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Relevant bibliographies by topics / Basalt Australia

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Journal articles

Academic literature on the topic 'Basalt Australia'

Author: Grafiati

Published: 4 June 2021

Last updated: 31 January 2023

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Journal articles on the topic "Basalt Australia"

1

Shayan, A., and G. W. Quick. "An alkali-reactive basalt from Queensland, Australia." International Journal of Cement Composites and Lightweight Concrete 10, no. 4 (1988): 209–14. http://dx.doi.org/10.1016/0262-5075(88)90050-4.

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2

Zhou, Binzhong, Peter Hatherly, Troy Peters, and Weijia Sun. "Coal seismic surveying over near-surface basalts: Experience from Central Queensland, Australia." GEOPHYSICS 79, no. 2 (2014): B109—B122. http://dx.doi.org/10.1190/geo2013-0259.1.

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Seismic reflection surveying in basalt-covered areas often fails to image underlying reflectors. To gain insights into the nature of the problem and obtain potential solutions, we have conducted experimental 2D seismic reflection and offset VSP surveys at two coal mines in the Bowen Basin of Australia. At the first mine, the basalt is relatively deep (114 m) and relatively thin (20 m). Conventional seismic acquisition and processing of a 2D seismic line provide poor results. However, upgoing reflections from layers below the basalt are clearly evident in the VSP survey and prestack depth migra

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3

Kislov, Evgeniy V., Anna V. Aseeva, Vladislav V. Vanteev, Anton Yurievich Sinyov, and Olga A. Eliseeva. "Naryn-Gol Creek Sapphire Placer Deposit, Buryatia, Russia." Minerals 12, no. 5 (2022): 509. http://dx.doi.org/10.3390/min12050509.

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A new gem corundum occurrence has been discovered in the Naryn-Gol Creek placer of the Dzhida volcanic field (Russia). In this placer deposit, sapphire associates with large crystals of garnet, spinel, augite, olivine, enstatite, ilmenite, Ti-magnetite, and alkali feldspar. Such a combination of minerals is typical for the placer deposits associated with alkali basalts widely distributed in Southeastern Asia and Australia. We have also found sapphire crystals in phonotephrites of the nearby Cenozoic alkali-basalt paleovolcano Barun Khobol Pravyi, and in basalt sample and trachybasalt from the

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4

Jati Widiatama, Angga, Happy Christin Natalia, Rinaldi Ikhram, et al. "Various sources of rare earth element enrichment at Manamas volcanic rock, Timor Island." IOP Conference Series: Earth and Environmental Science 882, no. 1 (2021): 012044. http://dx.doi.org/10.1088/1755-1315/882/1/012044.

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Abstract Manamas volcanic rock formed due to crustal thinning in fore arc setting. This research aims to provide information and the enrichment process of rare earth elements in Manamas Formation on the Timor Island and their tectonic implication. Manamas volcanic rock exposed in Bihati River, Baun, Timor consists of two different types of basalts, namely alkaline basalt and sub alkaline basalt. Analysis using ICP-MS method shows enrichment in large ion lithophile element and high field strength element. Subalkaline basalt has N-MORB patterns and alkaline basalt have OIB patterns. The Nb eleme

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5

Rolfe, Joe, Mark Keating, Craig Lemin, et al. "Evaluating leucaena in timbered northern basalt country in Queensland, Australia." Tropical Grasslands-Forrajes Tropicales 7, no. 4 (2019): 333–35. http://dx.doi.org/10.17138/tgft(7)333-335.

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6

Isbell, RF. "Krasnozems - a profile." Soil Research 32, no. 5 (1994): 915. http://dx.doi.org/10.1071/sr9940915.

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Since the first soil map of Australia by Prescott in 1931, acid red soils developed from basalt have been specifically recognized in spite of their very limited area of occurrence in eastern Australia from North Queensland to Tasmania in a rainfall zone of about 1000 to 4000 mm. Until the early 1950s these soils were known as red loams, but the term krasnozem became formalised in 1953 with the publication of Stephen's Manual of Australian Soils. Over the past 40 years, these soils have been extensively studied because their favourable agronomic properties have led to intensive land use. The kr

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7

Al-Yaseri, Ahmed, Mujahid Ali, Muhammad Ali, Reza Taheri, and Domenik Wolff-Boenisch. "Western Australia basalt-CO2-brine wettability at geo-storage conditions." Journal of Colloid and Interface Science 603 (December 2021): 165–71. http://dx.doi.org/10.1016/j.jcis.2021.06.078.

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8

McCarthy, P. M. "Three New Species of Porina (Trichotheliaceae) from Lord Howe Island, Australia." Lichenologist 29, no. 3 (1997): 229–36. http://dx.doi.org/10.1006/lich.1996.0077.

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9

Sutherland, F. L., R. R. Coenraads, D. Schwarz, L. R. Raynor, B. J. Barron, and G. B. Webb. "Al-rich diopside in alluvial ruby and corundum-bearing xenoliths, Australian and SE Asian basalt fields." Mineralogical Magazine 67, no. 4 (2003): 717–32. http://dx.doi.org/10.1180/0026461036740129.

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AbstractAlluvial rubies and sapphires are found in palaeodrainage deposits along the Cudgegong-Macquarie River system, central eastern New South Wales, Australia. A pink to red suite contains Cr (up to 0.6 wt.% Cr2O3) as the main chromophore, exceeding Fe (up to 0.5 wt.%Fe2O3). Corrosive etching suggests a prior xenocrystic Mesozoic-Cenozoic basaltic transport, while Cr2O3/Ga2O3to Fe2O3/TiO2ratios indicate an original metamorphic source. Syngenetic mineral inclusions include Al-rich diopside, meionite and anatase. The Al-rich diopside (‘fassaite’) contains extremely high Al2O3(20–21 wt.%). A b

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10

Mayer, Wolf. "The Geological Work of the Baudin Expedition in Australia (1801-1803): The Mineralogists, the Discoveries and the Legacy." Earth Sciences History 28, no. 2 (2009): 293–324. http://dx.doi.org/10.17704/eshi.28.2.mr134w5l2507053n.

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The Baudin expedition to Australia included among its scientific staff Louis Depuch and Joseph Charles Bailly, the first professionally educated geologists to visit this country. Together with the zoologist François Péron, they carried out the earliest geological surveys along large parts of its coast. Their views on the origin of the major rock types were mainly guided by Neptunist thinking. However, in line with the beliefs of a number of French geologists at the time, they recognized basalt as a volcanic rock. Their identification of earth materials was hampered by the still imprecise defin

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