of natural sapphirines. A similar occurrence of sapphirine has also been recorded in mantlederived xenoliths from the Stockdale kimberlite in Kansas. Re-examination of sapphirine granulites from Finero suggests that their primary assemblages and origin may have been similar to those of the Delegate xenolith. Sapphirine is clearly stable under upper-mantle conditions in Ca-Al-Mg-rich bulk compositions.

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8

Kent, Ray W., Simon P. Kelley, and Malcolm S. Pringle. "Mineralogy and 40Ar/39Ar geochronology of orangeites (Group II kimberlites) from the Damodar Valley, eastern India." Mineralogical Magazine 62, no. 3 (June 1998): 313–23. http://dx.doi.org/10.1180/002646198547701.

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AbstractA suite of ultramafic-mafic alkaline igneous rocks in the Damodar Valley, eastern India, contains carbonate, phosphate and titanate minerals that are not characteristic or common in minettes or lamproites, but are typical of orangeites (Group II kimberlite) from southern Africa. Phlogopite grains from the Damodar alkaline rocks yield mean 40Ar/39Ar ages of 116.6±0.8 Ma, 113.5±0.5 Ma and 109.1±0.7 Ma (1σ errors) using laser dating techniques. These ages are similar to the Rb-Sr ages of African orangeites, which lie mostly in the range 121 to 114 Ma. Prior to this study, only one possible occurrence of orangeite (the ∼820 m.y.-old Aries pipe, Western Australia) was known outside the Kaapvaal craton and its environs. If the Damodar alkaline rocks are bona fide orangeites, it is likely that they were generated at depths of >150 km, within the stability field of diamond.

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9

Keankeo, W., W. R. Taylor, and J. D. FitzGerald. "Clinoferrosilite-bearing kelyphite: a breakdown product of xenolithic garnet, Delegate breccia pipes, New South Wales, Australia." Mineralogical Magazine 64, no. 3 (June 2000): 469–79. http://dx.doi.org/10.1180/002646100549364.

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AbstractGarnet pyroxenite xenoliths from the Delegate nephelinitic breccia pipes, New South Wales, Australia, contain relict garnets (py40 alm39 gr21) which are replaced by dark kelyphitic rims resulting from garnet breakdown. The kelyphite is composed of a lamellar intergrowth of secondary minerals, in which the lamellae are <1 μm in width. Analyses by SEM and ICPMS reveal that the kelyphite has an identical bulk chemical composition to the primary garnet. Kelyphitic rims on garnet are well known from xenoliths and xenocrysts in kimberlite pipes and from tectonically-uplifted mafic and ultramafic rocks in some metamorphic terranes. Orthopyroxene occurs in metamorphic kelyphites and it has been assumed that orthopyroxene is also the breakdown product of garnet transported in basic-ultrabasic magmas. However, TEM study of Delegate kelyphite shows that the ultrafine lamellae do not contain orthopyroxene but are instead composed of magnesian clinoferrosilite (En45Fs55), and lesser ferroan spinel and anorthite. The clinoferrosilite is probably the inversion product of initially-formed magnesian protoferrosilite. The breakdown reaction is believed to result from a sudden change to lower temperature and pressure conditions when the xenoliths were transported in the Delegate magma from ∼40 km depth to the surface.

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10

Ramsay, R. R., D. Edwards, W. R. Taylor, N. M. S. Rock, and B. J. Griffin. "Compositions of garnet and spinel from the Aries diamondiferous kimberlite pipe, central Kimberley Block, Western Australia — implications for exploration." Journal of Geochemical Exploration 51, no. 1 (April 1994): 59–78. http://dx.doi.org/10.1016/0375-6742(94)90005-1.

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11

Tappert, R., J. Foden, K. Muehlenbachs, and K. Wills. "Garnet Peridotite Xenoliths and Xenocrysts from the Monk Hill Kimberlite, South Australia: Insights into the Lithospheric Mantle beneath the Adelaide Fold Belt." Journal of Petrology 52, no. 10 (August 12, 2011): 1965–86. http://dx.doi.org/10.1093/petrology/egr036.

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12

R. H. M. "J. E. Glover & P. G. Harris (eds) 1985. Kimberlite Occurrence and Origin: A Basis for Conceptual Models in Exploration. Revised edition; a summary of presented papers, i + 298 pp. Geology Publication no. 8. Nedlands, Australia: University of Australia Extension. Price A$ 19.00 (Western Australia). A$22 (other Australia), A$26 (overseas). Paperback." Geological Magazine 123, no. 3 (May 1986): 318–19. http://dx.doi.org/10.1017/s0016756800034841.

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13

Downes, Peter J., Brendan J. Griffin, and William L. Griffin. "Mineral chemistry and U-Pb SHRIMP geochronology of xenoliths and xenocrysts from the Aries micaceous kimberlite: Constraints on the composition and age of the central Kimberley Craton, Western Australia." ASEG Extended Abstracts 2006, no. 1 (December 2006): 1–9. http://dx.doi.org/10.1071/aseg2006ab036.

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14

DOWNES, PETER J., JO-ANNE WARTHO, and BRENDAN J. GRIFFIN. "Magmatic Evolution and Ascent History of the Aries Micaceous Kimberlite, Central Kimberley Basin, Western Australia: Evidence from Zoned Phlogopite Phenocrysts, and UV Laser 40Ar/39Ar Analysis of Phlogopite–Biotite." Journal of Petrology 47, no. 9 (June 2, 2006): 1751–83. http://dx.doi.org/10.1093/petrology/egl026.

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15

Menzies, M. "J. E. Glover, and P. G. Harris, eds. Kimberlite Occurrence and Origin: A Basis for Conceptual Models in Exploration. Geology Department and University Extension, the University of Western Australia Perth, 1984. 298 pp. Price (post free) $ (Australian) 26." Mineralogical Magazine 50, no. 357 (September 1986): 544. http://dx.doi.org/10.1180/minmag.1986.050.357.23.

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16

Downes, Peter J., Brendan J. Griffin, and William L. Griffin. "Mineral chemistry and zircon geochronology of xenocrysts and altered mantle and crustal xenoliths from the Aries micaceous kimberlite: Constraints on the composition and age of the central Kimberley Craton, Western Australia." Lithos 93, no. 1-2 (January 2007): 175–98. http://dx.doi.org/10.1016/j.lithos.2006.06.005.

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17

Tappert, Ralf, John Foden, Larry Heaman, Michelle C. Tappert, Shannon E. Zurevinski, and Kevin Wills. "The petrology of kimberlites from South Australia: Linking olivine macrocrystic and micaceous kimberlites." Journal of Volcanology and Geothermal Research 373 (March 2019): 68–96. http://dx.doi.org/10.1016/j.jvolgeores.2019.01.022.

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18

Hamilton, Jessica L., Siobhan A. Wilson, Bree Morgan, Anna L. Harrison, Connor C. Turvey, David J. Paterson, Gregory M. Dipple, and Gordon Southam. "Accelerating Mineral Carbonation in Ultramafic Mine Tailings via Direct CO2 Reaction and Heap Leaching with Potential for Base Metal Enrichment and Recovery." Economic Geology 115, no. 2 (March 1, 2020): 303–23. http://dx.doi.org/10.5382/econgeo.4710.

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Abstract Accelerated carbonation of ultramafic mine tailings has the potential to offset CO2 emissions produced by mining ores from Cu-Ni-platinum group element, podiform chromite, diamondiferous kimberlite, and historical chrysotile deposits. Treatments such as acid leaching, reaction of tailings with elevated concentrations of gaseous CO2, and optimization of tailings pore water saturation have been shown to enhance CO2 sequestration rates in laboratory settings. The next challenge is to deploy treatment technologies on the pilot and field scale while minimizing cost, energy input, and adverse environmental impacts. Implementation of accelerated tailings carbonation at field scale will ideally make use of in situ treatments or modified ore-processing routes that employ conventional technology and expertise and operate at close to ambient temperatures and pressures. Here, we describe column experiments designed to trial two geochemical treatments that address these criteria: (1) direct reaction of partially saturated ultramafic tailings with synthetic flue gas from power generation (10% CO2 in N2) and (2) repeated heap leaching of ultramafic tailings with dilute sulfuric acid. In the first experiment, we report rapid carbonation of brucite [Mg(OH)2] in the presence of 10% CO2 gas within tailings sampled from the Woodsreef chrysotile mine, New South Wales, Australia. Within four weeks, we observe a doubling of the amount of CO2 stored within minerals relative to what is achieved after three decades of passive mineral carbonation via air capture in the field. Our simulated heap leaching experiments, treated daily with 0.08 M H2SO4, produce high-Mg leachates that have the potential to sequester 21.2 kg CO2 m–2 y–1, which is approximately one to two orders of magnitude higher than the rate of passive carbonation of the Woodsreef mine tailings. Although some nesquehonite (MgCO3 · 3H2O) forms from these leachates, most of the Mg is precipitated as Mg sulfate minerals instead. Therefore, an acid other than H2SO4 could be used; otherwise, sulfate removal would be required to maximize CO2 sequestration potential from acid heap leaching treatments. Reactive transport modeling (MIN3P) is employed to simulate acid leaching experiments and predict the effects of heap leaching for up to five years. Finally, our synchrotron X-ray fluorescence microscopy results for leached tailings material reveal that valuable trace metals (Fe, Ni, Mn, Co, Cr) become highly concentrated within secondary Fe (hydr)oxide minerals at the pH neutralization horizon within our column experiments. This discrete horizon migrates downward, and our reactive transport models indicate it will become increasingly enriched in first-row transition metals in response to continued acid leaching. Acid-leaching treatments for accelerated mineral carbonation could therefore be useful for ore processing and recovery of base metals from tailings, waste rock, or low-grade ores.

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19

Smith, Robert J. "Geophysics in Australian mineral exploration." GEOPHYSICS 50, no. 12 (December 1985): 2637–65. http://dx.doi.org/10.1190/1.1441888.

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I review a variety of recent case histories illustrating the application of geophysics in mineral exploration in Australia. Geophysics is now an integral part of most programs. Examples are given of contributions by geophysics to all stages of mineral exploration, from regional area selection through to mine planning and development. Specific case histories summarized are as follows: (a) Olympic Dam copper‐uranium‐gold deposit, discovered using a conceptual genetic model and regional geophysical data; (b) Ellendale diamondiferous kimberlites, illustrating the use of low level, detailed airborne magnetics; (c) Ranger uranium orebodies, discovered by detailed airborne radiometric surveys; (d) geologic mapping near Mary Kathleen with color displays of airborne radiometric data; (e) mapping of lignite in basement depressions of the Bremer Basin, near Esperance, with INPUT; (f) White Leads, a lead‐zinc sulfide deposit discovered with induced polarization (IP) and TEM, near Broken Hill; (g) Hellyer, a lead‐zinc‐silver‐gold deposit discovered with UTEM; (h) application of geophysical logging near Kanmantoo; (i) Cowla Peak, a subbituminous steaming coal deposit mapped with ground TEM; and (j) Cook Colliery, where high‐resolution seismic reflection methods have successfully increased the workable reserves.

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20

Davies, R. M., S. Y. O'Reilly, and W. L. Griffin. "Diamonds from Wellington, NSW: insights into the origin of eastern Australian diamonds." Mineralogical Magazine 63, no. 4 (August 1999): 447–71. http://dx.doi.org/10.1180/002646199548619.

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AbstractDiamonds from alluvial deposits near Wellington, New South Wales, have been characterized on the basis of morphological features, mineral inclusions, C isotope signatures, N content and aggregation state and internal structure. The diamonds are of two types. The larger group (Group A) is indistinguishable from diamonds found worldwide from kimberlitic and lamproitic host rocks. This group is inferred to have formed in a peridotitic mantle source in Pre-Cambrian subcratonic lithosphere. The second group (Group B) is unique in its internal structures (which show evidence of growth in a stress field and non-planar facets), has unusually heavy C isotopic compositions and contains Ca-rich eclogitic inclusions. This group is inferred to have formed in a subducting slab. Diamonds of both groups have external features (corrosion structures and polish) indicating transport to the surface by lamproitic-like magmas. The diamonds show evidence of long residence at the earth's surface and significant alluvial reworking: they are not accompanied by typical diamond indicator minerals.

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21

Chen, Y. D., Suzanne Y. O'Reilly, P. D. Kinny, and W. L. Griffin. "Dating lower crust and upper mantle events: an ion microprobe study of xenoliths from kimberlitic pipes, South Australia." Lithos 32, no. 1-2 (March 1994): 77–94. http://dx.doi.org/10.1016/0024-4937(94)90022-1.

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22

O'Reilly, Suzanne Y., D. Chen, W. L. Griffin, and C. G. Ryan. "Minor elements in olivine from spinel lherzolite xenoliths: implications for thermobarometry." Mineralogical Magazine 61, no. 405 (April 1997): 257–69. http://dx.doi.org/10.1180/minmag.1997.061.405.09.

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AbstractThe proton microprobe has been used to determine contents of Ca, Ti, Ni, Mn and Zn in the olivine of 54 spinel lherzolite xenoliths from Australian and Chinese basalts. These data are compared with proton-probe data for Ni, Mn and Zn in the olivine of 180 garnet peridotite xenoliths from African and Siberian kimberlites. Fe, Mn, Ni and Zn contents are well-correlated; because the spinel lherzolite olivines have higher mean Fe contents than garnet peridotite olivines (average Fo89.6vs. Fo90–92) they also have lower Ni and higher Mn contents. Zn and Fe are well-correlated in garnet peridotite olivine, but in spinel peridotites this relationship is perturbed by partitioning of Zn into spinel. None of these elements shows significant correlation with temperature. Consistent differences in trace-element contents of olivines in the two suites is interpreted as reflecting the greater degree of depletion of Archean garnet peridotites as compared to Phanerozoic spinel lherzolites. Ca and Ti contents of spinel-peridotite olivine are well correlated with one another, and with temperature as determined by several types of geothermometer. However, Ca contents are poorly correlated with pressure as determined by the Ca-in-olivine barometer of Köhler and Brey (1990). This reflects the strong T-dependence of this barometer: the uncertainty in pressure (calculated by this method) which is produced by the ±50°C uncertainty expected of any geothermometer is ca ± 8 kbar, corresponding to the entire width of the spinel-lherzolite field at 900–1200°C.

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23

Breen, Sally, and Jay Daniel Thompson. "Live through This." M/C Journal 21, no. 5 (December 6, 2018). http://dx.doi.org/10.5204/mcj.1490.

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If you live through this with me, I swear that I would die for you— Hole, “Asking for It” (1994)The 1990s was a curious decade – post-1980s excess and the Black Monday correction, we limped into the last decade of the 20th century with a whimper, not a bang. The baby boomers were in ascendency, shaking off the detritus of a century of extremes behind closed doors.It’s easy now to think that the disaffection manifesting in Generation X and in particular in the grunge music scene was a put on, an act. But in most big game cultures the emerging generation was caught between old school regimes that refused to recognise very obvious failures and what appeared to be distant, no access futures. This point has been compellingly made by Mark Davis, the author of one of the essays in this 'nineties' issue of M/C Journal.The editors of this issue came of age in 1990s Australia. Or, to paraphrase grunge act Hole, we lived through this. And what a time to be alive! How appropriate to revisit the twentieth century’s swansong as the second decade of the twenty-first century nears its own denouement.When we sat down to work on this issue, one clear question arose: How to explain this 1990s nostalgia? Commentators have proffered a slew of explanations. These have ranged from the “20 year cycles” for nostalgia in popular culture (Tucker) to a desire for an apparently simpler, more trouble-free and, well, less connected time. As Atkinson wryly observes: “While we had the internet in the grunge era, it didn't necessarily dominate your life at that point. Your existence was probably a bunch more focused on IRL than URLs.”Some contributors invoke 1990s nostalgia. Paul Stafford provides a reverential and autoethnographic account of his experiences as a fan of grunge music during that genre’s early 1990s heyday. Renee Middlemost describes the excoriating response from fans to The Simpsons’ episode “That 90s Show”. Middlemost’s essay reminds us of the program’s brilliance prior to “jumping the shark” in the 2000s.Yes, the 1990s hosted transgressive, test of time-standing examples of popular culture. This includes the ‘grunge’ music genre that arose in the US circa the early 1990s, in the work of bands such as Hole, Nirvana, Pearl Jam and Soundgarden (see Stafford’s essay). Grunge music and its associated sub-cultural markers went on to flourish globally in countries such as Poland, as Marek Jezinski and Lukasz Wojtkowski describe in their contribution.The 1990s also saw lesser known, but no less significant, pop cultural phenomena. Julian Novitz revisits the Doctor Who novels published between 1991 and 1997. These novels are particularly significant given that the 1990s have commonly been regarded as the “wilderness years” for that franchise.The 1990s saw an increased feminist visibility in popular culture. This visibility is suggested in Jessica Ford’s essay on Roseanne/Roseanne Barr’s feminism, Claire Knowles’s reading of Agent Scully (of X Files fame) as feminist icon, and Justine Ettler’s reflection on her meeting with US “post-punk-feminist” Kathy Acker. Ettler is the author of the breakout Australian novel The River Ophelia (1995), which was influenced by Acker’s oeuvre, and of which Acker was evidently a fan.Yet, 1990s feminisms had their limitations. They lacked, for example, the focus of intersectionality that was conceptualised by African-American legal scholar Kimberle Crenshaw during the late 1980s, and that is only now (in the 21st century) really starting to take shape, albeit not without a struggle. Ford makes this point when analysing the “whiteness” of Roseanne/Roseanne’s gender politics in the 90s and 2018.In other areas, too, the 90s were not “all good”. There was no such thing as regional arts development funds. There was no reconciliation or Beyond Blue. No #MeToo or #TimesUp. No kombucha or viral campaigns or shops open after five. No royal commissions into child abuse. Australia was yet to have a female prime minister or governor general. Mentioning global warming meant you were a crackpot. Gender reassignment was something your nanna and your neighbour had never heard about.Put simply, then, the 1990s cannot be described in entirely affirmative or negative terms. The 1990s (as with any decade, really) is too complex for such summations.In some ways the 1990s was about what was started (internet insurgence), what was set on fire (Die Yuppy Die), and what came after the ashes drifted. Many of our writers have taken this comparative view, exploring the then(s) and now(s) and the enormous gaps between that don’t just register in years. Mark Davis, for example, argues the Alt Right is far more nightmarish in the new millennium than even he could have imagined.Some contributors have explored the merger of old and new, past and future in creative and idiosyncratic ways. Chris Campanioni theorises “the cover and the glitch, two performative and technological enactments that fomented the collapse between author-reader and user-machine.” Campanioni’s exploration focuses, in particular, on the Y2K bug and David Lynch’s cult series Twin Peaks (1990-91), and the much hyped reboot in 2017.In his feature essay contribution, Mitch Goodwin reminds us that 1999 — and its anticipation of technological dystopia (Y2K anxieties ahoy!) — “could not have happened” without 1995. Goodwin teases out this point via readings of two futuristic thrillers Johnny Mnemonic and Strange Days.As Goodwin puts it:It might seem strange now but tapping into the contents of Keanu Reeve’s brain was a utopian data moment in 1995. This was still the digital frontier when the network was as yet not fully colonised by corporate America. The Lo-Teks effectively delivering a global moment of healing via satellite. These were the dreams we had in the nineties.While no single collection could hope to encapsulate the complexity of the period spanning 1990 to 1999. The contributors to the ‘Nineties’ issue of M/C Journal have given this one helluva go.References Bernstein, Sara. “Why Gen X Isn’t Psyched for the ‘90s Revival.” Vox. 13 Mar. 2018. <https://www.vox.com/2018/3/13/17064842/gen-x-90s-revival>.Crenshaw, Kimberle. “Demarginalizing the Intersection of Race and Sex: A Black Feminist Critique of Antidiscrimination Doctrine, Feminist Theory and Antiracist Politics.” University of Chicago Legal Forum 1 (1989): 139-167.Davis, Mark. Gangland: Cultural Elites and the New Generationalism. St Leonards, NSW: Allen & Unwin, 1997.Hole. “Asking for It.” Live through This. Georgia, US: City Slang, 1994.

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