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Статті в журналах з теми "Tennant Creek"

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Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 19 лютого 2023

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1

Franks, PJ, A. Gibson, and EP Bachelard. "Xylem Permeability and Embolism Susceptibility in Seedlings of Eucalyptus camaldulensis Dehnh. From Two Different Climatic Zones." Functional Plant Biology 22, no. 1 (1995): 15. http://dx.doi.org/10.1071/pp9950015.

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We examined the hydraulic architecture of Eucalyptus camaldulensis seedlings from two climatically different provenances: Petford in north Queensland, which is humid; and Tennant Creek in the Northern Territory, which is semi-arid. Xylem liquid specific permeability (Kg) was calculated from measurements of xylem air permeability (Kg) and hydraulic resistances (R) were also calculated. Embolism susceptibility curves were constructed by measuring Kg in the stems of young seedlings. Canopy leaf areas were mapped and sap flows through the Tennant Creek and Petford seedlings were simulated. Results showed that the permeability of stem wood in the Tennant Creek seedling was about 40% higher than in Petford, and the permeability of its branch wood was about 25% higher. The threshold water potential for initiation of embolisms (Ψt) was slightly lower in Tennant Creek seedlings (- 3.3 MPa compared with - 3.0 MPa) and the number of embolisms with decreasing Ψ was lower for Tennant Creek seedlings. Sap flow simulations showed differences in the distribution of water throughout the seedling canopies. The results are discussed in terms of the ecology of the two eucalypt provenances.

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2

Johnstone, Andrew. "Basement interpretation of the Tennant Creek region." ASEG Extended Abstracts 2001, no. 1 (December 2001): 1–4. http://dx.doi.org/10.1071/aseg2001ab064.

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3

Bowman, J. R. "The 1988 Tennant Creek, northern territory, earthquakes: A synthesis." Australian Journal of Earth Sciences 39, no. 5 (December 1992): 651–69. http://dx.doi.org/10.1080/08120099208728056.

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4

Gulson, Brian L., Ross R. Large, and Patricia M. Porritt. "Gold exploration using lead isotopes at Tennant Creek, Australia." Applied Geochemistry 3, no. 3 (May 1988): 243–54. http://dx.doi.org/10.1016/0883-2927(88)90104-7.

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5

Gulson, Brian L., Ross R. Large, and Patricia M. Porritt. "Gold exploration using lead isotopes at Tennant Creek, Australia." Journal of Geochemical Exploration 32, no. 1-3 (April 1989): 309–10. http://dx.doi.org/10.1016/0375-6742(89)90068-x.

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6

McCaffrey, Robert. "Teleseismic investigation of the January 22, 1988 Tennant Creek, Australia, earthquakes." Geophysical Research Letters 16, no. 5 (May 1989): 413–16. http://dx.doi.org/10.1029/gl016i005p00413.

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7

Tanaka, Kazuhiro, Michael N. Machette, Anthony J. Crone, and J. Roger Bowman. "ESR dating of aeolian sand near tennant creek, Northern territory, Australia." Quaternary Science Reviews 14, no. 4 (January 1995): 385–93. http://dx.doi.org/10.1016/0277-3791(95)00032-1.

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8

Hoschke, T. "A new drill hole magnetometer: preliminary results from the Tennant Creek area." Exploration Geophysics 16, no. 4 (September 1985): 365–74. http://dx.doi.org/10.1071/eg985365.

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9

Gray, Dennis, Sherry Saggers, David Atkinson, Brooke Sputore, and Deirdre Bourbon. "Beating the grog: an evaluation of the Tennant Creek liquor licensing restrictions." Australian and New Zealand Journal of Public Health 24, no. 1 (February 2000): 39–44. http://dx.doi.org/10.1111/j.1467-842x.2000.tb00721.x.

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10

Compston, D. "Time constraints on the evolution of the Tennant Creek Block, northern Australia." Precambrian Research 71, no. 1-4 (February 1995): 107–29. http://dx.doi.org/10.1016/0301-9268(94)00058-y.

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11

Hoschke, T. "Geophysical Discovery and Evaluation of the West Peko Copper-gold Deposit, Tennant Creek." Exploration Geophysics 22, no. 3 (September 1991): 485–95. http://dx.doi.org/10.1071/eg991485.

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12

Bowman, J. Roger. "Geodetic evidence for conjugate faulting during the 1988 Tennant Creek, Australia earthquake sequence." Geophysical Journal International 107, no. 1 (October 1991): 47–56. http://dx.doi.org/10.1111/j.1365-246x.1991.tb01155.x.

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13

Bowman, J. Roger, and James W. Dewey. "Relocation of teleseismically recorded earthquakes near Tennant Creek, Australia: Implications for midplate seismogenesis." Journal of Geophysical Research 96, B7 (1991): 11973. http://dx.doi.org/10.1029/91jb00923.

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14

Cattach, Malcolm, and Andrew Foley. "A Sub-Audio Magnetics Case Study: Orlando Au-Cu-Bi Deposit, Tennant Creek, Australia." Exploration Geophysics 36, no. 2 (June 2005): 147–56. http://dx.doi.org/10.1071/eg05147.

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15

Kerr, R. C., and J. R. Lister. "The lateral intrusion of silicic magmas into unconsolidated sediments: The Tennant Creek porphyry revisited." Australian Journal of Earth Sciences 42, no. 2 (April 1995): 223–24. http://dx.doi.org/10.1080/08120099508728193.

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16

Duggan, M. B., and A. L. Jaques. "Mineralogy and geochemistry of Proterozoic shoshonitic lamprophyres from the Tennant Creek Inlier, northern territory." Australian Journal of Earth Sciences 43, no. 3 (June 1996): 269–78. http://dx.doi.org/10.1080/08120099608728254.

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17

Carfoot, Gavin. "‘Enough is Enough’: songs and messages about alcohol in remote Central Australia." Popular Music 35, no. 2 (April 14, 2016): 222–30. http://dx.doi.org/10.1017/s0261143016000040.

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Анотація:

AbstractThis article examines some of the ways in which Australia's First Peoples have responded to serious community health concerns about alcohol through the medium of popular music. The writing, performing and recording of popular songs about alcohol provide an important example of community-led responses to health issues, and the effectiveness of music in communicating stories and messages about alcohol has been recognised through various government-funded recording projects. This article describes some of these issues in remote Australian Aboriginal communities, exploring a number of complexities that arise through arts-based ‘instrumentalist’ approaches to social and health issues. It draws on the author's own experience and collaborative work with Aboriginal musicians in Tennant Creek, a remote town in Australia's Northern Territory.

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18

Turner, G., G. Osborne, J. Cook, J. Kinkela, R. Bills, R. Smith, G. Hird, A. Cuison, and S. Zulic. "Examples of the use of seismic reflection to re-invigorate a mature field: Tennant Creek." ASEG Extended Abstracts 2016, no. 1 (December 2016): 1–8. http://dx.doi.org/10.1071/aseg2016ab319.

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19

Rattenbury, M. S. "Stratigraphic and structural controls on ironstone mineralization in the Tennant Creek goldfield, Northern Territory, Australia." Australian Journal of Earth Sciences 39, no. 5 (December 1992): 591–602. http://dx.doi.org/10.1080/08120099208728052.

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20

McPhie, J. "The Tennant Creek porphyry revisited: A synsedimentary sill with peperite margins, Early Proterozoic, Northern Territory." Australian Journal of Earth Sciences 40, no. 6 (December 1993): 545–58. http://dx.doi.org/10.1080/08120099308728103.

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21

Stolz, A. J., R. R. Large, P. Robinson, and R. Wedekind. "Criteria for distinguishing between gold-bearing and barren ironstones at Tennant Creek, Northern Territory, Australia." Journal of Geochemical Exploration 51, no. 3 (September 1994): 247–64. http://dx.doi.org/10.1016/0375-6742(94)90009-4.

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22

McCaffrey, Robert, and Joanne Fredrich. "Source Parameters of Large Australian Intracontinental Earthquakes." Seismological Research Letters 59, no. 4 (October 1, 1988): 315. http://dx.doi.org/10.1785/gssrl.59.4.315.

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Abstract We have examined the largest earthquakes in the Australian continent over the past 20 years by modeling their teleseismic long-period P and SH and short-period P waveforms. Eight earthquakes beneath the continent show thrust faulting at depths shallower than 10 km. Three (1, 2, 4 below) produced surface faulting and their waveforms indicate centroid depths of 3 km or less. The P-axes in the southwestern half of the continent have easterly trends. Preliminary examination of the 3 large earthquakes near Tennant Creek on 22 January, 1988, (7–9) indicate thrusting at less than 10 km depth, but with N-trending P-axes. The largest event (9), at 12:06 GMT, had a seismic moment of roughly 1019 Nm, which makes it comparable in size to the 1968 Meckering event (1). One event (6) beneath the continental margin indicates strike-slip at 26 km depth.

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23

McInnes, B. I. A., R. R. Keays, D. D. Lambert, J. Hellstrom, and J. S. Allwood. "Re–Os geochronology and isotope systematics of the Tanami, Tennant Creek and Olympic Dam Cu–Au deposits." Australian Journal of Earth Sciences 55, no. 6-7 (August 2008): 967–81. http://dx.doi.org/10.1080/08120090802097443.

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24

Egan, JL, and RJ Williams. "Lifeform distributions of woodland plant species along a moisture availability gradient in Australia's monsoonal tropics." Australian Systematic Botany 9, no. 2 (1996): 205. http://dx.doi.org/10.1071/sb9960205.

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Анотація:

A series of vegetation sites was established in Australia's Northern Territory between Darwin and Tennant Creek, a distance of approximately 1000 km and 7° latitude (12°30'–19°30'S). This region encompasses a strong environmental gradient in mean annual moisture availability (450–1600 mm) whilst remaining within a predominantly summer monsoonal rainfall regime. All sites are within eucalypt-savanna habitats on lighter textured soils (sands–loams). Major changes in family and species representation occur at approximately 16–17° latitude, supporting findings of other workers. Within these eucalypt-savanna communities, the percentage of annual species is consistently around 30% regardless of latitude. However, the distribution of resource allocation strategies used by perennial plants exhibits distinct latitudinal trends. The proportion of deciduous and seasonally perennial species declines with latitude whilst suffrutescent shrub species become increasingly abundant. Species possessing root structures adapted for storage purposes appear to be limited to latitudes north of 15°S.

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25

Trendall, A. F., E. H. Francis, and J. McPhie. "Discussion and reply The Tennant Creek porphyry revisited: A synsedimentary sill with peperite margins, early Proterozoic, northern territory." Australian Journal of Earth Sciences 41, no. 4 (August 1994): 391–94. http://dx.doi.org/10.1080/08120099408728149.

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26

Bowman, J. R., G. Gibson, and T. Jones. "Aftershocks of the 1988 January 22 Tennant Creek, Australia Intraplate Earthquakes: Evidence For A Complex Thrust-Fault Geometry." Geophysical Journal International 100, no. 1 (January 1990): 87–97. http://dx.doi.org/10.1111/j.1365-246x.1990.tb04570.x.

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27

Gibson, A., KT Hubick, and EP Bachelard. "Effects of Abscisic Acid on Morphological and Physiological Responses to Water Stress in Eucalyptus camaldulensis Seedlings." Functional Plant Biology 18, no. 2 (1991): 153. http://dx.doi.org/10.1071/pp9910153.

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The effects of abscisic acid (ABA) and a subsequent water stress on the physiological and morphological characteristics of seedlings of three provenances of Eucalyptus camaldulensis Dehnh. grown in pots in a glasshouse were compared 56 days after application of ABA. Seedlings from a high rainfall monsoon provenance in the dry tropics (Katherine, Northern Territory, Australia) were largely unaffected by ABA or by water strees in either physiological or morphological characteristics. Seedlings from a lower rainfall monsoon provenance in the humid tropics (Petford, Queensland) responded to water stress by reducing gas exhange while increasing photosynthetic capacity, indicated by increased leaf nitrogen and chlorophyll concentrations, and both short- and long-term leaf transpiration efficiency, indicated by changes in carbon-isotope discrimination. The changes were largest when ABA was also applied. Seedlings from semi-arid Tennant Creek (Northern Territory), which had the highest assimilation rates overall, responded to both ABA and water stress primarily by morphological changes including suppression of apical growth and increase in specific leaf weight. The results are discussed in terms of specific adaptations for establishment in increasingly dry environments and the possible role of ABA in mediating stress responses.

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28

Skirrow, R. G., and J. L. Walshe. "Reduced and Oxidized Au-Cu-Bi Iron Oxide Deposits of the Tennant Creek Inlier, Australia: An Integrated Geologic and Chemical Model." Economic Geology 97, no. 6 (September 1, 2002): 1167–202. http://dx.doi.org/10.2113/gsecongeo.97.6.1167.

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29

Goodwin, James A., and Roger G. Skirrow. "Mapping IOCG-related alteration using 3D gravity and magnetic inversion: an example from the Tennant Creek – Mount Isa region, northern Australia." ASEG Extended Abstracts 2019, no. 1 (November 11, 2019): 1–6. http://dx.doi.org/10.1080/22020586.2019.12073080.

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30

Jiang, Wenping, Jingming Duan, Michael Doublier, Andrew Clark, Anthony Schofield, Ross C. Brodie, and James Goodwin. "Application of multiscale magnetotelluric data to mineral exploration: an example from the east Tennant region, Northern Australia." Geophysical Journal International 229, no. 3 (February 16, 2022): 1628–45. http://dx.doi.org/10.1093/gji/ggac029.

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SUMMARY The footprint of a mineral system is potentially detectable at a range of scales and lithospheric depths, reflecting the size and distribution of its components. Magnetotellurics is one of a few techniques that can provide multiscale data sets to image and understand mineral systems. We have used long-period data from the Australian Lithospheric Architecture Magnetotelluric Project (AusLAMP) as a first-order reconnaissance survey to resolve large-scale lithospheric architecture for mapping areas of mineral potential in northern Australia. The 3-D resistivity model reveals a broad conductivity anomaly extending from the Tennant Creek district to the Murphy Province in the lower crust and upper mantle, representing a potential fertile source region for mineral systems. Results from a higher-resolution infill magnetotelluric survey reveal two prominent conductors in an otherwise resistive host whose combined responses result in the lithospheric-scale conductivity anomaly mapped in the AusLAMP model. Integration of the conductivity structure with deep seismic reflection data reveals a favourable crustal architecture linking the lower, fertile source regions with potential depositional sites in the upper crust. The enhanced conductivity likely resulted from the remnant (metallic) material deposited when fluids were present during the ‘ancient’ tectonic events. This observation strongly suggests that the deep-penetrating major faults potentially acted as pathways for transporting metalliferous fluids to the upper crust where they could form mineral deposits. This result and its integration with other geophysical and geochronological data sets suggest high prospectivity for major mineral deposits in the vicinity of these major faults, that is, Gulunguru Fault and Lamb Fault. In addition to these insights, interpretation of high-frequency magnetotelluric data acquired during the infill survey helps to characterize cover and assist with selecting targets for stratigraphic drilling which, in turn, can validate the models and improve our understanding of basement geology, cover sequences and mineral potential. This study demonstrates that integration of geophysical data from multiscale surveys is an effective approach to scale reduction during mineral exploration in covered terranes with limited geological knowledge.

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31

Doyle, Hugh A. "Geophysical exploration for gold—A review." GEOPHYSICS 55, no. 2 (February 1990): 134–46. http://dx.doi.org/10.1190/1.1442820.

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It is almost impossible to get a direct geophysical response from gold because of the low grades in deposits, except when electromagnetic detectors are used for individual shallow nuggets. However, indirect geophysical indications may occur through association of gold with particular host rocks, marker beds, or structures which are, for example, of unusual magnetization, density, electric polarization, or conductivity/resistivity. Useful markers may be magnetic dolerites, banded iron formations, shales with magnetite, conductive and/or polarizable pyrites, or other sulfide (detectable by IP methods) and silicified zones more resistive than surrounding rocks. Mapping of faults and shear zones, with which gold may be associated, is also valuable (e.g., by magnetic, EM surveys, etc.). Magnetite depletion is characteristic of some deposits, resulting in zones of low anomalies; for example, ferromagnetic minerals in mafic volcanics are destroyed by carbonatization. Resistivity patterns may indicate altered rocks which contain mineralization, thus the use of VLF-EM methods in Canada and MMR in Australia. Geophysical methods have been important in the search for gold in the Witwatersrand Basin of South Africa (magnetic, gravity, and even seismic reflection methods), various areas of Canada, e.g., the Abitibi greenstone belt (magnetic, EM, and IP surveys), and to a smaller extent in Australia (e.g., Tennant Creek, NT and Water Tank Hill, WA). However, the value of geophysical methods should not be exaggerated since physical contrasts are often low.

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32

Gibson, A., EP Bachelard, and KT Hubick. "Growth Strategies of Eucalyptus camaldulensis Dehnh. At Three Sites in Northern Australia." Functional Plant Biology 21, no. 5 (1994): 653. http://dx.doi.org/10.1071/pp9940653.

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The morphology and physiology of trees of Eucalyptus camaldulensis growing in the field at two monsoonal and one semi-arid location were compared. In the wet season, shoot growth at the monsoonal locations was similar and larger than that at the semi-arid location. In the dry season, new shoot growth at the more humid monsoonal location (Petford) was similar to growth in the wet season while at the less humid (Katherine) and the semi-arid (Tennant Creek) locations, shoot growth was foreshortened and the leaves had larger dry weights per unit area. In the summer wet season, leaves on both the north and south sides of the trees were maintained at or below (by up to 5�C) air temperatures throughout the day except for north facing leaves at Petford which were consistently above (by up to 3�C) air temperatures. Midday gas exchange in the dry season at both monsoonal localities was restricted to trees at the water's edge, whereas most trees, including those at drier sites, at the semi-arid location exhibited significant rates of gas exchange. The results, which are discussed in relation to environmental variables (vapour pressure deficits, wind speeds) to which the trees are exposed, and to previous results obtained in the glasshouse, indicate that the differences in shoot growth and physiology are adaptations to the environment in which the trees have evolved.

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33

Compston, D. M., and I. McDougall. "40Ar‐39Ar and K‐Ar age constraints on the Early Proterozoic Tennant Creek Block, northern Australia, and the age of its gold deposits∗." Australian Journal of Earth Sciences 41, no. 6 (December 1994): 609–16. http://dx.doi.org/10.1080/08120099408728171.

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34

Bradley, John, Frances Devlin-Glass, and Elizabeth Mackinlay. "Diwurruwurru: Towards a New Kind of Two-Way Classroom." Australian Journal of Indigenous Education 27, no. 2 (December 1999): 24–26. http://dx.doi.org/10.1017/s1326011100600546.

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A project is currently underway at http://arts.deakin.edu.au which is innovative on a number of fronts. It has multiple beginnings: in the proactive, as culture dissemination work of a number of Yanyuwa and Garrwa women, who proclaimed in the white man’s world that they were ‘bosses themselves’ (Gale 1983) and who in various ways have sought to bring their culture to the attention of the wider world. This has been accomplished through a prize-winning (Atom Australian Teachers of Media awards in 1991) film, Buwarrala Akarriya: Journey East (1989), of are-enacted ritual foot-walk in 1988 from Borroloola to Manankurra 90 kilometres away. They also made a another prize winning film called Ka-wayawayarna: The Aeroplane Dance (1993) which won the Royal Anthropological Society of London award for the best ethnographic film in 1995. Since 1997 senior Yanyuwa women have been involved on a regular basis in sharing their knowledge of Yanyuwa performance practice with tertiary students in a subject called Women’s Music and Dance in Indigenous Australia which is offered as a course in anthropology through the Aboriginal and Torres Strait Islander Studies Unit, they have also lectured in core anthropology subjects in the faculty of Social and Behavourial Sciences Department of Anthropology and Sociology at the University of Queensland. They have also engaged actively in work as language preservers and teachers at the Borroloola Community Education Centre (hereafter BCEC) and in the Tennant Creek Language Centre program called Papulu Apparr-Kari.

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35

Huston, David L., Chris Bolger, and Greg Cozens. "A comparison of mineral deposits at the Gecko and White Devil deposits; implications for ore genesis in the Tennant Creek District, Northern Territory, Australia." Economic Geology 88, no. 5 (August 1, 1993): 1198–225. http://dx.doi.org/10.2113/gsecongeo.88.5.1198.

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36

Choy, George L., and J. Roger Bowman. "Rupture process of a multiple main shock sequence: Analysis of teleseismic, local, and field observations of the Tennant Creek, Australia, earthquakes of January 22, 1988." Journal of Geophysical Research 95, B5 (1990): 6867. http://dx.doi.org/10.1029/jb095ib05p06867.

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37

Bartleet, Brydie-Leigh, Naomi Sunderland, and Gavin Carfoot. "Enhancing intercultural engagement through service learning and music making with Indigenous communities in Australia." Research Studies in Music Education 38, no. 2 (October 6, 2016): 173–91. http://dx.doi.org/10.1177/1321103x16667863.

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This article explores the potential for music making activities such as jamming, song writing, and performance to act as a medium for intercultural connection and relationship building during service learning programs with Indigenous communities in Australia. To set the context, the paper begins with an overview of current international perspectives on service learning and then moves towards a theoretical and practical discussion of how these processes, politics, and learning outcomes arise when intercultural engagement is used in service learning programs. The paper then extends this discussion to consider the ways in which shared music making can bring a sense of intercultural “proximity” that has the potential to evoke deep learning experiences for all involved in the service learning activity. These learning experiences arise from three different “facings” in the process of making music together: facing others together; facing each other; facing ourselves. In order to flesh out how these theoretical ideas work in practice, the article draws on insights and data from Queensland Conservatorium Griffith University’s award winning Winanjjikari Service Learning Program, which has been running in partnership with Barkly Regional Arts and Winanjjikari Music Centre in Tennant Creek since 2009. This program involves annual service learning trips where university music students travel to Central Australia to work alongside Aboriginal and non-Indigenous musicians and artists on a range of community-led projects. By looking at the ways in which shared music making brings participants in this program “face to face”, we explore how this proximity leads to powerful learning experiences that foster mutual appreciation, relationship building, and intercultural reconciliation.

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38

EWART, A., L. W. POPPLE, and K. B. R. HILL. "Five new species of grass cicadas in the genus Graminitigrina (Hemiptera: Cicadidae: Cicadettinae: Cicadettini) from Queensland and Northern Territory, Australia: comparative morphology, songs, behaviour and distributions." Zootaxa 4228, no. 1 (February 7, 2017): 1. http://dx.doi.org/10.11646/zootaxa.4228.1.1.

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Five new species of small grass cicadas belonging to the genus Graminitigrina Ewart and Marques are described, together with detailed analyses of their calling songs. Four species occur in Queensland, G. aurora n. sp. from eastern central Queensland near Fairbairn Dam; G. flindensis n. sp. from central Queensland between Hughenden northwards for at least 108 km; G. einasleighi n. sp. from near The Lynd, Einasleigh River, northeastern Queensland; G. selwynensis n. sp. from the Selwyn Range, northwestern Queensland, at locations about 40 km east of Mount Isa and 25 km southwest of Cloncurry, this latter here transferred from G. bowensis Ewart and Marques; G. uluruensis n. sp. from Uluru and the Olgas in southwestern Northern Territory, extending northwards through Tennant Creek and apparently further north to near Larrimah, a linear distance of approximately 1190 km. These new species bring the known Graminitigrina species to ten, all superficially similar in colour and morphology. A key to male specimens is provided for the 10 species. Additional distribution records and additional aural song recordings are presented for G. bowensis, these requiring the transfer of populations previously identified as G. bowensis from Croydon and Georgetown, northern Gulf region, to G. karumbae Ewart and Marques. Detailed comparative analyses, including NMDS analyses, of the songs of all 10 species are provided, which show that the song parameters are appropriate to distinguish the species, although some partial overlap is noted in the waveform plots between the songs of G. uluruensis n. sp. and G. flindensis n. sp. Regional variations of song parameters are noted in the calling songs of most of the species described.

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39

Fraser, G. L., K. Hussey, and D. M. Compston. "Timing of Palaeoproterozoic Au–Cu–Bi and W-mineralization in the Tennant Creek region, northern Australia: Improved constraints via intercalibration of 40Ar/39Ar and U–Pb ages." Precambrian Research 164, no. 1-2 (June 2008): 50–65. http://dx.doi.org/10.1016/j.precamres.2008.03.005.

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40

Skirrow, Roger G., Andrew J. Cross, Andreï Lecomte, and Julien Mercadier. "A shear-hosted Au-Cu-Bi metallogenic event at ~1660 Ma in the Tennant Creek goldfield (northern Australia) defined by in-situ monazite U-Pb-Th dating." Precambrian Research 332 (September 2019): 105402. http://dx.doi.org/10.1016/j.precamres.2019.105402.

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41

Campbell, I. H., D. M. Compston, J. P. Richards, J. P. Johnson, and A. J. R. Kent. "Review of the application of isotopic studies to the genesis of Cu‐Au mineralisation at Olympic Dam and Au mineralisation at Porgera, the Tennant Creek district and Yilgarn Craton." Australian Journal of Earth Sciences 45, no. 2 (April 1998): 201–18. http://dx.doi.org/10.1080/08120099808728382.

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42

Goodge, John W. "Crustal heat production and estimate of terrestrial heat flow in central East Antarctica, with implications for thermal input to the East Antarctic ice sheet." Cryosphere 12, no. 2 (February 8, 2018): 491–504. http://dx.doi.org/10.5194/tc-12-491-2018.

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Abstract. Terrestrial heat flow is a critical first-order factor governing the thermal condition and, therefore, mechanical stability of Antarctic ice sheets, yet heat flow across Antarctica is poorly known. Previous estimates of terrestrial heat flow in East Antarctica come from inversion of seismic and magnetic geophysical data, by modeling temperature profiles in ice boreholes, and by calculation from heat production values reported for exposed bedrock. Although accurate estimates of surface heat flow are important as an input parameter for ice-sheet growth and stability models, there are no direct measurements of terrestrial heat flow in East Antarctica coupled to either subglacial sediment or bedrock. As has been done with bedrock exposed along coastal margins and in rare inland outcrops, valuable estimates of heat flow in central East Antarctica can be extrapolated from heat production determined by the geochemical composition of glacial rock clasts eroded from the continental interior. In this study, U, Th, and K concentrations in a suite of Proterozoic (1.2–2.0 Ga) granitoids sourced within the Byrd and Nimrod glacial drainages of central East Antarctica indicate average upper crustal heat production (Ho) of about 2.6 ± 1.9 µW m−3. Assuming typical mantle and lower crustal heat flux for stable continental shields, and a length scale for the distribution of heat production in the upper crust, the heat production values determined for individual samples yield estimates of surface heat flow (qo) ranging from 33 to 84 mW m−2 and an average of 48.0 ± 13.6 mW m−2. Estimates of heat production obtained for this suite of glacially sourced granitoids therefore indicate that the interior of the East Antarctic ice sheet is underlain in part by Proterozoic continental lithosphere with an average surface heat flow, providing constraints on both geodynamic history and ice-sheet stability. The ages and geothermal characteristics of the granites indicate that crust in central East Antarctica resembles that in the Proterozoic Arunta and Tennant Creek inliers of Australia but is dissimilar to other areas like the Central Australian Heat Flow Province that are characterized by anomalously high heat flow. Age variation within the sample suite indicates that central East Antarctic lithosphere is heterogeneous, yet the average heat production and heat flow of four age subgroups cluster around the group mean, indicating minor variation in the thermal contribution to the overlying ice sheet from upper crustal heat production. Despite these minor differences, ice-sheet models may favor a geologically realistic input of crustal heat flow represented by the distribution of ages and geothermal characteristics found in these glacial clasts.

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43

"95/03756 Feasibility study for Tennant Creek solar thermal power station." Fuel and Energy Abstracts 36, no. 4 (July 1995): 271. http://dx.doi.org/10.1016/0140-6701(95)95377-h.

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Chitturi, Sridhar. "Adoption Of Telemedicine -need of the hour." JMS SKIMS 23, no. 3 (September 1, 2020). http://dx.doi.org/10.33883/jms.v23i3.780.

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I would like to describe our experience in telemedicine for the provision of health care in the Northern Territory of Australia and its relevance for the state of Jammu and Kashmir. Northern Territory is a large landmass spread over 1.4 million square kilometers with a population of only 250,000. Major healthcare facilities are located in cities of Darwin and Alice Springs with smaller hospitals in Katherine, Gove, and Tennant Creek. Many small communities are located in remote areas with limited access to health care. We have adopted telemedicine more than a decade ago and gradually scaled up the services which came handy during the latest pandemic due to SARS-CoV-2.

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45

Rattenbury, M. S. "A linked fold-thrust model for the deformation of the Tennant Creek goldfield, northern Australia." Mineralium Deposita 29, no. 3 (July 1994). http://dx.doi.org/10.1007/bf00206873.

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46

"A linked fold-thrust model for the deformation of the Tennant Creek goldfield, northern Australia." International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts 32, no. 7 (October 1995): 306. http://dx.doi.org/10.1016/0148-9062(95)92276-n.

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47

Stolz, A. J., and R. S. Morrison. "Proterozoic igneous activity in the Tennant Creek region, Northern Territory, Australia, and its relationship to Cu-Au-Bi mineralisation." Mineralium Deposita 29, no. 3 (July 1994). http://dx.doi.org/10.1007/bf00206869.

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Zaw, Khin, D. L. Huston, R. R. Large, T. Mernagh, and C. F. Hoffmann. "Microthermometry and geochemistry of fluid inclusions from the Tennant Creek gold-copper deposits: implications for ore deposition and exploration." Mineralium Deposita 29, no. 3 (July 1994). http://dx.doi.org/10.1007/bf00206872.

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49

Zenhäusern, Géraldine, Simon C. Stähler, John F. Clinton, Domenico Giardini, Savas Ceylan, and Raphaël F. Garcia. "Low-Frequency Marsquakes and Where to Find Them: Back Azimuth Determination Using a Polarization Analysis Approach." Bulletin of the Seismological Society of America, May 25, 2022. http://dx.doi.org/10.1785/0120220019.

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ABSTRACT National Aeronautics and Space Administration’s Interior Exploration using Seismic Investigations, Geodesy, and Heat Transport (InSight) mission on Mars continues to record seismic data over 3 yr after landing, and over a thousand marsquakes have been identified, to date. With only a single seismic station, the determination of the epicentral location is far more challenging than on the Earth. The Marsquake Service (MQS) produces seismicity catalogs from data collected by InSight, and provides distance and back azimuth estimates when these can be reliably determined; when both are available, these are combined to provide a location. Currently, MQS does not assign a back azimuth to the vast majority of marsquakes. In this work we develop and apply a polarization analysis method to determine the back azimuth of seismic events from the polarization of observed P- and S-wave arrivals. The method is first applied to synthetic marsquakes and then calibrated using a set of well-located earthquakes that have been recorded in Tennant Creek, Australia. We find that the back azimuth is estimated reliably using our polarization method. The same approach is then used for a set of high-quality marsquakes recorded up to October 2021. We are able to estimate back azimuths for 24 marsquakes, 16 of these without MQS back azimuths. We locate most events to the east of InSight, in the general region of Cerberus Fossae.

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Haren, Matthew T., John Setchell, David L. John, and Mark Daniel. "The impacts of withdrawal and replacement of general practitioner services on aeromedical service trends: a 13-year interrupted time-series study in Tennant Creek, Northern Territory." BMC Health Services Research 15, no. 1 (June 2015). http://dx.doi.org/10.1186/s12913-015-1110-y.

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