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Статті в журналах з теми "Musgrave Province"

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Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 28 січня 2023

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1

Gum, J. C., and E. A. Belousova. "Musgrave Province Reconnaissance Using TerraneChrony™." ASEG Extended Abstracts 2006, no. 1 (December 2006): 1–7. http://dx.doi.org/10.1071/aseg2006ab061.

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2

Wade, B. P., D. E. Kelsey, M. Hand, and K. M. Barovich. "The Musgrave Province: Stitching north, west and south Australia." Precambrian Research 166, no. 1-4 (October 2008): 370–86. http://dx.doi.org/10.1016/j.precamres.2007.05.007.

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3

Soerensen, Camilla, Andy Love, Tim Munday, Carmen Krapf, Adrian Costar, Kent Inverarity, Michael Gogoll, and Mat Gilfedder. "Uncovering the Musgrave Province in South Australia using airborne EM." ASEG Extended Abstracts 2018, no. 1 (December 2018): 1–5. http://dx.doi.org/10.1071/aseg2018abt5_3h.

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4

Carr, Lidena, Russell Korsch, Arthur Mory, Roger Hocking, Sarah Marshall, Ross Costelloe, Josef Holzschuh, and Jenny Maher. "Structural and stratigraphic architecture of Australia's frontier onshore sedimentary basins: the Western Officer and Southern Carnarvon basins, Western Australia." APPEA Journal 52, no. 2 (2012): 670. http://dx.doi.org/10.1071/aj11084.

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During the past five years, the Onshore Energy Security Program, funded by the Australian Government and conducted by Geoscience Australia, in conjunction with state and territory geological surveys, has acquired deep seismic reflection data across several frontier sedimentary basins to stimulate petroleum exploration in onshore Australia. This extended abstract presents data from two seismic lines collected in Western Australia in 2011. The 487 km long Yilgarn-Officer-Musgrave (YOM) seismic line crossed the western Officer Basin in Western Australia, and the 259 km long, Southern Carnarvon Seismic line crossed the Byro Sub-basin of the Southern Carnarvon Basin. The YOM survey imaged the Neoproterozoic to Devonian western Officer Basin, one of Australia's underexplored sedimentary basins with hydrocarbon potential. The survey data will also provide geoscientific knowledge on the architecture of Australia's crust and the relationship between the eastern Yilgarn Craton and the Musgrave Province. The Southern Carnarvon survey imaged the onshore section of the Ordovician to Permian Carnarvon Basin, which offshore is one of Australia's premier petroleum-producing provinces. The Byro Sub-basin is an underexplored depocentre with the potential for both hydrocarbon and geothermal energy. Where the seismic traverse crossed the Byro Sub-basin it imaged two relatively thick half graben, on west dipping bounding faults. Structural and sequence stratigraphic interpretations of the two seismic lines are presented in this extended abstract.

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5

Joly, Aurore, Alan Aitken, Mike Dentith, TC McCuaig, Alok Porwal, Hugh Smithies, Ian Tyler, and Shane Evans. "Architecture and evolution of the West Musgrave Province, and implications for mineral prospectivity." ASEG Extended Abstracts 2012, no. 1 (December 2012): 1–4. http://dx.doi.org/10.1071/aseg2012ab204.

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6

Pollett, Alicia, Stephan Thiel, Betina Bendall, Tom Raimondo, and Martin Hand. "Mapping the Gawler Craton–Musgrave Province interface using integrated heat flow and magnetotellurics." Tectonophysics 756 (April 2019): 43–56. http://dx.doi.org/10.1016/j.tecto.2019.02.017.

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7

Karykowski, Bartosz T., Paul A. Polito, Wolfgang D. Maier, and Jens Gutzmer. "Origin of Cu-Ni-PGE Mineralization at the Manchego Prospect, West Musgrave Province, Western Australia." Economic Geology 110, no. 8 (November 9, 2015): 2063–85. http://dx.doi.org/10.2113/econgeo.110.8.2063.

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8

PERKINS, PHILIP D. "New species (130) of the hyperdiverse aquatic beetle genus Hydraena Kugelann from Papua New Guinea, and a preliminary analysis of areas of endemism (Coleoptera: Hydraenidae)." Zootaxa 2944, no. 1 (June 8, 2011): 1. http://dx.doi.org/10.11646/zootaxa.2944.1.1.

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The Papua New Guinea (PNG) species of the water beetle genus Hydraena Kugelann, 1794, are revised, based on the study of 7,411 databased specimens. The two previously named species are redescribed, and 130 new species are described. The species are placed in 32 species groups. High resolution digital images of all primary types are presented (online version in color), scanning electron micrographs of representative species are given, and geographic distributions are mapped. Male genitalia, representative female terminal abdominal segments and representative spermathecae are illustrated. Papua New Guinea Hydraena species are typically found in sandy/gravelly stream margins, often in association with streamside litter; some species are primarily pond or swamp dwelling, and a few species are usually found in the hygropetric splash zone on stream boulders or on rocks at the margins of waterfalls. The geographic distributions of PNG Hydraena are compared with the Areas of Freshwater Endemism recently proposed by Polhemus and Allen (2007), and found to substantially support those areas. Only one species, H. impercepta Zwick, 1977 is known to be found in both Australia and Papua New Guinea. The probable Australian origins of the PNG hydraenid genera Gymnochthebius and Limnebius are discussed. The origins of just a few species of PNG Hydraena appear to clearly be Australia, and of comparatively recent origin, whereas the origins of the remainder remain problematic because of lack of knowledge of the Hydraena fauna in Papua Province, Indonesia, and islands large and small to the west of New Guinea. No endemic genera of Hydraenidae are currently known for New Guinea, whereas 98% of the known species are endemic. New species of Hydraena are: H. acumena (Eastern Highlands Province: Koma River, tributary of Fio River), H. adelbertensis (Madang Province: Adelbert Mts., below Keki), H. akameku (Madang Province: Akameku–Brahmin, Bismarck Range), H. altapapua (Southern Highlands Province: Sopulkul, 30–35 km NE Mendi), H. ambra (Eastern Highlands Province: Wanitabi Valley, nr. Okapa), H. ambripes (Madang Province: Finisterre Mts., Naho River Valley, Budemu), H. ambroides (Eastern Highlands Province: Wanitabi Valley, nr. Okapa), H. apertista (Madang Province: Finisterre Mts., Lower Naho Valley, Hinggia), H. apexa (Eastern Highlands Province: Okapa), H. aquila (Madang Province: Simbai area), H. aulaarta (Western Highlands Province: Kundum), H. austrobesa (Central Province: nr. Port Moresby, Sogeri Plateau, Musgrave River), H. bacchusi (Eastern Highlands Province: Wanitabi Valley, nr. Okapa), H. balkei (Eastern Highlands Province: Akameku–Brahmin, Bismarck Range), H. bicarinova (Eastern Highlands Province: Wanitabi Valley, nr. Okapa), H. bifunda (Morobe Province: c. 7 mi. Lae–Bulolo road), H. biundulata (Morobe Province: Lae–Bulolo road), H. brahman (Madang Province: Ramu Valley, 4.5 km N Brahman), H. bubulla (Madang Province: Akameku–Brahmin, Bismarck Range), H. buloba (Morobe Province: Herzog Mts., Wagau), H. buquintana (Western Highlands Province: Mt. Hagen town area), H. carinocisiva (Eastern Highlands Province: Aiyura), H. carmellita (Morobe Province: Herzog Mts., Wagau), H. cavifrons (Madang Province: Ramu Valley, 4.5 km N Brahman), H. cheesmanae (Central Province: Kokoda), H. clarinis (Madang Province: Sepik Ramu Basin, Kojé Creek), H. colorata (Morobe Province: 5 miles W of Lae, Buins Creek), H. confluenta (Eastern Highlands Province: Umg. [=environs of] Kainantu, Onerunka), H. copulata (Gulf Province: Marawaka, Mala), H. cunicula (Madang Province: Akameku–Brahmin, Bismarck Range), H. decepta (Eastern Highlands Province: Okapa), H. diadema (Eastern Highlands Province: Purosa Valley, nr. Okapa), H. dudgeoni (Madang Province: Sepik Ramu Basin, Kojé Creek), H. einsteini (Central Province: Port Moresby–Brown River road), H. essentia (Eastern Highlands Province: Sepik River Basin, stream beside milestone labelled G-99), H. exhalista (Gulf Province: Marawaka, Mala), H. fasciata (Morobe Province: Herzog Mts., Wagau), H. fascinata (Madang Province: Finisterre Mts., Naho River Valley, nr. Moro), H. fasciolata (Madang Province: Madang, Ohu Village), H. fasciopaca (Madang Province: Keki, Adelbert Mts.), H. fenestella (Morobe Province: Lae-Bulolo road), H. foliobba (Morobe Province: Herzog Mts., Wagau), H. formosopala (East Sepik Province: Prince Alexander Mts., Wewak), H. funda (Central Province: Moitaka, 7 miles N of Port Moresby), H. fundacta (Madang Province: Adelbert Mts., Sewan–Keki), H. fundapta (Central Province: Port Moresby–Brown River road), H. fundarca (Eastern Highlands Province: Okapa), H. fundextra (Morobe Province: Markham Valley, Gusap), H. galea (Eastern Highlands Province: Akameku–Brahmin, Bismarck Range, 700 m), H. herzogestella (Morobe Province: Herzog Mts., Bundun), H. hornabrooki (East Sepik Province: Sepik, main river), H. huonica (Madang Province: Kewensa, Finisterre Range, Yupna, Huon Peninsula), H. ibalimi (Sandaun Province: Mianmin), H. idema (Eastern Highlands Province: Umg. [=environs of] Onerunka, Ramu River), H. impala (Central Province: nr. Port Moresby, Sogeri Plateau, Musgrave River), H. incisiva (Morobe Province: Herzog Mts., Wagau), H. incista (Western Highlands Province: Simbai, Kairong River), H. infoveola (Gulf Province: Marawaka, Mala), H. inhalista (Madang Province: Finisterre Mts., Naho River Valley, Damanti), H. inplacopaca (Eastern Highlands Province: Waisa, nr. Okapa), H. insandalia (Eastern Highlands Province: Headwaters of Fio River, 0.5 km downstream of river crossing on Herowana/Oke Lookout path, ca. 4.5 km N of Herowana airstrip), H. intensa (Morobe Province: Lae–Bulolo road), H. johncoltranei (National Capital District, Varirata NP), H. jubilata (Madang Province: Finisterre Mts., Naho River Valley, Budemu), H. koje (Madang Province: Sepik Ramu Basin, Kojé Creek), H. koma (Eastern Highlands Province: Koma River, tributary of Fio River, 100 m downstream of rattan bridge crossing, ca. 3.8 km S by E of Herowana airstrip), H. labropaca (Central Province: nr. Port Moresby, Sogeri Plateau, Musgrave River), H. lassulipes (Morobe Province: Herzog Mts., Wagau), H. limbobesa (Gulf Province: Marawaka, near Ande), H. maculopala (Madang Province: Madang, Ohu Village), H. manulea (Morobe Province: Lae, Buins Creek), H. manuloides (Central Province: Port Moresby–Brown River road), H. marawaka (Gulf Province: Marawaka, Mala), H. mercuriala (Sandaun Province: May River), H. mianminica (Sandaun Province:May River), H. nanocolorata (Madang Province: Sepik Ramu Basin, Kojé Creek), H. nanopala (Madang Province: Sepik Ramu Basin, Kojé Creek), H. nitidimenta (Eastern Highlands Province: Koma River, tributary of Fio River, at rattan bridge crossing, ca. 2.6 km N by W of Herowana airstrip), H. okapa (Eastern Highlands Province: Wanitabi Valley, nr. Okapa), H. ollopa (Western Highlands Province: Kundum), H. otiarca (Morobe Province: Herzog Mts., Wagau, Snake River), H. owenobesa (Morobe Province: ca. 10 km S Garaina Saureri), H. pacificica (Morobe Province: Huon Pen., Kwapsanek), H. pala (Morobe Province: Lae–Bulolo road, Gurakor Creek), H. palamita (Central Province: nr. Port Moresby, Sogeri Plateau, Musgrave River), H. paxillipes (Morobe Province: Lae–Bulolo road, Patep Creek), H. pectenata (Madang Province: Finisterre Mts., Naho River Valley, Damanti), H. pegopyga (Madang Province: Ramu Valley, 3 km N Brahman), H. penultimata (Sandaun Province: May River), H. perpunctata (Madang Province: Sepik Ramu Basin, Kojé Creek), H. pertransversa (Eastern Highlands Province: Clear stream, summit of Kassem Pass at forest level), H. phainops (Morobe Province: Lae–Bulolo road, Patep Creek), H. photogenica (Eastern Highlands Province: Goroka, Mt. Gahavisuka), H. picula (Eastern Highlands Province: Goroka, Daulo Pass), H. pilulambra (Eastern Highlands Province: Clear stream, summit of Kassem Pass at forest level), H. pluralticola (Morobe Province: c. 7 miles Lae–Bulolo road), H. processa (Morobe Province: Herzog Mts., Wagau), H. quadriplumipes (Madang Province: Aiome area), H. quintana (Morobe Province: Markham Valley, Lae–Kainantu road, Erap R), H. ramuensis (Madang Province: Ramu Valley, 6 km N Brahman), H. ramuquintana (Madang Province: Ramu Valley, 6 km N Brahman), H. receptiva (Morobe Province: Lae–Bulolo road), H. remulipes (Morobe Province: Herzog Mts., Wagau), H. reticulobesa (Madang Province: Finisterre Mts., Naho River Valley, Moro), H. sagatai (Sandaun Province: Abau River), H. saluta (Madang Province: Finisterre Mts., Naho River Valley, Damanti), H. sepikramuensis (Madang Province: Ramu Valley, Sare River, 4 km N Brahman), H. sexarcuata (Eastern Highlands Province: Akameku–Brahmin, Bismarck Range), H. sexsuprema (Madang Province: Finisterre Mts., Naho River Valley, Damanti), H. spinobesa (Madang Province: Finisterre Mts., Naho River Valley, Budemu), H. striolata (Oro Province: Northern District, Tanbugal Afore village), H. supersexa (Eastern Highlands Province: Okapa), H. supina (Eastern Highlands Province: Wanitabi Valley, nr. Okapa), H. tarsotricha (Morobe Province: Herzog Mts., Wagau, Snake River), H. tetana (Eastern Highlands Province: Okapa), H. thola (Central Province: Port Moresby– Brown River road), H. tholasoris (Morobe Province: Markham Valley, Gusap, c. 90 miles NW of Lae), H. thumbelina (Madang Province: Finisterre Mts., Naho River Valley, Damanti), H. thumbelipes (Sandaun Province: Mianmin), H. tibiopaca (Morobe Province: ridge between Aseki–Menyamya), H. torosopala (Madang Province: Keki, Adelbert Mts.), H. torricellica (Morobe Province: Torricelli Mts., village below Sibilanga Stn.), H. transvallis (Madang Province: Finisterre Mts., Naho River Valley, Damanti), H. trichotarsa (Morobe Province: Lae–Bulolo road), H. tricosipes (Morobe Province: Herzog Mts., Wagau), H. tritropis (Madang Province: Sepik Ramu Basin, Kojé Creek), H. tritutela (Morobe Province: ca. 10 km S Garaina Saureri), H. ulna (Morobe Province: Herzog Mts., Wagau), H. variopaca (Eastern Highlands Province: Wanitabi Valley, nr. Okapa), H. velvetina (Eastern Highlands Province: Purosa Valley, nr. Okapa).

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9

Schwarz, A., and S. Constable. "Structural and geochemical characteristics of the Ngunala Intrusion of the Giles Complex, Musgrave Province, South Australia." Applied Earth Science 116, no. 4 (December 2007): 201–14. http://dx.doi.org/10.1179/174327507x272003.

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10

Smithies, R. H., C. L. Kirkland, F. J. Korhonen, A. R. A. Aitken, H. M. Howard, W. D. Maier, M. T. D. Wingate, R. Quentin de Gromard, and K. Gessner. "The Mesoproterozoic thermal evolution of the Musgrave Province in central Australia — Plume vs. the geological record." Gondwana Research 27, no. 4 (June 2015): 1419–29. http://dx.doi.org/10.1016/j.gr.2013.12.014.

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11

Kirkland, Christopher L., R. Hugh Smithies, Ailsa J. Woodhouse, Heather M. Howard, Michael T. D. Wingate, Elena A. Belousova, John B. Cliff, Rosanna C. Murphy, and Catherine V. Spaggiari. "Constraints and deception in the isotopic record; the crustal evolution of the west Musgrave Province, central Australia." Gondwana Research 23, no. 2 (March 2013): 759–81. http://dx.doi.org/10.1016/j.gr.2012.06.001.

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12

Glorie, Stijn, Kate Agostino, Rian Dutch, Mark Pawley, James Hall, Martin Danišík, Noreen J. Evans, and Alan S. Collins. "Thermal history and differential exhumation across the Eastern Musgrave Province, South Australia: Insights from low-temperature thermochronology." Tectonophysics 703-704 (April 2017): 23–41. http://dx.doi.org/10.1016/j.tecto.2017.03.003.

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13

Carr, Lidena, Russell Korsch, Wolfgang Preiss, Sandra Menpes, Josef Holzschuh, and Ross Costelloe. "Structural and stratigraphic architecture of Australia's frontier onshore sedimentary basins: the Arckaringa, Officer, Amadeus, and Georgina basins." APPEA Journal 51, no. 2 (2011): 703. http://dx.doi.org/10.1071/aj10083.

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The Onshore Energy Security Program—funded by the Australian Government and conducted by Geoscience Australia—has acquired deep seismic reflection data in conjunction with state and territory geological surveys, across several frontier sedimentary basins to stimulate petroleum exploration in onshore Australia. Here, we present data from two seismic lines collected in SA and NT. Seismic line 08GA-OM1 crossed the Arckaringa and Officer basins in SA and the southern-most Amadeus Basin in NT. Seismic line 09GA-GA1 crossed the northeastern part of the Amadeus Basin and the complete width of the southern Georgina Basin in NT. Structural and sequence stratigraphic interpretations of the seismic lines will be presented here, followed by an assessment of the petroleum potential of the basins. Seismic line 08GA-OM1 also crosses the Neoproterozoic to Devonian eastern Officer Basin. The basin is structurally complex in this area, being dominated by south-directed thrust faults and fault-related folds—providing potential for underthrust petroleum plays. The northern margin of the basin is overthrust to the south by the Mesoproterozoic Musgrave Province. To the north, the Moorilyanna Trough of the Officer Basin is a major depocentre of up to 7,000 m deep. Both seismic lines cross parts of the eastern Amadeus Basin. Seismic line 08GA-OM1 shows that the southern margin of the basin is overthrust to the north by the Musgrave Province with the main movement during the Petermann Orogeny. In the northeast, seismic line 09GA-GA1 crosses two parts of the basin separated by the Paleoproteroozic to Mesoproterozoic Casey Inlier (part of the Arunta Region). The northern margin of the basin is imaged seismically as a southward-verging, thinned-skinned thrust belt, showing considerable structural thickening of the stratigraphic succession. Seismic line 09GA-GA1 was positioned to cross that part of the southern Georgina Basin that was considered previously to be in the oil window. Here, the basin has a complex southern margin, with Neoproterozoic stratigraphy being thrust interleaved with basement rocks of the Arunta Region. The main part of the basin, containing a Neoproterozoic to Devonian succession, is asymmetric, thinning to the north where it overlies the Paleoproterozoic Davenport Province. The well, Phillip–2, drilled adjacent to the seismic line, intersected basement at a depth of 1,489 m, and has been used to map the stratigraphic sequences across the basin.

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14

Smithies, R. H., H. M. Howard, P. M. Evins, C. L. Kirkland, D. E. Kelsey, M. Hand, M. T. D. Wingate, A. S. Collins, and E. Belousova. "High-Temperature Granite Magmatism, Crust–Mantle Interaction and the Mesoproterozoic Intracontinental Evolution of the Musgrave Province, Central Australia." Journal of Petrology 52, no. 5 (April 7, 2011): 931–58. http://dx.doi.org/10.1093/petrology/egr010.

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15

AITKEN, A., and P. BETTS. "Constraints on the Proterozoic supercontinent cycle from the structural evolution of the south-central Musgrave Province, central Australia." Precambrian Research 168, no. 3-4 (February 2009): 284–300. http://dx.doi.org/10.1016/j.precamres.2008.10.006.

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16

Stamoulis, Vicki. "A Case Study Using Radiometrics as a First Pass Technique to Geological Mapping in the Musgrave Province in South Australia." ASEG Extended Abstracts 2004, no. 1 (December 2004): 1–4. http://dx.doi.org/10.1071/aseg2004ab139.

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17

Evins, Paul M., R. Hugh Smithies, Heather M. Howard, Christopher L. Kirkland, Michael T. D. Wingate, and Simon Bodorkos. "Devil in the detail; The 1150–1000Ma magmatic and structural evolution of the Ngaanyatjarra Rift, west Musgrave Province, Central Australia." Precambrian Research 183, no. 3 (December 2010): 572–88. http://dx.doi.org/10.1016/j.precamres.2010.02.011.

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18

Aitken, Alan R. A., and Peter G. Betts. "Multi-scale integrated structural and aeromagnetic analysis to guide tectonic models: An example from the eastern Musgrave Province, Central Australia." Tectonophysics 476, no. 3-4 (October 2009): 418–35. http://dx.doi.org/10.1016/j.tecto.2009.07.007.

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19

Grguric, B. A., Z. Seat, J. M. A. Hronsky, and G. J. Miles. "The Succoth Cu-Ni-Pd deposit: A new taxite-hosted magmatic sulphide system in the West Musgrave Province, Western Australia." Ore Geology Reviews 92 (January 2018): 397–415. http://dx.doi.org/10.1016/j.oregeorev.2017.11.026.

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20

Aitken, A. R. A., P. G. Betts, B. F. Schaefer, and S. E. Rye. "Assessing uncertainty in the integration of aeromagnetic data and structural observations in the Deering Hills region of the Musgrave Province." Australian Journal of Earth Sciences 55, no. 8 (December 2008): 1127–38. http://dx.doi.org/10.1080/08120090802266600.

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21

Karykowski, Bartosz T., Paul A. Polito, Wolfgang D. Maier, Jens Gutzmer, and Joachim Krause. "New insights into the petrogenesis of the Jameson Range layered intrusion and associated Fe-Ti-P-V-PGE-Au mineralisation, West Musgrave Province, Western Australia." Mineralium Deposita 52, no. 2 (May 10, 2016): 233–55. http://dx.doi.org/10.1007/s00126-016-0655-y.

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22

Donnellan, Nigel, Alfredo Camacho, Roland Maas, and Richard C. Price. "Mantle Upwelling or Plume Activity on the Periphery of the Warakurna LIP: Evidence from the Geochemistry and Petrogenesis of the Alcurra Dolerite in the Eastern Musgrave Province." Journal of Petrology 60, no. 2 (December 19, 2018): 301–27. http://dx.doi.org/10.1093/petrology/egy113.

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23

Bache, Francois, Paul Walshe, Juergen Gusterhuber, Sandra Menpes, Mattilda Sheridan, Sergey Vlasov, and Lance Holmes. "Exploration of the south-eastern part of the Frontier Amadeus Basin, Northern Territory, Australia." APPEA Journal 58, no. 1 (2018): 190. http://dx.doi.org/10.1071/aj17221.

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Анотація:

The Neoproterozoic to Late Paleozoic-aged Amadeus Basin is a large (~170 000 km2) east–west-trending basin, bounded to the south by the Musgrave Province and to the north by the Arunta Block of the Northern Territory. Commercial oil and gas production is established in the northern part of the basin but the southern part is still a frontier exploration area. Vintage and new seismic reflection data have been used with well data along the south-eastern Amadeus Basin to construct a new structural and depositional model. Three major phases of deformation controlling deposition have been identified. The first phase is characterised by a SW–NE trending structural fabric and is thought to be older than the deposition of the first sediments identified above basement (Heavitree and Bitter Springs formations). The second phase corresponds to the Petermann Orogeny (580–540 Ma) and trends in a NW–SE orientation. The third phase is the Alice Springs Orogeny (450–300 Ma) and is oriented W–E to WNW–ESE in this part of the basin. This tectono-stratigraphic model involving three distinct phases of deformation potentially explains several critical observations: the lack of Heavitree reservoir at Mt Kitty-1, limited salt movements before the Petermann Orogeny (~300 Ma after its deposition) and salt-involved structures that can be either capped by the Petermann Unconformity and overlying Cambrian to Devonian sediments, or can reach the present day surface. Finally, this model, along with availability of good quality seismic data, opens new perspectives for the hydrocarbon exploration of the Amadeus Basin. Each of the tectonic phases impacts the primary petroleum system and underpins play-based exploration.

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Medlin, C. C., S. M. Jowitt, R. A. F. Cas, R. H. Smithies, C. L. Kirkland, R. A. Maas, M. Raveggi, H. M. Howard, and M. T. D. Wingate. "Petrogenesis of the A-type, Mesoproterozoic Intra-caldera Rheomorphic Kathleen Ignimbrite and Comagmatic Rowland Suite Intrusions, West Musgrave Province, Central Australia: Products of Extreme Fractional Crystallization in a Failed Rift Setting." Journal of Petrology 56, no. 3 (March 1, 2015): 493–525. http://dx.doi.org/10.1093/petrology/egv007.

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Williamson, Tom, Peter Clark, A. G. Hopkins, Rab Houston, Gillian Rose, Stuart Woolf, Adrian Rifkin, et al. "Review of Culture and Cultivation in Early Modern England: Writing and the Land, by Michael Leslie and Timothy Raylor; Death and the Metropolis: Studies in the Demographic History of London 1670-1830, by John Landers; Capitalism, Culture and Decline in Britain, 1750-1990, by W. D. Rubinstein; Subverting Scotland's Past: Scottish Whig Historians and the Creation of an Anglo-British Identity, 1689-c.1830, by Colin Kidd; Outsiders: Class, Gender and Nation, by Dorothy Thompson; Land and Economy in Baroque Italy: Valpolicella, 1630-1797, by Peter Musgrave; The Seduction of the Mediterranean: Writing, Art, and Homosexual Fantasy, by Robert Aldrich; Geographical Inquiry and American Historical Problems, by Carville Earle; Historical Atlas of Canada, Vol. II: The Land Transformed, 1880-1891, by R. Louis Gentilcore; In the Absence of Towns: Settlement and Country Trade in Southside Virginia, 1730-1800, by Charles J. Farmer; North American Cattle-Ranching Frontiers: Origins, Diffusion, and Differentiation, by Terry G. Jordan; From Wooden Ploughs to Welfare: Why Indian Policy Failed in the Prairie Provinces, by Helen Buckley; Russian Refuge: Religion, Migration, and Settlement on the North American Pacific Rim, by Susan Wiley Hardwick; La Paz de Dios y del Rey: la Conquista de la Selva Lacandona, 1525-1821. Oro Verde: la Conquista de la Selva Lacandona por los Maderos Tabasqueños, 1822-1949, by Jan de Vos; Haciendas and 'Ayllus': Rural Society in the Bolivian Andes in the Eighteenth and Nineteenth Centuries, by Herbert S. Klein; Ideology and Landscape in Historical Perspective: Essays on the Meanings of Some Places in the Past, by A. R.H. Baker and G. Bilger; The Early Modern World-System in Georgraphical Perspectie, by Hans-Jurgen Nitz; European Expansion and Migration: Essays on the Intercontinental Migration from Africa, Asia and Europe, by P. C. Emmer and M. Mörner; Mass Migration in Europe: The Legacy and the Future, by Russell King; Asia in the Making of Europe, Volume III: A Century of Advance Book 1: Trade, Missions, Literature; Book 2: South Asia; Book 3: Southeast Asia; Book 4: East Asia, by Donald F. Lach and Edwin J. Van Kley; The Remaking of Istanbul: Portrait of an Ottoman City in the Nineteenth Century, by Zeynep Çelik; The Shona and Their Neighbours, by David Beach and Imperial Eyes: Travel Writing and Transculturation, by Mary Louise Pratt." Journal of Historical Geography 20, no. 4 (October 1994): 465–98. http://dx.doi.org/10.1006/jhge.1994.1037.

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Thiel, Stephan, Bruce R. Goleby, Mark J. Pawley, and Graham Heinson. "AusLAMP 3D MT imaging of an intracontinental deformation zone, Musgrave Province, Central Australia." Earth, Planets and Space 72, no. 1 (July 11, 2020). http://dx.doi.org/10.1186/s40623-020-01223-0.

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Aitken, Alan R. A., Peter G. Betts, Roberto F. Weinberg, and Daniel Gray. "Constrained potential field modeling of the crustal architecture of the Musgrave Province in central Australia: Evidence for lithospheric strengthening due to crust-mantle boundary uplift." Journal of Geophysical Research 114, B12 (December 23, 2009). http://dx.doi.org/10.1029/2008jb006194.

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Ebhota, Williams S., and Pavel Y. Tabakov. "Assessment and performance analysis of roof-mounted crystalline stand-alone photovoltaic (SAPV) system at selected sites in South Africa." Bulletin of the National Research Centre 46, no. 1 (August 27, 2022). http://dx.doi.org/10.1186/s42269-022-00929-3.

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Abstract Background Technology is deployed to take the advantage of the ultimate energy from the sun (solar energy) to be used as heat or clean electricity. This energy is classified as “sustainable energy” or “renewable energy” because it requires a short period to naturally replenish the used energy. The application of solar energy involves the conversion of the natural energy resource into a usable form, either as heat or as electricity. The device consists of solar cells made from semiconductor materials, such as silicon, cadmium telluride, gallium arsenide, and so on. Solar potential is both location- and climate-dependent; it is characterised by low energy intensity and intermittency, which limit its application; an improvement in photovoltaic (PV) system performance will facilitate more deployment of the clean electricity system. Therefore, this study provides PV potential and system information required for reliable and optimised solar PV systems at chosen locations. This work uses a 5-stage solar PV system assessment and system performance evaluation utilising Solargis Prospect software. The PV potential and system performance of nine selected site locations in South Africa was conducted using this method. The nine PV site locations are Bloemfontein (Free State), Germiston (Gauteng), Mahikeng (North-West), Mbombela (Mpumalanga), Musgrave (Kwazulu-Natal), Musina (Limpopo), Port Nolloth (Northern Cape), Port Elizabeth (Eastern Cape), and Worcester (Western Cape). Result The results of the study were categorised into PV meteorological and system performance parameters as follows. Photovoltaic meteorological parameters—the site in Mahikeng has the highest global horizontal irradiance (GHI), 2156 kWh/m2, and a corresponding specific PV power output (1819.3 kWh/kWp), closely followed by Bloemfontein (2111.5 kWh/m2, 1819.4 kWh/kWp) and Port Nolloth (2003.2 kWh/m2, 1820.5 kWh/kWp). The lowest GHI (1645.1 kWh/m2) and specific PV power output (1436.6 kWh/kWp) were recorded in Musgrave. Photovoltaic system performance parameters—the range of performance ratio (PR) between 75.8 and 77.7% was reported across the nine sites. This ratio met the acceptable benchmark of PR. The highest specific PV power output loss, 118.8 kWh/kWp, was obtained at sites in Bloemfontein, Mahikeng, and Port Nolloth, while the lowest, 93.8 kWh/kWp, was in Musgrave. Conclusions The results of the solar PV potential assessment and the evaluation of PV systems performance in the chosen sites across the nine provinces of South Africa show huge PV potential and energy yield. From the results, it was observed that the range of the yearly average of: (1) GHI among the sites is 1645.1–2156 kWh/m2; (2) direct normal irradiation among the sites is 1785.3–2559.3 kWh/m2; (3) diffuse horizontal irradiation among the sites is 512.5–686kWh/m2; (4) global tilted irradiation among the sites is 1849.2–2397.1 kWh/m2; (5) the temperature (TEMP) among the sites is 16–23 °C; (6) specific PV power output (PVOUT specific) among the sites is 1436.6–1820.5 kWh/kWp; (7) total PV power output (PVOUT total) among the sites is 14.366–2397.1 MWh; and (8) the performance ratio among the sites is 75.8–77.7%. Based on the solar resource and performance results of the PV system obtained, the deployment of monocrystalline solar PV technology in all the considered sites across South Africa is technically viable.

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