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Journal articles on the topic 'Broken Hill'

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Author: Grafiati

Published: 4 June 2021

Last updated: 20 February 2023

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1

Yellowlees, Peter, and Anil Kaushik. "The Broken Hill Psychopathology Project." Australian and New Zealand Journal of Psychiatry 26, no. 2 (June 1, 1992): 197–207. http://dx.doi.org/10.3109/00048679209072028.

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2

Nutman, A. P., and K. Ehlers. "Archaean crust near Broken Hill?" Australian Journal of Earth Sciences 45, no. 5 (October 1998): 687–94. http://dx.doi.org/10.1080/08120099808728426.

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3

Salter, Hayley, Leanne Zammit, Tracy Horsburgh, and Lisa Drysdale. "BHP — A Broken Hill Perspective." Health Information Management 29, no. 4 (December 2000): 189–91. http://dx.doi.org/10.1177/183335830002900417.

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4

GUTHRIE, D. I. "Letter from Broken Hill Hospital." Australian Occupational Therapy Journal 17, no. 3 (August 27, 2010): 45. http://dx.doi.org/10.1111/j.1440-1630.1970.tb00414.x.

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5

Yellowlees, Peter M., and Anil V. Kaushik. "The Broken Hill Psychopathology Project." Australian & New Zealand Journal of Psychiatry 26, no. 2 (June 1992): 197–207. http://dx.doi.org/10.1177/000486749202600203.

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The main objective of this study was to describe the psychiatric disorders seen in patients presenting for treatment in rural New South Wales. The patients were seen primarily in the community, in both public and private practice, but also in the local base hospital and prison. Seven hundred and seven patients were consecutively examined during the study period. The results of this study were compared with a previous Australia-wide study to identify specific disorders that were more prevalent in rural areas. Alcohol abuse and dependence stood out as being much more prevalent. Life problems such as domestic violence, sexual assault, and incest occurred commonly in women referred for psychiatric assessment. More than ten percent of the study patients were children aged under 17, who had similar prevalence rates of the various psychiatric disorders to a national comparison. It is concluded that alcohol abuse is very common in rural New South Wales, particularly in men, although there are also high rates in women, and this is probably related, in part at least, to the high rates of domestic violence, sexual assault and incest. It appears probable that there is a cycle of alcohol abuse in men leading to domestic violence and sexual abuse in women and children. This may contribute to the latter becoming anxious and depressed. The rates of the major functional psychiatric disorders were similar to those seen nationally. There is a great need for the maldistribution of psychiatrists between metropolitan and rural areas to be addressed.

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6

Murcutt, Glenn. "The Mining Museum of Broken Hill." Perspecta 27 (1992): 168. http://dx.doi.org/10.2307/1567182.

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7

Gregson, Sarah. "Defending Internationalism in Interwar Broken Hill." Labour History, no. 86 (2004): 115. http://dx.doi.org/10.2307/27515970.

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8

Parker, S., and C. Verardo. "Broken Hill Mapping— A Cartographic Milestone." Cartography 30, no. 2 (December 2001): 41–47. http://dx.doi.org/10.1080/00690805.2001.9714157.

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9

Balding, Bill, and Sean Reddan. "Lead and environmental health in Broken Hill." New South Wales Public Health Bulletin 8, no. 12 (1997): 97. http://dx.doi.org/10.1071/nb97038.

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10

Stevens, B. P. J. "Magnetic susceptibility mapping at Broken Hill, Australia." Exploration Geophysics 30, no. 3-4 (September 1999): 105–12. http://dx.doi.org/10.1071/eg999105.

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11

See, Adrian, Adrian C. Lim, Katie Le, Jo-Ann See, and Stephen P. Shumack. "Operational teledermatology in Broken Hill, rural Australia." Australasian Journal of Dermatology 46, no. 3 (August 2005): 144–49. http://dx.doi.org/10.1111/j.1440-0960.2005.00166.x.

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12

Lyle, David, Bill Balding, Hugh Burke, and Steven Begg. "NSW Lead Management Program in Broken Hill." New South Wales Public Health Bulletin 12, no. 6 (2001): 165. http://dx.doi.org/10.1071/nb01054.

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13

Mulongo, A. H. "Tide Broken Hill skull: a Zambian casexs." Museum International 44, no. 2 (June 1992): 103–4. http://dx.doi.org/10.1111/j.1468-0033.1992.tb02202.x.

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14

Emerson, Don. "Conductivities of Broken Hill Style Lead Ores." Preview 2017, no. 188 (June 2017): 37–40. http://dx.doi.org/10.1071/pvv2017n188p37.

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15

Birch, W. D., E. A. J. Burke, V. J. Wall, and M. A. Etheridge. "Ecandrewsite, the zinc analogue of ilmenite, from Little Broken Hill, New South Wales, Australia, and the San Valentin Mine, Sierra de Cartegena, Spain." Mineralogical Magazine 52, no. 365 (April 1988): 237–40. http://dx.doi.org/10.1180/minmag.1988.052.365.10.

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AbstractEcandrewsite, the zinc analogue of ilmenite, is a new mineral which was first described from the Broken Hill lode in 1970 and discovered subsequently in ores from Little Broken Hill (New South Wales) and the San Valentin Mine, Spain. The name ‘ecandrewsite’ was used in a partial description of the mineral in ‘Minerals of Broken Hill’ (1982), thereby establishing the Little Broken Hill locality, specifically the Melbourne Rockwell Mine, as the type locality. Microprobe analysis of ecandrewsite from the type locality gave ZnO 30.42 (wt.%), FeO (total Fe) 11.37, MnO 7.64, TiO2 50.12, total 99.6%, yielding an empirical formula of (Zn0.59Fe0.24Mn0.17)1.00Ti0.99O3 based on 3 oxygen atoms. All compositions from Little Broken Hill and the San Valentin Mine are ferroan manganoan ecandrewsite. The strongest lines in the X-ray powder diffraction data are (d in Å, (hkil), I/Io):2.746, (104), 100; 2.545, (110), 80; 1.867, (024), 40; 3.734, (012), 30; 1.470, (3030), 30; 1.723, (116), 25. Ecandrewsite is hexagonal, space group RR3¯ assigned from a structural study, with a = 5.090(1), c = 14.036(2)Å, V = 314.6(3)Å3, Z = 6, D(calc.) = 4.99. The mineral is opaque, dark brown to black with a similar streak, and a submetallic lustre. In plane polarized light the reflection colour is greyish white with a pinkish tinge. Reflection pleochroism is weak, but anisotropism is strong with colours from greenish grey to dark brownish grey. Reflectance data in air between 470 and 650 nm are given. At the type locality, ecandrewsite forms disseminated tabular euhedral grains up to 250 × 50 µm, in quartz-rich metasediments. Associated minerals include almandine-spessartine, ferroan gahnite and rutile. The name is for E. C. Andrews, pioneering geologist in the Broken Hill region of New South Wales. Type material consisting of one grain is preserved in the Museum of Victoria (M35700). The mineral and name were approved by the IMA Commission on New Minerals and Mineral Names in 1979.

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16

Parr, Joanna. "The preservation of pre-metamorphic colloform banding in pyrite from the Broken Hill-type Pinnacles deposit, New South Wales, Australia." Mineralogical Magazine 58, no. 392 (September 1994): 461–71. http://dx.doi.org/10.1180/minmag.1994.058.392.11.

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AbstractTwo distinct generations of pyrite, with different morphologies, are described from the Proterozoic Broken Hill-type Pinnacles deposit in western NSW. The earlier, py1, forms concentric layers interpreted as colloform banding. Although the textures are somewhat similar to those observed in supergene alteration zones, textural relationships in fresh rocks suggest that these are pre-metamorphic and that the pyrite formed as the result of precipitation from hydrothermal fluids in open veins, vugs and fissures. The second generation, py2, post-dates py1 and forms euhedral overgrowths on it. It is interpreted as being synchronous with the main phase of base metal sulphide mineralisation. The textures reported here are previously unrecorded for Broken Hill-type mineralisation, and have implications for the regional identification of feeder zones to the Broken Hill deposit. The evidence supports a model in which mineralising conditions at the Pinnacles were characterised by slightly higher oxygen and lower sulphur fugacity (further constrained by Fe contents of sphalerite) than at Broken Hill, where pyrrhotite is the major Fe sulphide.The pre-metamorphic textures observed in the pyrite at the Pinnacles deposit are also unusual because they have survived granulite facies metamorphism and five phases of deformation, whereas previously the preservation of such textures has not been recognised at metamorphic grades greater than amphibolite facies.

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17

Xue, Zong Zhan, Deng Fa He, and Xiao Heng Wang. "The Cognition Decide the Exploration- The Exploration Study on Buried Hill Reservoir in the Liaohe Basin." Advanced Materials Research 616-618 (December 2012): 166–69. http://dx.doi.org/10.4028/www.scientific.net/amr.616-618.166.

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In recent years the buried hill exploration was a main power for increasing reserve& production in the Liaohe oil field. By the research and analysis on the buried hill reservoir exploration in the Liaohe oil field in the paper, It point out that the previously mistake cognition was broken through in the buried hill reservoir exploration with the seismic, logging etc. technology development. The achievement list as: 1. The conclusion is drawn about the depth of the buried hill reservoir determined by the depth of the source rock which clarified the mistake about the buried hill reservoir formed only in the shallow formation. 2. The inner of the buried hill reservoir of the metamorphic rock is a fissure-cave system formed by the various and layered rocks which served as an oil accumulation place which broke through the cognition on no pore in the deep inner of the buried hill reservoir. 3.The reservoir-formed pattern is built on the study of the controlled factor in the buried hill reservoir which denied the barrier of the basalt layer for oil and gas translation over the buried hill reservoir .In this paper by the summary of the cognition breakthrough and achievement, it shows the next exploration direction in buried hill reservoir in the Liaohe depression.

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18

Both, R. A., and E. F. Stumpfl. "Distribution of silver in the Broken Hill orebody." Economic Geology 82, no. 4 (July 1, 1987): 1037–43. http://dx.doi.org/10.2113/gsecongeo.82.4.1037.

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19

Carr, Paul, Malcolm Southwood, and Jeff Chen. "Fluorapatite from Broken Hill, New South Wales, Australia." Rocks & Minerals 97, no. 1 (December 20, 2021): 16–27. http://dx.doi.org/10.1080/00357529.2022.1989948.

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20

Richards, D. J. "CRAE’s Approach to Downhole TEM at Broken Hill." Exploration Geophysics 18, no. 3 (June 1987): 279–84. http://dx.doi.org/10.1071/eg987279.

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21

Webster, A. E. "Delamerian refolding of the Palaeoproterozoic Broken Hill Block." Australian Journal of Earth Sciences 43, no. 1 (February 1996): 85–89. http://dx.doi.org/10.1080/08120099608728237.

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22

Stevens, B. P. J., E. Rothery, and A. E. Webster. "Delamerian refolding of the Palaeoproterozoic Broken Hill Block." Australian Journal of Earth Sciences 44, no. 2 (April 1997): 275–79. http://dx.doi.org/10.1080/08120099708728310.

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23

Burke, Hugh, Bill Balding, and David Lyle. "Reducing lead exposure in children in Broken Hill." New South Wales Public Health Bulletin 14, no. 3 (2003): 52. http://dx.doi.org/10.1071/nb03016.

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24

Burgess, F. L. "OK100 tank cell operation at Pasminco — Broken Hill." Minerals Engineering 10, no. 7 (July 1997): 723–41. http://dx.doi.org/10.1016/s0892-6875(97)00051-4.

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25

Vassallo, J. J., and R. H. Vernon. "Origin of megacrystic felsic gneisses at Broken Hill." Australian Journal of Earth Sciences 47, no. 4 (August 2000): 733–48. http://dx.doi.org/10.1046/j.1440-0952.2000.00805.x.

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26

Flynn, Barbara. "Trade Unions and the Law: The Broken Hill Dispute." Journal of Industrial Relations 30, no. 1 (March 1988): 32–53. http://dx.doi.org/10.1177/002218568803000102.

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The Broken Hill mines dispute erupted in February 1986. It resulted in a two-month lockout of employees and the permanent loss of 860 jobs—almost a third of the local mining industry's workforce. A study of the Broken Hill dispute will be useful to unions, management and students. The experiences of the Broken Hill unions are indicative of problems facing all Australian unions in this period of economic uncertainty. The union and company industrial and legal tactics in the dispute are analysed in this paper. The use of the law by management to thwart the industrial objectives of the unions is an important theme. It is apparent that in future the Australian union movement will need to be aware of the implications at law of their industrial strategies and that they should seek legal advice at an early stage in a dispute. They should also ensure their contract of employment offers adequate protection at law.

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27

Millsteed, P. W. "Marshite–miersile solid solution and iodargyrite from Broken Hill, New South Wales, Australia." Mineralogical Magazine 62, no. 04 (August 1998): 471–75. http://dx.doi.org/10.1180/002646198547846.

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Abstract Microprobe analysis of marshite and miersite from Broken Hill, Australia, demonstrate extensive solid solution between the end-members CuI and AgI, indicating the possibility of a complete solid-solution series. Unit-cell parameters increase from 6.054 Å for marshite to 6.504 Å for miersite, closely following Vegard's Law. The Cu content of iodargyrite is generally below the limit of detection, but one zoned crystal contained 0.28 wt.% Cu. Crystallization of either miersite or iodargyrite at Broken Hill appears to be dependent upon the local availability and ratio of copper, silver and iodine ions.

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28

Jones, David. "Re-greening ‘The Hill’: Albert Morris and the transformation of the Broken Hill landscape." Studies in the History of Gardens & Designed Landscapes 31, no. 3 (September 2011): 181–95. http://dx.doi.org/10.1080/14601176.2010.540804.

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29

Carr, P. F., B. Selleck, M. Stott, and P. Williamson. "NATIVE LEAD AT BROKEN HILL, NEW SOUTH WALES, AUSTRALIA." Canadian Mineralogist 46, no. 1 (February 1, 2008): 73–85. http://dx.doi.org/10.3749/canmin.46.1.73.

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30

Plimer, Ian R. "Strata-bound scheelite in meta-evaporites, Broken Hill, Australia." Economic Geology 89, no. 3 (May 1, 1994): 423–37. http://dx.doi.org/10.2113/gsecongeo.89.3.423.

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31

Inegbenebor, A. I., P. A. Williams, R. E. Bevins, M. P. Lambert, and Alan D. Hart. "Composition of pyromorphites from Broken Hill, New South Wales." Records of the Australian Museum, Supplement 15 (October 16, 1992): 29–37. http://dx.doi.org/10.3853/j.0812-7387.15.1992.81.

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32

Guillen, Antonio, Richard Lane, Gabriel Courrioux, Terry Lees, Ph Calcagno, and Philip Mclnerney. "Constrained Gravity 3D Litho-Inversion Applied to Broken Hill." ASEG Extended Abstracts 2004, no. 1 (December 2004): 1–6. http://dx.doi.org/10.1071/aseg2004ab057.

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33

Henderson, R. J., and B. P. J. Stevens. "Discussion on: “Magnetic Susceptibility Mapping at Broken Hill, Australia”." Exploration Geophysics 31, no. 4 (September 2000): 629. http://dx.doi.org/10.1071/eg00629.

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34

Bishop, John, Noel Carroll, Mike Asten, Mike Hatch, and Scott Macinnes. "Finding Sphalerite at Broken Hill With Drillhole Magnetometric Resistivity." Exploration Geophysics 28, no. 1-2 (March 1997): 6–10. http://dx.doi.org/10.1071/eg997006.

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35

Norris, Ken. "Review Essay: “From This Broken Hill”: Leonard Cohen'sStranger Music." American Review of Canadian Studies 24, no. 3 (October 1994): 363–75. http://dx.doi.org/10.1080/02722019409481772.

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36

Birch, W. D. "Zinc-manganese carbonates from Broken Hill, New South Wales." Mineralogical Magazine 50, no. 355 (March 1986): 49–53. http://dx.doi.org/10.1180/minmag.1986.050.355.07.

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AbstractSpecimens of honey-brown to pinkish-brown globular carbonates encrusting concretionary goethite–coronadite from the oxidized zone at Broken Hill, New South Wales, have compositions in the rhodochrosite–smithsonite series. This may be the first extensive natural occurrence of this solid-solution series. Growth of the carbonates occurred in zones which have near uniform composition. The ratio MnCO3/(MnCO3 + ZnCO3) for each zone bears a linear relationship to the measured d spacing for the 104 X-ray reflections. Because cerussite is the only other mineral associated with the Zn-Mn carbonates and because of an absence of detailed locality information, the paragenetic significance of these minerals cannot be determined. The solutions depositing them may have been derived from the near-surface equivalents of the Zinc Lode horizons.

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37

Smith, Luke, and Tasman Gillfeather-Clark. "Self Organising Maps - A Case Study of Broken Hill." ASEG Extended Abstracts 2018, no. 1 (December 2018): 1–6. http://dx.doi.org/10.1071/aseg2018abt7_2g.

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38

Rattray, K. J., M. R. Taylor, D. J. M. Bevan, and A. Pring. "Compositional segregation and solid solution in the lead-dominant alunite-type minerals from Broken Hill, N.S.W." Mineralogical Magazine 60, no. 402 (October 1996): 779–85. http://dx.doi.org/10.1180/minmag.1996.060.402.07.

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AbstractA study of the composition and unit cell data of a suite of lead-rich minerals of the alunite-jarosite group from the oxidized zone of the ore body at Broken Hill, New South Wales, Australia, has revealed almost complete XO4 (X = As, P, S) solid solution in these minerals at this deposit. The species in the group noted are hidalgoite, hinsdalite, beudantite, segnitite and plumbogummite. These minerals at Broken Hill exhibit a number of growth textures, including oscillatory zoning, colloform banding and replacements. Zoning in these minerals is due to the segregation of Al- and Fe-rich members, and compositions indicate a strong coupling of Fe3+ with and Al with

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39

Lyle, David M., Frances T. Boreland, Najeebullah Soomro, and Melinda Glisson-Gladman. "Is Time Spent Outside the Family Home a Risk Factor for Lead Exposure in Pre-School Children Living in Broken Hill?" International Journal of Environmental Research and Public Health 18, no. 15 (July 21, 2021): 7721. http://dx.doi.org/10.3390/ijerph18157721.

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Broken Hill is amongst a group of communities internationally that are at greater risk from lead due to active or historical lead industries. Current evidence suggests there is no safe level of lead for young children. This paper describes places outside the family home where young Broken Hill children spend time and considers the potential for this to contribute to lead risk. We interviewed 65 families of children 3 years old or younger and detailed the top five places children spent time at outside the family home. Exposure to private residences outside the family home was recorded for most (88%) young children. Nearly two thirds stayed there five or more hours per week. Most children went there on a weekly basis over many months (median, 12 months), increasing the likelihood of exposure to lead hazards. Further investigation of the lead hazard and risk behaviour of children at these residences would assist in developing guidelines for remediation of the lead hazard for all private residences in Broken Hill. This approach to elucidating the potential sources and pathways of lead and other heavy metal exposures for young children may have merit in other settings where comprehensive zonal remediation is not feasible or may not be warranted.

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40

Hay, John. "Broken Hearths: Melville's Israel Potter and the Bunker Hill Monument." New England Quarterly 89, no. 2 (June 2016): 192–221. http://dx.doi.org/10.1162/tneq_a_00528.

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When he dedicated Israel Potter to the Bunker Hill Monument, Herman Melville gestured to an eminent national memorial which took so long to build that it appeared to be in ruins before it was finished. Melville's novel addresses the temporal quirks of both patriotic communal commemoration and posthumous personal recognition.

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41

Spry, Paul G., and Graham S. Teale. "A classification of Broken Hill-type deposits: A critical review." Ore Geology Reviews 130 (March 2021): 103935. http://dx.doi.org/10.1016/j.oregeorev.2020.103935.

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42

Birch, William D. "Broken Hill New South Wales, Australia: Its Contribution to Mineralogy." Rocks & Minerals 82, no. 1 (January 2007): 40–49. http://dx.doi.org/10.3200/rmin.82.1.40-49.

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43

Frost, B. R., S. M. Swapp, and J. Mavrogenes. "Textural Evidence for Extensive Melting of the Broken Hill Orebody." Economic Geology 106, no. 5 (July 22, 2011): 869–82. http://dx.doi.org/10.2113/econgeo.106.5.869.

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44

Boreland, Frances, Margaret S. Lesjak, and David M. Lyle. "Managing environmental lead in Broken Hill: a public health success." New South Wales Public Health Bulletin 19, no. 10 (2008): 174. http://dx.doi.org/10.1071/nb07099.

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45

Bishop, J. R. "DHEM Surveys of the 2K Area, North Mine, Broken Hill." Exploration Geophysics 27, no. 2-3 (June 1996): 51–65. http://dx.doi.org/10.1071/eg996051.

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46

Ruszkowski, Mr Peter. "An analysis of the Broken Hill exploration initiative petrophysical database." Exploration Geophysics 29, no. 3-4 (September 1998): 592–96. http://dx.doi.org/10.1071/eg998592.

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47

Stevens, B. P. J., and G. M. Bradley. "Sedimentology in metamorphic rocks, the Willyama Supergroup, Broken Hill, Australia." Australian Journal of Earth Sciences 65, no. 1 (December 3, 2017): 25–59. http://dx.doi.org/10.1080/08120099.2018.1399462.

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48

Lotfolah Hamedani, Mohammad, Ian Rutherford Plimer, and Chaoshui Xu. "Orebody Modelling for Exploration: The Western Mineralisation, Broken Hill, NSW." Natural Resources Research 21, no. 3 (June 19, 2012): 325–45. http://dx.doi.org/10.1007/s11053-012-9177-1.

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49

Doyle, C., and I. Cartwright. "The role of fluids in retrograde shearing: Broken Hill, Australia." Journal of Geochemical Exploration 69-70 (June 2000): 575–79. http://dx.doi.org/10.1016/s0375-6742(00)00062-5.

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50

Millsteed, Paul W. "Faceting Transparent Rhodonite from Broken Hill, New South Wales, Australia." Gems & Gemology 42, no. 2 (June 1, 2006): 151–58. http://dx.doi.org/10.5741/gems.42.2.151.

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