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Artykuły w czasopismach na temat "Marine sediments South Australia St"

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Lee, Won-Je. "Choanoflagellates (Protist) from Marine Sediments of South-Eastern Australia." Korean Journal of Systematic Zoology 23, no. 1 (May 31, 2007): 1–7. http://dx.doi.org/10.5635/kjsz.2007.23.1.001.

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Maher, W. A. "Trace metal concentrations in marine organisms from St. Vincent Gulf, South Australia." Water, Air, and Soil Pollution 29, no. 1 (May 1986): 77–84. http://dx.doi.org/10.1007/bf00149330.

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Jones, MR. "Surficial sediments of the western Gulf of Carpentaria, Australia." Marine and Freshwater Research 38, no. 1 (1987): 151. http://dx.doi.org/10.1071/mf9870151.

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Modern sedimentation in the Gulf of Carpentaria is confined principally to marginal areas in water depths of less than 50 m. Within this zone, the distribution of sediments is irregular, being controlled by proximity to sediment sources and degree of exposure to waves and tidal activity. This is particularly so in the western gulf, where fluvial sediments supplied to Limmen Bight have been transported by waves and tides northwards beyond that embayment to accumulate in the sheltered environment of Blue Mud Bay. Limmen Bight is exposed to the south-easterlies, which produce sufficient wave acti
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Fernandes, Milena, Ali Shareef, Rai Kookana, Sam Gaylard, Sonja Hoare, and Tim Kildea. "The distribution of triclosan and methyl-triclosan in marine sediments of Barker Inlet, South Australia." Journal of Environmental Monitoring 13, no. 4 (2011): 801. http://dx.doi.org/10.1039/c0em00612b.

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Schrale, G., R. Boardman, and M. J. Blaskett. "Investigating Land Based Disposal of Bolivar Reclaimed Water, South Australia." Water Science and Technology 27, no. 1 (January 1, 1993): 87–96. http://dx.doi.org/10.2166/wst.1993.0022.

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The Bolivar Sewage Treatment Works (STW) processes the urban and industrial sewage from the northern and eastern suburbs of Adelaide. The treatment capacity is equivalent to the sewage production of 1.1 million people. The disposal of more than 40 000 ML of reclaimed water into the sea has caused a progressive degradation of about 950 ha of seagrass beds which threatens the sustainability of the fisheries and marine ecosystems of Gulf St. Vincent. The current practice will no longer be viable to achieve compliance with the SA Marine Environment Protection Act, 1990. A Inter-Departmental Workin
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Murray‐Wallace, C. V., and R. W. L. Kimber. "Evaluation of the amino acid racemization reaction in studies of Quaternary marine sediments in South Australia." Australian Journal of Earth Sciences 34, no. 3 (September 1987): 279–92. http://dx.doi.org/10.1080/08120098708729411.

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Cann, John H., Antonio P. Belperio, Victor A. Gostin, and Colin V. Murray-Wallace. "Sea-Level History, 45,000 to 30,000 yr B.P., Inferred from Benthic Foraminifera, Gulf St. Vincent, South Australia." Quaternary Research 29, no. 2 (March 1988): 153–75. http://dx.doi.org/10.1016/0033-5894(88)90058-0.

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Surficial sediments of Gulf St. Vincent, South Australia, are predominantly bioclastic, cool-temperate carbonates. Benthic foraminifera are abundant and distribution of species is closely related to water depth. For example, Massilina milletti is most common at depths ca. 40 m, while Discorbis dimidiatus is characteristics of shallow, subtidal environments. Elphidium crispum, a shallow-water species, and E. macelliforme, favoring deeper water, provide a useful numerical ratio. Their logarithmic relative abundance, in the sediment size fraction 0.50–0.25 mm, correlates strongly with water depth
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Shen, Li, Liu, Li, and Zhang. "Gas Permeability and Production Potential of Marine Hydrate Deposits in South China Sea." Energies 12, no. 21 (October 28, 2019): 4117. http://dx.doi.org/10.3390/en12214117.

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The permeability of marine sediments is critical to the gas production assessment of hydrate reservoirs. In this work, the sample of natural marine sediments was obtained from Shenhu Area of South China Sea at the depth of 1600 m, and the gas permeability of the sample was measured in the laboratory under various confining pressures. The porosity of the sample decreased from 41.82% to 29.54%, and the effective gas permeability of the sample decreased from 2.638 × 10−16 m2 to 0.872 × 10−16 m2 as the confining pressure increased from 0 to 23 MPa. The gas permeability of the natural sediments was
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Moussavi-Harami, R., and D. I. Gravestock. "BURIAL HISTORY OF THE EASTERN OFFICER BASIN, SOUTH AUSTRALIA." APPEA Journal 35, no. 1 (1995): 307. http://dx.doi.org/10.1071/aj94019.

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The intracratonic Officer Basin of central Australia was formed during the Neoproterozoic, approximately 820 m.y. ago. The eastern third of the Officer Basin is in South Australia and contains nine unconformity-bounded sequence sets (super-sequences), from Neoproterozoic to Tertiary in age. Burial history is interpreted from a series of diagrams generated from well data in structurally diverse settings. These enable comparison between the stable shelf and co-existing deep troughs. During the Neoproterozoic, subsidence in the north (Munyarai Trough) was much higher than in either the south (Gil
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Cann, John H., Colin V. Murray-Wallace, Naomi J. Riggs, and Antonio P. Belperio. "Successive foraminiferal faunas and inferred palaeoenvironments associated with the postglacial (Holocene) marine transgression, Gulf St Vincent, South Australia." Holocene 16, no. 2 (February 2006): 224–34. http://dx.doi.org/10.1191/0959683606hl907rp.

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Rozprawy doktorskie na temat "Marine sediments South Australia St"

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Daniel, Richard F. "Carbonate sediments of a cool-water embayment, Streaky Bay, South Australia /." Title page, contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09PH/09phd1847.pdf.

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Mee, Aija C. "Origin, formation and environmental significance of sapropels in shallow Holocene coastal lakes of Southeastern Australia." 2007. http://hdl.handle.net/2440/57295.

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Title page, contents and abstract only. The complete thesis in print form is available from the University of Adelaide Library.<br>The aims of this investigation on the Holocene carbonate successions of three shallow, ephemeral lakes from the Cooring coastal plain were: to determine the timing of the sapropel ’events’ in the three lakes; to determine the origin of the sapropelic organic matter and evaluate changes; to establish whether sapropel deposition in these shallow, coastal lakes primarily reflects increased organic matter delivery to the sediments during periods of enhanced terrestrial
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Daniel, Richard F. (Richard Francis). "Carbonate sediments of a cool-water embayment, Streaky Bay, South Australia." 2002. http://web4.library.adelaide.edu.au/theses/09PH/09phd1847.pdf.

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"March 2002" Includes bibliographical references (leaves 145-161) An analogue for shallow marine carbonate sedimentation and deposition on a broad passive margin is described from the eastern Great Australian Bight.
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Książki na temat "Marine sediments South Australia St"

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Heggie, D. T. Continental margin transects: Geochemistry of surface sediments from the southern Australian continental margin including offshore west Tasmania, South Australia and Victoria : projects 121.13, 121.20 and 121.38. Canberra: Australian Geological Survey Organisation, 1993.

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