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Статті в журналах з теми "Arunta"

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Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 28 січня 2023

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1

Passchier, Cees, and Ben Goscombe. "Pseudo-boudins in Pegmatite, Arunta, Australia." Journal of Structural Geology 30, no. 3 (March 2008): 273. http://dx.doi.org/10.1016/j.jsg.2007.07.006.

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2

Andrews, JA, and IA Rose. "Glycine max (L.) Merr. (soybean) cv. Arunta." Australian Journal of Experimental Agriculture 36, no. 6 (1996): 761. http://dx.doi.org/10.1071/ea9960761.

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3

Zavaleta Villanueva, Jesús Raúl, Giovani Alonso Reátegui García, and María Etelvina Duarte Lizarzaburu. "Caracterización de agregados de cinco canteras de la provincia de Tacna y su optimación de uso en obras de construcción." INGENIERÍA INVESTIGA 2, no. 2 (December 24, 2020): 340–56. http://dx.doi.org/10.47796/ing.v2i2.410.

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Анотація:

La caracterización de los agregados de las cinco principales canteras de la provincia de Tacna que permita optimizar su uso en obras de construcción. Estudio de tipo cuantitativo, explicativa y descriptiva donde se determinó las propiedades físicas del agregado realizando los ensayos según los parámetros establecidos en la Norma Técnica Peruana NTP 400.037. Se elaboró el diseño de mezcla según el método ACI para f’c= 210 kg/cm2. Posterior a ello se realizaron nueve testigos de concreto, para cada de las siguientes canteras; Arunta, Magollo, Arunta II, Jonas I y la propuesta para explotación ubicada en el distrito de Sama, a edades de 7, 14 y 28 días. Al realizar el ensayo de compresión se observó que el concreto realizado con los diferentes agregados cumple con los parámetros establecidos por la Norma Técnica Peruana. La cantera propuesta ubicada en el distrito de Sama, mostró óptimas condiciones para la explotación de agregados, ya que al realizar el ensayo de compresión obtuvo una resistencia de 319,61 kg/cm2 a 28 días.

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4

Moulds, M. S. "A review of the tribe Thophini Distant (Hemiptera: Cicadoidea: Cicadidae) with the description of a new species of Thopha Amyot & Serville." Insect Systematics & Evolution 32, no. 2 (2001): 195–203. http://dx.doi.org/10.1163/187631201x00155.

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AbstractThe tribe Thophini is redefined. It includes only the genera Thopha Amyot & Serville and Arunta Distant, both of which are endemic to Australia. The Caribbean genus Uhleroides Distant is excluded from the Thophini and is transferred to the Zammarini Distant. A new species, Thopha emmotti, is described from western Queensland and a key to the species of Thopha Amyot & Serville is provided.

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5

Goleby, B. R., C. Wright, and B. L. N. Kennett. "Preliminary deep reflection studies in the Arunta Block, Central Australia." Geophysical Journal International 89, no. 1 (April 1987): 437–42. http://dx.doi.org/10.1111/j.1365-246x.1987.tb04443.x.

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6

Warren, R. G., and B. J. Hensen. "Peraluminous sapphirine from the Aileron district, Arunta Block, central Australia." Mineralogical Magazine 51, no. 361 (September 1987): 409–15. http://dx.doi.org/10.1180/minmag.1987.051.361.07.

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AbstractSpecimens collected from a small lens of phlogopite-rich rock in the granulite-facies terrain of the Arunta Block, central Australia, have unusual bulk compositions and mineral assemblages. One sample consists of phlogopite enclosing blue spinel (mg 96) with minute granules of corundum and sapphirine at the margins; a second of phlogopite enclosing porphyroblasts of corundum and peraluminous sapphirine. In the first the sapphirine is close to the 7 : 9 : 3 composition; in the other it is markedly peraluminous, e.g. (Mg1.628Fe0.028)Al4.714Si0.636O10, intermediate between the 7 : 9 : 3 and 3 : 5 : 1 members. The texture suggests that this sapphirine is a stable phase in equilibrium with eastonitic phlogopite and corundum. The very potassic, very magnesian bulk composition of the rocks is attributed to potassium metasomatism of a protolith consisting of magnesian chlorite and quartz.

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7

Arnold, J. "Metamorphic events in the eastern Arunta Inlier, Part 1. Metamorphic petrology." Precambrian Research 71, no. 1-4 (February 1995): 183–205. http://dx.doi.org/10.1016/0301-9268(94)00061-u.

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8

Collins, W. "Geochronological constraints on orogenic events in the Arunta Inlier: a review." Precambrian Research 71, no. 1-4 (February 1995): 315–46. http://dx.doi.org/10.1016/0301-9268(94)00067-2.

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9

Collins, W. J., and C. Teyssier. "Crustal scale ductile fault systems in the Arunta Inlier, central Australia." Tectonophysics 158, no. 1-4 (February 1989): 49–66. http://dx.doi.org/10.1016/0040-1951(89)90314-4.

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10

Collins, W. J., and C. Teyssier. "Crustal ductile fault systems in the Arunta Inlier, central Australia—Reply." Tectonophysics 158, no. 1-4 (February 1989): 70–73. http://dx.doi.org/10.1016/0040-1951(89)90316-8.

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11

Vry, J. K. "Boron-free kornerupine from the Reynolds Range, Arunta Block, central Australia." Mineralogical Magazine 58, no. 390 (March 1994): 27–37. http://dx.doi.org/10.1180/minmag.1994.058.390.03.

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AbstractNearly boron-free kornerupine is locally abundant in pods or lenses of coarse-grained, non-foliated, Mg- and Al-rich rocks that occur at high metamorphic grades in early Proterozoic metapelitic rocks from the Reynolds Range, Northern Territory, Australia. This is the third reported occurrence of boron-free kornerupine worldwide. The samples consist almost entirely of coarse-grained kornerupine and its breakdown products sapphirine, cordierite, and gedrite or orthopyroxene. The kornerupine contains only 0.45 wt.% B2O3, corresponding to 0.098 B atoms per 22 (O, OH), and closely approximates 11:10:11 in terms of molar ratios of (MgO + FeOtotal):Al2O3:SiO2, with XMg = Mg/(Mg + Fetotal) = 0.874. The unusual textures and bulk compositions of the rocks in the pods are interpreted to have resulted from metasomatism and high-grade metamorphism (750 to 800° and ∼ 4.5 kbar) of precursors that may have included sedimentary Mg-rich clays. Rocks containing boron-poor, and relatively boronrich kornerupine (2.18 wt.% B2O3; XMg = 0.892) are separated in outcrop by as little as 10 m of the foliated cordierite-quartzite country rock and other rock types, suggesting that the compositions or amounts of the metasomatic fluids varied on a local scale.

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12

Kirkby, Alison, and Jingming Duan. "The conductivity structure of the Georgina-Arunta region from magnetotelluric data." ASEG Extended Abstracts 2018, no. 1 (December 2018): 1–5. http://dx.doi.org/10.1071/aseg2018abp053.

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13

Greenhalgh, S. A., Cedric Wright, Bruce Goleby, and Sugiharto Soleman. "Seismic anisotrdpy in granuulte facies rocks of the Arunta Block, central Australia." Geophysical Research Letters 17, no. 10 (September 1990): 1513–16. http://dx.doi.org/10.1029/gl017i010p01513.

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14

Foden, J. "Metamorphic events in the eastern Arunta Inlier, Part 2. Nd_Sr_Ar isotopic constraints." Precambrian Research 71, no. 1-4 (February 1995): 207–27. http://dx.doi.org/10.1016/0301-9268(94)00062-v.

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15

Dunlap, W. "Paleozoic deformation and isotopic disturbance in the southeastern Arunta Block, central Australia." Precambrian Research 71, no. 1-4 (February 1995): 229–50. http://dx.doi.org/10.1016/0301-9268(94)00063-w.

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16

Ding, P., and P. R. James. "Crustal scale ductile fault systems in the Arunta Inlier, central Australia—Discussion." Tectonophysics 158, no. 1-4 (February 1989): 67–69. http://dx.doi.org/10.1016/0040-1951(89)90315-6.

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17

Sivell, W. J., J. D. Foden, and R. W. Lawrence. "The Entire anorthositic gneiss, eastern Arunta Inlier, Central Australia: Geochemistry and petrogenesis." Australian Journal of Earth Sciences 32, no. 4 (December 1985): 449–65. http://dx.doi.org/10.1080/08120098508729343.

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18

GOSCOMBE, B. "High-Grade Reworking of Central Australian Granulites: Metamorphic Evolution of the Arunta Complex." Journal of Petrology 33, no. 4 (August 1, 1992): 917–62. http://dx.doi.org/10.1093/petrology/33.4.917.

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19

TEYSSIER, C., C. AMRI, and B. HOBBS. "South Arunta Block: the internal zones of a Proterozoic overthrust in central Australia." Precambrian Research 40-41 (October 1988): 157–73. http://dx.doi.org/10.1016/0301-9268(88)90066-6.

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20

Young, D. "U_Pb zircon dating of tectonomagmatic events in the northern Arunta Inlier, central Australia." Precambrian Research 71, no. 1-4 (February 1995): 45–68. http://dx.doi.org/10.1016/0301-9268(94)00055-v.

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21

Greenhalgh, S. A., S. Sugiharto, C. Wright, and B. R. Goleby. "Tomographic reconstruction of upper crustal velocity variations in the Arunta Block, central Australia." Tectonophysics 173, no. 1-4 (February 1990): 63–72. http://dx.doi.org/10.1016/0040-1951(90)90204-l.

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22

Mawby, Hand, and Foden. "Sm-Nd evidence for high-grade Ordovician metamorphism in the Arunta Block, central Australia." Journal of Metamorphic Geology 17, no. 6 (November 1999): 653–68. http://dx.doi.org/10.1046/j.1525-1314.1999.00224.x.

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23

Anderson, J. R., D. E. Kelsey, M. Hand, and W. J. Collins. "Conductively driven, high-thermal gradient metamorphism in the Anmatjira Range, Arunta region, central Australia." Journal of Metamorphic Geology 31, no. 9 (October 18, 2013): 1003–26. http://dx.doi.org/10.1111/jmg.12054.

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24

WARREN, R. G., and R. D. SHAW. "Volcanogenic Cu?Pb?Zn bodies in granulites of the central Arunta Block, central Australia." Journal of Metamorphic Geology 3, no. 4 (December 1985): 481–99. http://dx.doi.org/10.1111/j.1525-1314.1985.tb00331.x.

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25

DIENER, J. F. A., R. W. WHITE, and R. POWELL. "Granulite facies metamorphism and subsolidus fluid-absent reworking, Strangways Range, Arunta Block, central Australia." Journal of Metamorphic Geology 26, no. 6 (August 2008): 603–22. http://dx.doi.org/10.1111/j.1525-1314.2008.00782.x.

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26

Obee, H. K., and S. H. White. "Faults and associated fault rocks of the Southern Arunta block, Alice Springs, Central Australia." Journal of Structural Geology 7, no. 6 (January 1985): 701–12. http://dx.doi.org/10.1016/0191-8141(85)90145-2.

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27

Rickard, M. J. "Central Australia (Arunta Complex and Amadeus Basin)—history of work and outline of problems." Tectonophysics 158, no. 1-4 (February 1989): 1–4. http://dx.doi.org/10.1016/0040-1951(89)90311-9.

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28

Whiting, T. H. "Magnetic Mineral Petrogenesis, Rock Magnetism and Aeromagnetic Response in the Eastern Arunta Inlier, Northern Territory." Exploration Geophysics 19, no. 1-2 (March 1988): 377–83. http://dx.doi.org/10.1071/eg988377.

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29

Kirkby, Alison, and Jingming Duan. "Crustal Structure of the Eastern Arunta Region, Central Australia, From Magnetotelluric, Seismic, and Magnetic Data." Journal of Geophysical Research: Solid Earth 124, no. 8 (August 2019): 9395–414. http://dx.doi.org/10.1029/2018jb016223.

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30

Goleby, B. R., C. Wright, C. D. N. Collins, and B. L. N. Kennett. "Seismic reflection and refraction profiling across the Arunta Block and the Ngalia and Amadeus Basins." Australian Journal of Earth Sciences 35, no. 3 (September 1988): 275–94. http://dx.doi.org/10.1080/08120098808729447.

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31

Morrissey, L. J., M. Hand, T. Raimondo, and D. E. Kelsey. "Long-lived high-T , low-P granulite facies metamorphism in the Arunta Region, central Australia." Journal of Metamorphic Geology 32, no. 1 (October 31, 2013): 25–47. http://dx.doi.org/10.1111/jmg.12056.

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32

Norman, A. R., and G. L. Clarke. "A barometric response to late compression in the Strangways Metamorphic Complex, Arunta Block, central Australia." Journal of Structural Geology 12, no. 5-6 (January 1990): 667–84. http://dx.doi.org/10.1016/0191-8141(90)90081-9.

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33

COOPER, J., G. MORTIMER, and P. JAMES. "Rate of Arunta Inlier evolution at the eastern margin of the Entia Dome, central Australia." Precambrian Research 40-41 (October 1988): 217–31. http://dx.doi.org/10.1016/0301-9268(88)90069-1.

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34

OLIVER, R., R. LAWRENCE, B. GOSCOMBE, P. DING, W. SIVELL, and D. BOWYER. "Metamorphism and crustal considerations in the harts range and neighbouring regions, arunta inlier, central australia." Precambrian Research 40-41 (October 1988): 277–95. http://dx.doi.org/10.1016/0301-9268(88)90072-1.

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35

Das, Kaushik, and M. Yoshida. "A Report of the Post-Conference Field Trip in the Eastern Arunta Inlier, Central Australia." Gondwana Research 3, no. 2 (April 2000): 271–74. http://dx.doi.org/10.1016/s1342-937x(05)70110-6.

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36

Scrimgeour, Ian, and Johann G. Raith. "High-grade reworking of Proterozoic granulites during Ordovician intraplate transpression, eastern Arunta Inlier, central Australia." Geological Society, London, Special Publications 184, no. 1 (2001): 261–87. http://dx.doi.org/10.1144/gsl.sp.2001.184.01.13.

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37

Scrimgeour, I., and J. G. Raith. "A sapphirine-phlogopite-cordierite paragenesis in a low-P amphibolite facies terrain, Arunta Inlier, Australia." Mineralogy and Petrology 75, no. 1-2 (May 1, 2002): 123–30. http://dx.doi.org/10.1007/s007100200019.

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38

Thompson, A., and J. McKinnon-Matthews. "Greenfield nickel sulphide exploration using airborne and ground EM techniques in the Eastern Arunta Region, NT." ASEG Extended Abstracts 2009, no. 1 (2009): 1. http://dx.doi.org/10.1071/aseg2009ab073.

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39

Gunn, P. J., D. Maidment, and P. Milligan. "Interpreting Aeromagnetic Data in Areas of Limited Outcrop: an Example From the Arunta Block, Northern Territory." Exploration Geophysics 26, no. 2-3 (June 1, 1995): 227–32. http://dx.doi.org/10.1071/eg995227.

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40

Warren, R. G., and B. J. Hensen. "The P-T evolution of the Proterozoic Arunta Block, central Australia, and Implications for tectonic evolution." Geological Society, London, Special Publications 43, no. 1 (1989): 349–55. http://dx.doi.org/10.1144/gsl.sp.1989.043.01.30.

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41

Claoué-Long, Jonathan C., and Dean M. Hoatson. "Proterozoic mafic–ultramafic intrusions in the Arunta Region, central AustraliaPart 2: Event chronology and regional correlations." Precambrian Research 142, no. 3-4 (December 6, 2005): 134–58. http://dx.doi.org/10.1016/j.precamres.2005.08.006.

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42

Hoatson, Dean M., Shen-su Sun, and Jonathan C. Claoué-Long. "Proterozoic mafic–ultramafic intrusions in the Arunta Region, central AustraliaPart 1: Geological setting and mineral potential." Precambrian Research 142, no. 3-4 (December 6, 2005): 93–133. http://dx.doi.org/10.1016/j.precamres.2005.09.004.

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43

Black, L. "An assessment, based on U_Pb zircon data, of Rb_Sr dating in the Arunta Inlier, central Australia." Precambrian Research 71, no. 1-4 (February 1995): 3–15. http://dx.doi.org/10.1016/0301-9268(94)00053-t.

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44

Collins, W. "SHRIMP ionprobe dating of short-lived Proterozoic tectonic cycles in the northern Arunta Inlier, central Australia." Precambrian Research 71, no. 1-4 (February 1995): 69–89. http://dx.doi.org/10.1016/0301-9268(94)00056-w.

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45

Read, C. M., and I. Cartwright. "Meteoric fluid infiltration in the middle crust during shearing: examples from the Arunta Inlier, central Australia." Journal of Geochemical Exploration 69-70 (June 2000): 333–37. http://dx.doi.org/10.1016/s0375-6742(00)00134-5.

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46

Whiting, T. H. "Aeromagnetics as an aid to geological mapping—a case history from the Arunta Inlier, Northern Territory." Australian Journal of Earth Sciences 33, no. 2 (June 1986): 271–86. http://dx.doi.org/10.1080/08120098608729364.

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47

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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Анотація:

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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48

Dirks, P. H. G. M. "Intertidal and subtidal sedimentation during a mid‐Proterozoic marine transgression, reynolds range group, Arunta block, central Australia." Australian Journal of Earth Sciences 37, no. 4 (December 1990): 409–22. http://dx.doi.org/10.1080/08120099008727941.

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49

SCRIMGEOUR, I., P. KINNY, D. CLOSE, and C. EDGOOSE. "High- granulites and polymetamorphism in the southern Arunta Region, central Australia: Evidence for a 1.64Ga accretional event." Precambrian Research 142, no. 1-2 (November 30, 2005): 1–27. http://dx.doi.org/10.1016/j.precamres.2005.08.005.

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50

Zhao, J. "SHRIMP U_Pb zircon geochronology of granites in the Arunta Inlier, central Australia: implications for Proterozoic crustal evolution." Precambrian Research 71, no. 1-4 (February 1995): 17–43. http://dx.doi.org/10.1016/0301-9268(94)00054-u.

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