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Artykuły w czasopismach na temat "Southeast Queensland"
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Sinclair, E. R. "PINEAPPLE GROWTH IN SOUTHEAST QUEENSLAND". Acta Horticulturae, nr 334 (październik 1993): 171–86. http://dx.doi.org/10.17660/actahortic.1993.334.17.
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Ulm, Sean. "Reassessing Marine Fishery Intensification in Southeast Queensland". Queensland Archaeological Research 13 (1.12.2002): 79. http://dx.doi.org/10.25120/qar.13.2002.70.
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A review of the archaeological evidence underlying a model by Walters of late Holocene Aboriginal marine fishery intensification in southeast Queensland is undertaken. The results of a regional review of the available fish bone neither support an argument for a general pattern of increase in fish discard at coastal sites nor the claim for an exponential increase through time in the number of sites exhibiting fish remains. Major taphonomic issues and research biases are considered to have played a role in structuring the archaeological database of the region.
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McNiven, Ian J. "Bevel-edged tools from coastal southeast Queensland". Antiquity 66, nr 252 (wrzesień 1992): 701–9. http://dx.doi.org/10.1017/s0003598x00039405.
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Thies, Detlev, i Susan Turner. "Jurassic actinopterygian fish from Monto, southeast Queensland". Alcheringa: An Australasian Journal of Palaeontology 25, nr 4 (styczeń 2001): 381–86. http://dx.doi.org/10.1080/03115510108619227.
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Evans, M. L. "ARTHROPOD SPECIES IN SOYBEANS IN SOUTHEAST QUEENSLAND". Australian Journal of Entomology 24, nr 3 (sierpień 1985): 169–77. http://dx.doi.org/10.1111/j.1440-6055.1985.tb00218.x.
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McKay, Belinda. "Imagining the Hinterland: Literary Representations of Southeast Queensland Beyond the Brisbane Line". Queensland Review 12, nr 1 (styczeń 2005): 59–74. http://dx.doi.org/10.1017/s1321816600003913.
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Southeast Queensland — the region encompassing Coolangatta and the McPherson Range to the south, Cooloola and the Blackall Range to the north, and the Great Dividing Range to the west — represents one of Queensland's most significant literary landscapes. For millennia, this area — defined by mountains and waterways — contained important gathering places for ceremonies and trade, and its inhabitants elaborated the meaning of the landscape in a rich complex of stories and other cultural practices such as the bunya festivals. Colonisation disrupted but did not obliterate these cultural associations, which remain alive in the oral traditions of local Aboriginal people and, in more recent times, have surfaced in the work of writers like Oodgeroo Noonuccal and Sam Watson.
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Woodall, PF. "The Cattle Egret, Ardeola-Ibis, in Southeast Queensland". Wildlife Research 13, nr 4 (1986): 575. http://dx.doi.org/10.1071/wr9860575.
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Annual counts made by the Queensland Ornithological Society (1972-83) were used to monitor cattle egret numbers in south-east Queensland. Numbers in coastal areas were reasonably stable during this period but, after an initial stage of low numbers, the inland population increased rapidly from 1975 to 1981. An exponential equation, N=0.752 exp(0.320t), gave the best fit to these data. Declines in numbers in 1977 might have been associated with low rainfall in the Moreton meteorological region. At the start of the survey the cattle egret was the most abundant ardeid in coastal areas and, as its numbers increased in inland areas, there was a coincidental decline in numbers of great egret Egretta alba.
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Hiscock, Peter, i J. Hall. "Technological change at Platypus Rockshelter (KB:A70), southeast Queensland". Queensland Archaeological Research 5 (1.01.1988): 63–89. http://dx.doi.org/10.25120/qar.5.1988.160.
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Platypus Rockshelter yielded a rich and varied assemblage of stone artefacts. In this paper we describe temporal change in the artefact assemblage and, by implication, prehistoric technology, concentrating particularly on the evidence for chert stoneworking. Readers are referred to accompanying papers by Hall et al (1988) and Hall and Hiscock (1988) in this volume of QAR for details of the stratigraphy and dating of the site. What is important to reiterate here is that the deposit provides a discontinuous sequence of occupation dating back to approximately 5300 years BP. This, plus the fact the radiocarbon samples were selected to date stratigraphic transition, means that the artefactual sequence is divided into a number of sharply-bounded analytical units, and change can be identified between but not within these units. The necessity for the cultural sequence to be subdivided in this way makes it likely that gradual changes in prehistory will be seen as episodic, and that each unit may be a compilation of a number of discrete occupation events (cf. Frankel 1988). Thus, while we employ strata as minimal units of comparison in the artefactual analysis, we make no assumptions about the uniformity within, and rate of change between, those units. The purpose of the paper is to characterize the long-term changes in the technology of the inhabitants of the site.
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Hiscock, Peter, i J. Hall. "Technological change at Bushrangers cave (LA:A11), southeast Queensland". Queensland Archaeological Research 5 (1.01.1988): 90–112. http://dx.doi.org/10.25120/qar.5.1988.161.
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Bushrangers Cave is the oldest mainland archaeological site so far discovered in the Moreton Region of southeast Queensland. Occupation began approximately 6000 years ago, at a time when the rising seas flooded Moreton Bay and reached their present levels. Several researchers have suggested that after the infilling of the Bay food resources were more plentiful, and that during the last 6000 years there was population growth and a restructuring of Aboriginal society (Hall 1982, 1986; Morwood 1986). At least some of these changes should be visible at Bushrangers Cave and Hall (1986:101) has argued that economic and social reorganization may be reflected in the procurement of stone material by the knappers who left stone artefacts in the cave. Indications that stone from the vicinity of the cave may have been transported some distance during the late Holocene raise similar possibilities (Bird et al 1987). Exploratory excavations and preliminary analysis of the recovered artefacts was reported by Hall (1986), who demonstrated that changes in artefact frequency and raw material type did occur. Further radiocarbon dates and more detailed investigations of the artefactual assemblage are presented in this paper. While a more complete understanding of the site will require the excavation of a larger area, the data described below enable some preliminary conclusions to be drawn about chronological change in stone procurement, stoneworking technology and the nature and intensity of occupation.
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Herrington, M. E., C. M. Hardner, M. Wegener, L. L. Woolcock i M. J. Dieters. "Breeding objective for strawberry in subtropical southeast Queensland". Acta Horticulturae, nr 1127 (listopad 2016): 203–10. http://dx.doi.org/10.17660/actahortic.2016.1127.32.
Pełny tekst źródłaRozprawy doktorskie na temat "Southeast Queensland"
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Smith, Annette Deborah (Tam). "Archaeological spatial variability on Bribie Island, Southeast Queensland /". St. Lucia, Qld, 2003. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe17698.pdf.
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Gustafson, Johann A. "Hammerhead sharks (Sphyrnidae) of southeast Queensland: habitat and movements". Thesis, Griffith University, 2020. http://hdl.handle.net/10072/397639.
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Hammerhead sharks (Sphyrnidae) are iconic and charismatic species that have received little attention until more recently, resulting in knowledge gaps about life histories, habitats, behaviours and migratory drivers, mostly in the southern hemisphere such as Australian waters. Globally, shark populations are declining as many species extinction risk has increased under the threat of fishing and habitat degradation. Hammerhead shark (Sphyrnidae) populations are highly susceptible to human-induced pressure such as long lines and are currently undergoing severe declines, especially in Australia. Recently, hammerhead sharks have been added to the International Union for Conservation of Nature’s (IUCN) Red List of Threatened Species, with scalloped hammerhead listed as critically endangered. Therefore, further information is needed to address the current shortfalls regarding hammerheads in Australia, for the management and conservation of these species.
Earlier research using catch data from the Queensland Shark Control Program (QSCP) showed a decline in numbers of caught hammerhead sharks since the start of the program in 1960. A review of the literature (CHAPTER 1) revealed that hammerhead sharks were understudied in Australia, with information shortfalls on movement, resource use, nursery areas and habitat use. The general aim of this thesis was to provide a better understanding of the movement, distribution, habitat use and resource use of scalloped hammerhead shark (Sphyrna lewini) in Queensland, Australia to improve conservation and management strategies. I used multiple methodologies to determine (i) the distribution of suitable habitat for juvenile scalloped hammerhead sharks and the percentage of overlap with marine protected areas (CHAPTER 2); (ii) fine-scale movement of juvenile scalloped hammerheads within these habitats and determine behavioural states using high-resolution acoustic tracking (CHAPTER 3); (iii) thermal tolerance range “thermal niche” of hammerhead shark using historical catch records from the QSCP (CHAPTER 4); and (iv) resource overlap between hammerhead sharks species and with other co-existing large sharks using carbon and nitrogen stable isotopes (CHAPTER 5). This allowed me to build a solid baseline framework of the ecology of scalloped hammerhead sharks in Queensland.
The species distribution model identified 10,082.87 km2 of suitable habitat characterised by low current velocities (< 0.5 m-s), warm sea surface temperatures (> 20°C), estuarine/oceanic salinities (25-35 PSU) and shallow bathymetries (< 20 m). Suitable habitats occurred in coastal areas within wetland and seagrass habitats. Highly suitable areas accounted for 1,784.33 km2 of the total distribution and
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occurred around highly developed areas, such as Moreton Bay, Hervey Bay, Townsville and Cairns. Coastal beach areas of the Gold Coast were also uncovered as highly suitable habitats and may be due to close proximity of the Gold Coast seaway and Tweed River connections to more sheltered estuarine habitats. The majority of the predicted suitable distribution occurred within the lower protection multi-use zones (6,291.20 km2) and outside marine protected areas (3,791.67 km2); where no-take zones protected only 11 % and 8.56 % of high and medium modelled suitable habitats. Within these habitats, continuous tracking of two juvenile scalloped hammerhead sharks uncovered highly active diving behaviours where both sharks continuously dove from water surface to the bay floor over 12- and 3-hour tracks. Two diving patterns were observed in both sharks and described as A-type: one long dive with multiple small dives at depth, and B-type dives: one long dive without extra dives at depth. The two-state behavioural model uncovered low activity (forage) and high activity (direction) states, which were influenced by distance to seagrass and coral habitats as well as habitat depth.
Quantile regression modelling determined catches of hammerhead sharks in relation to changes in seas surface temperatures changed with latitude along the Queensland coast. Scalloped hammerhead catches in the southern areas were most likely to occur between 20℃ - 25℃ and likely to occur throughout the year in the northern areas, as sea surface temperatures remained above 22℃. Co-existing bull (Carcharias leucas) and tiger (Galeocerdo cuvier) sharks also occurred throughout this thermal range while white shark (Carcharodon carcharias) only occurred below 23℃. Stable isotope analysis revealed scalloped and great hammerhead sharks overlapped 69% in isotopic space and with several large shark species. Both hammerhead species undertook a seasonal dietary shift, and scalloped hammerheads showed a wider δ13C and lower δ15N than the more specialised great hammerhead. Tiger sharks feed at a lower trophic level overlapping mostly with both hammerhead sharks. White and bull sharks competed with hammerhead sharks at higher δ15N.
Overall, results from my research make original contributions to the knowledge of hammerhead sharks by identifying previously unreported distributions of suitable juvenile habitats of the scalloped hammerhead, which occurred in developed areas and within multi-use protection zones. Additionally, the research described previously unreported diving patterns and state-switching of juvenile hammerhead sharks within highly developed areas, highlighting the importance of wetland and estuarine habitats for shark conservation. Furthermore, the research showed high overlap in resource use between two endangered hammerhead species with several large predatory shark species. In iii summary, this thesis highlights the relevance of movement and habitat use information in the conservation and management of endangered iconic shark speciesThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Eng & Built Env
Science, Environment, Engineering and Technology
Full Text
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Mackay, Stephen John. "Drivers of Macrophyte Assemblage Structure in Southeast Queensland Streams". Thesis, Griffith University, 2007. http://hdl.handle.net/10072/367431.
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Recent drought and population growth along the east Australian coastline, combined with water quality issues and degradation of rivers of national significance, have focused attention on the importance of sustainable water resource use and maintenance of the ecological integrity of riverine ecosystems. Central to the development of stream management practices that minimise or ameliorate anthropogenic degradation of riverine ecosystems is an understanding of the principal drivers of ecosystem structure and function.
This thesis investigates the principal drivers of submersed macrophyte assemblage structure in streams of southeast Queensland, Australia. Fundamental to this thesis is the development and testing of a conceptual model of macrophyte assemblage structure in streams with disturbance (hydrology and hydraulics) and resource availability (nitrogen, phosphorus, carbon, light) as the principal axes of the model. The suitability of the conceptual model as a framework to describe the key drivers of macrophyte assemblage structure within the study area was explored by testing hypotheses of macrophyte assemblage structure at various spatial scales across disturbance and resource availability gradients. In particular, it was hypothesised that assemblage structure could be described in terms of appropriate measures of disturbance and resource availability; that extremes of disturbance (e.g. flooding) and resource availability (e.g. high shade) would limit macrophyte growth; and that species richness would vary according to the intermediate disturbance hypothesis. Furthermore, it was expected that flow regime changes resulting from flow regulation would have predictable impacts on macrophyte assemblage structure, in line with these hypotheses.
In general the results of this thesis supported hypotheses based on the conceptual model. Spatial and temporal patterns in macrophyte assemblage structure were associated with hydrologic-hydraulic and resource availability gradients. These patterns were shown to be consistent across a variety of spatial scales, but were tighter at the transect and hydraulic unit (riffle, run, pool) scales. The key descriptors of the disturbance axis of the conceptual model were bankfull shear stress, substrate stability, the coefficient of variation of mean daily discharge, days since last flood and the number of floods in the 12 months prior to sampling. Riparian canopy cover and alkalinity were identified as the key descriptors of the resource availability axis. However, geomorphological attributes such as bankfull depth and channel orientation were also important in structuring macrophyte assemblages.
From the conceptual model it was predicted that flow regulation by large dams would result in increased macrophyte abundance due to reduced disturbance frequency and magnitude. Further, it was predicted that reduced temporal hydrologic variability in sites with regulated flows would produce relatively stable macrophyte assemblages as disturbance frequency (i.e. the frequency of biomass loss) should be minimal compared with an unregulated stream of similar morphology and water quality. These predictions were tested in two ways.
Firstly, spatial patterns in assemblage structure were compared between regulated and unregulated sites. Flow regulation had no effect on species richness but macrophyte cover was higher than expected in regulated sites compared to macrophyte cover in unregulated reference sites. The extent of increase in macrophyte cover was dependent upon site location in the catchment, as hypothesised in the Serial Discontinuity Concept, and local (site-specific) characteristics. In the lower Brisbane River, the increase in macrophyte cover was relatively small as large macrophyte beds were natural features of this lowland river with limited riparian shading. In Yabba Creek, a mid-catchment tributary, the increase in macrophyte cover was relatively high, taking the form of extensive macrophyte beds which were uncommon in comparable (unregulated) streams characterised by high riparian canopy cover.
Secondly, the effect of flow regulation on temporal variability in macrophyte assemblage structure was examined over a 12 month period in a regulated stream (Yabba Creek) and an adjacent unregulated stream (Amamoor Creek). The magnitude of temporal environmental variability was similar for both creeks. Macrophyte assemblage structure was found to be highly variable in Amamoor Creek, and comparatively stable in Yabba Creek, in accordance with conceptual model predictions. Again it was found that local habitat conditions in each waterway (particularly riparian shading) had an overriding influence on the response of submersed macrophytes to hydrologic variability and flow regulation.
The effects of riparian shading on macrophyte assemblages were investigated further by examining the influence of riparian canopy cover and light availability on the growth of five aquatic macrophyte species in a stream rehabilitation site. This site was located in a second order headwater stream with a degraded riparian zone where unshaded parts of the site were infested with submersed and emergent macrophytes. Changes in assemblage structure were monitored over a two year period and related to changes in riparian canopy cover resulting from the regrowth of native riparian tubestock. Reductions in macrophyte abundance and changes in species composition were predicted from the conceptual model as riparian shade increased due to vegetation regrowth. The results are discussed in light of hypotheses derived from the conceptual model, particularly with respect to the effects of interactions between flow regulation and resource limitations on macrophyte assemblage structure.
The results of this thesis show that the conceptual model is a valid representation of the physical habitat template occupied by submersed macrophytes in the study area, and is also likely to be valid for lotic ecosystems in other bioregions, provided that herbivory is not a major (alternative) source of disturbance. However, the contribution of hydrology as the principal direct driver of macrophyte assemblage structure is questioned. This thesis has shown that local (site-specific) conditions, including riparian canopy cover and substrate stability, are probably more important drivers of macrophyte assemblage structure per se than hydrology itself. Local habitat conditions such as bed stability and substrate composition determine how features of the flow regime, such as discharge magnitude, influence macrophyte assemblage structure. Management strategies that focus solely on manipulating the hydrologic regime (e.g. by provision of environmental flows) may not fully accommodate the habitat template for submersed macrophytes in lotic ecosystems.Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
Griffith School of Environment
Full Text
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Chern, Peter Kyaw Zaw Naing. "Patterns of coal sedimentation in the Ipswich Basin Southeast Queensland". Thesis, Queensland University of Technology, 2004. https://eprints.qut.edu.au/15924/1/Peter_Chern_Thesis.pdf.
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The intermontane Ipswich Basin, which is situated 30km south-west of Brisbane, contains coal measures formed in the Late Triassic Epoch
following a barren non-depositional period. Coal, tuff, and basalt were deposited along with fluvial dominated sediments. The Ipswich Coal
Measures mark the resumption of deposition in eastern Australia after the coal hiatus associated with a series of intense tectonic activity in Gondwanaland during the Permo-Triassic interval. A transtensional tectonic
movement at the end of the Middle Triassic deformed the Toogalawah Group before extension led to the formation of the Carnian Ipswich Coal
Measures in the east.
The Ipswich Coal Measures comprise the Brassall and Kholo Subgroups. The Blackstone Formation, which forms the upper unit of the Brassall
Subgroup, contains seven major coal seams. The lower unit of the Brassall Subgroup, the Tivoli Formation, consists of sixteen stratigraphically
significant coal seams. The typical thickness of the Blackstone Formation is 240m and the Tivoli Formation is about 500m.
The coal seams of the Ipswich Basin differ considerably from those of other continental Triassic basins. However, the coal geology has previously attracted little academic attention and the remaining exposures of the Ipswich coalfield are rapidly disappearing now that mining has ceased. The primary aim of this project was to study the patterns of coal sedimentation and the response of coal seam characteristics to changing depositional
environments.
The coal accumulated as a peat-mire in an alluvial plain with meandering channel systems. Two types of peat-mire expansion occurred in the basin. Peat-mire aggradation, which is a replacement of water body by the peatmire,
was initiated by tectonic subsidence. This type of peat-mire expansion is known as terrestrialisation. It formed thick but laterally limited coal seams in the basin. Whereas, peat-mire progradation was related to
paludification and produced widespread coal accumulation in the basin.
The coal seams were separated into three main groups based on the mean seam thickness and aerial distribution of one-meter and four-meter thickness contour intervals. Group 1 seams within the one-meter thickness interval are
up to 15,000m2 in area, and seams within the four-meter interval have an aerial extent of up to 10,000m2. Group 1A contains the oldest seam with numerous intraseam clastic bands and shows a very high thickness to area ratio, which indicates high subsidence rates. Group 1B seams have moderately high thickness to area ratios. The lower clastic influx and slower subsidence rates favoured peat-mire aggradation. The Group 1A seam is relatively more widespread in aerial extent than seams from Group 1B. Group 1C seams have low mean thicknesses and small areas, suggesting short-lived peat-mires as a result of high clastic influx. Group 2 seams arebetween 15,000 and 35,000m2 in area within the one-meter interval, and between 5,000 and 10,000m2 within the four-meter interval. They have
moderately high area to thickness ratios, indicating that peat-mire expansion
occurred due to progressively shallower accommodation and a rising groundwater table. Group 3 seams, which have aerial extents from 35,000 to 45,000m2 within the one-meter thickness contour interval and from 10,000
to 25,000m2 within the four-meter interval, show high aerial extent to thickness ratios. They were deposited in quiet depositional environments
that favoured prolonged existence of peat-mires. Group 3 seams are all relatively young whereas most Group 1 seams are relatively old seams.
All the major fault systems, F1, F2 and F3, trend northwest-southeast. Apart from the West Ipswich Fault (F3), the F1 and F2 systems are broad Palaeozoic basement structures and thus they may not have had a direct influence on the formation of the much younger coal measures. However, the sedimentation patterns appear to relate to these major fault systems. Depocentres of earlier seams in the Tivoli Formation were restricted to the northern part of the basin, marked by the F1 system. A major depocentre
shift occurred before the end of the deposition of the Tivoli Formation as a result of subsidence in the south that conformed to the F2 system configuration. The Blackstone Formation depocentres shifted to the east (Depocentre 1) and west (Depocentre 2) simultaneously. This depocentre shift was associated with the flexural subsidence produced by the
rejuvenation of the West Ipswich Fault. Coal accumulation mainly occurred in Depocentre 1.
Two types of seam splitting occurred in the Ipswich Basin. Sedimentary splitting or autosedimentation was produced by frequent influx of clastic sediments. The fluvial dominant depositional environments created the
random distribution of small seam splits. However, the coincidence of seam splits and depocentres found in some of the seams suggests tectonic splitting. Furthermore, the progressive splitting pattern, which displays seam splits overlapping, was associated with continued basin subsidence. The tectonic splitting pattern is more dominant in the Ipswich Basin.
Alternating bright bands shown in the brightness profiles are a result of oscillating water cover in the peat-mire. Moderate groundwater level, which was maintained during the development of the peat, reduced the possibility of salinisation and drowning of the peat swamp. On the other hand, a slow continuous rise of the groundwater table, that kept pace with the vertical growth of peat, prevented excessive oxidation of peat.
Ipswich coal is bright due to its high vitrinite content. The cutinite content is also high because the dominant flora was pteridosperms of Dicroidium assemblage containing waxy and thick cuticles. Petrographic study revealed that the depositional environment was telmatic with bog forest formed under ombrotrophic to mesotrophic hydrological conditions. The high preservation
of woody or structured macerals such as telovitrinite and semifusinite indicates that coal is autochthonous. The high mineral matter content in coal is possibly due to the frequent influx of clastic and volcanic sediments.
The Ipswich Basin is part of a much larger Triassic basin extending to Nymboida in New South Wales. Little is known of the coal as it lacks exposures. It is apparently thin to absent except in places like Ipswich and Nymboida. This study suggests that the dominant control on depocentres of thick coal at Ipswich has been the tectonism. Fluvial incursions and
volcanism were superimposed on this.
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Chern, Peter Kyaw Zaw Naing. "Patterns of Coal Sedimentation in the Ipswich Basin Southeast Queensland". Queensland University of Technology, 2004. http://eprints.qut.edu.au/15924/.
Pełny tekst źródłaStreszczenie:
The intermontane Ipswich Basin, which is situated 30km south-west of Brisbane, contains coal measures formed in the Late Triassic Epoch following a barren non-depositional period. Coal, tuff, and basalt were deposited along with fluvial dominated sediments. The Ipswich Coal Measures mark the resumption of deposition in eastern Australia after the coal hiatus associated with a series of intense tectonic activity in Gondwanaland during the Permo-Triassic interval. A transtensional tectonic movement at the end of the Middle Triassic deformed the Toogalawah Group before extension led to the formation of the Carnian Ipswich Coal Measures in the east. The Ipswich Coal Measures comprise the Brassall and Kholo Subgroups. The Blackstone Formation, which forms the upper unit of the Brassall Subgroup, contains seven major coal seams. The lower unit of the Brassall Subgroup, the Tivoli Formation, consists of sixteen stratigraphically significant coal seams. The typical thickness of the Blackstone Formation is 240m and the Tivoli Formation is about 500m. The coal seams of the Ipswich Basin differ considerably from those of other continental Triassic basins. However, the coal geology has previously attracted little academic attention and the remaining exposures of the Ipswich coalfield are rapidly disappearing now that mining has ceased. The primary aim of this project was to study the patterns of coal sedimentation and the response of coal seam characteristics to changing depositional environments. The coal accumulated as a peat-mire in an alluvial plain with meandering channel systems. Two types of peat-mire expansion occurred in the basin. Peat-mire aggradation, which is a replacement of water body by the peatmire, was initiated by tectonic subsidence. This type of peat-mire expansion is known as terrestrialisation. It formed thick but laterally limited coal seams in the basin. Whereas, peat-mire progradation was related to paludification and produced widespread coal accumulation in the basin. The coal seams were separated into three main groups based on the mean seam thickness and aerial distribution of one-meter and four-meter thickness contour intervals. Group 1 seams within the one-meter thickness interval are up to 15,000m2 in area, and seams within the four-meter interval have an aerial extent of up to 10,000m2. Group 1A contains the oldest seam with numerous intraseam clastic bands and shows a very high thickness to area ratio, which indicates high subsidence rates. Group 1B seams have moderately high thickness to area ratios. The lower clastic influx and slower subsidence rates favoured peat-mire aggradation. The Group 1A seam is relatively more widespread in aerial extent than seams from Group 1B. Group 1C seams have low mean thicknesses and small areas, suggesting short-lived peat-mires as a result of high clastic influx. Group 2 seams arebetween 15,000 and 35,000m2 in area within the one-meter interval, and between 5,000 and 10,000m2 within the four-meter interval. They have moderately high area to thickness ratios, indicating that peat-mire expansion occurred due to progressively shallower accommodation and a rising groundwater table. Group 3 seams, which have aerial extents from 35,000 to 45,000m2 within the one-meter thickness contour interval and from 10,000 to 25,000m2 within the four-meter interval, show high aerial extent to thickness ratios. They were deposited in quiet depositional environments that favoured prolonged existence of peat-mires. Group 3 seams are all relatively young whereas most Group 1 seams are relatively old seams. All the major fault systems, F1, F2 and F3, trend northwest-southeast. Apart from the West Ipswich Fault (F3), the F1 and F2 systems are broad Palaeozoic basement structures and thus they may not have had a direct influence on the formation of the much younger coal measures. However, the sedimentation patterns appear to relate to these major fault systems. Depocentres of earlier seams in the Tivoli Formation were restricted to the northern part of the basin, marked by the F1 system. A major depocentre shift occurred before the end of the deposition of the Tivoli Formation as a result of subsidence in the south that conformed to the F2 system configuration. The Blackstone Formation depocentres shifted to the east (Depocentre 1) and west (Depocentre 2) simultaneously. This depocentre shift was associated with the flexural subsidence produced by the rejuvenation of the West Ipswich Fault. Coal accumulation mainly occurred in Depocentre 1. Two types of seam splitting occurred in the Ipswich Basin. Sedimentary splitting or autosedimentation was produced by frequent influx of clastic sediments. The fluvial dominant depositional environments created the random distribution of small seam splits. However, the coincidence of seam splits and depocentres found in some of the seams suggests tectonic splitting. Furthermore, the progressive splitting pattern, which displays seam splits overlapping, was associated with continued basin subsidence. The tectonic splitting pattern is more dominant in the Ipswich Basin. Alternating bright bands shown in the brightness profiles are a result of oscillating water cover in the peat-mire. Moderate groundwater level, which was maintained during the development of the peat, reduced the possibility of salinisation and drowning of the peat swamp. On the other hand, a slow continuous rise of the groundwater table, that kept pace with the vertical growth of peat, prevented excessive oxidation of peat. Ipswich coal is bright due to its high vitrinite content. The cutinite content is also high because the dominant flora was pteridosperms of Dicroidium assemblage containing waxy and thick cuticles. Petrographic study revealed that the depositional environment was telmatic with bog forest formed under ombrotrophic to mesotrophic hydrological conditions. The high preservation of woody or structured macerals such as telovitrinite and semifusinite indicates that coal is autochthonous. The high mineral matter content in coal is possibly due to the frequent influx of clastic and volcanic sediments. The Ipswich Basin is part of a much larger Triassic basin extending to Nymboida in New South Wales. Little is known of the coal as it lacks exposures. It is apparently thin to absent except in places like Ipswich and Nymboida. This study suggests that the dominant control on depocentres of thick coal at Ipswich has been the tectonism. Fluvial incursions and volcanism were superimposed on this.
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Morrison, Fiona Clare, i n/a. "Altitudinal Variation in the Life History of Anurans in Southeast Queensland". Griffith University. School of Environmental and Applied Science, 2002. http://www4.gu.edu.au:8080/adt-root/public/adt-QGU20031125.120847.
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Global declines and disappearances of amphibians from high altitude, pristine habitats have been reported in recent years. To date the cause of many of these declines and/or disappearances has not been identified. Although it is well documented that life history characteristics of temperate amphibians are influenced by altitude (due to systematic variation of temperature with altitude), little work has been carried out on the effects of altitude on Australian anurans. This lack of ecological data is a major impediment to identifying the causal factors responsible for amphibian declines. Due to differences in life history characteristics, high altitude populations may be less resilient than their lowland counterparts and subsequently may be more vulnerable to extinction. Consequently, the main aim of this study was to determine whether altitude influenced life history characteristics and ultimately population resilience of anurans in the southeast Queensland region. Six anuran species; Litoria chloris, L. lesueuri, L. pearsoniana (Anura: Hylidae), Mixophyes fasciolatus, M. fleayi and M. iteratus (Anura: Myobatrachidae) were studied over three field seasons (1997-1999) in 18 sites of varying altitude (100-950m) in the southeast Queensland region. The life history characteristics examined were: activity and breeding season length, fecundity and egg size, number of clutches produced per season, tadpole growth and development rates, longevity, age at maturity, reproductive life span, average lifetime fecundity, survival and recapture rates. The data were collected using a combination of field-based surveys (body sizes, clutch sizes, and survival and recapture rates), museum specimen dissections (clutch and egg sizes), reciprocal transplant field experiments (tadpole growth and development rates) and skeletochronology (longevity, age at maturity, reproductive lifespan and average lifetime fecundity). On average, high altitude populations of all species had shorter breeding and activity seasons than low altitude populations (up to 10 weeks less in some cases). The magnitude of the difference in breeding season length varied among years depending on the average temperature and rainfall for the year; i.e. differences appeared greater in warmer and wetter years. Within a population males had longer breeding and activity seasons than females. Although breeding season length varied with altitude, the number of nights that individuals were active within the breeding season did not vary; i.e. low altitude populations were not active for more nights despite having a longer breeding season. This result was attributed to the absence of a relationship between individual activity and environmental variables (air temperature, rainfall, etc.) in many of the populations. Generally, intraspecific clutch size did not vary significantly with altitude. This result was due to the absence of a significant relationship between female body size and altitude (as clutch size is proportional to female body size). Egg size also did not vary with altitude however, suggesting egg size may be canalized (i.e. fixed) in these species. Results also suggest that females of these species only produce one clutch of eggs per season. Interspecific differences in reproductive characteristics largely reflected differences in reproductive mode, larval habitat and female body size. Altitude negatively influenced growth and development rates in L. chloris and development rates in L. pearsoniana. Tadpoles raised at high altitudes were also generally larger at each Gosner Development Stage in both species. The results of the reciprocal transplant experiments suggested that most of the variation in growth and development rates was due to environmental factors (water temperature) rather than genetic or maternal factors. Altitude or genetic factors did not significantly affect tadpole survival in either species. The results suggest that tadpoles occurring at high altitudes take longer to reach metamorphosis and do so at a larger size than their lowland counterparts. With the exception of L. lesueuri, skeletochronology was suitable for age estimation in the study species. Altitude had a significant effect on the age at maturity or longevity in some of the species, however there were trends toward older individuals and older ages at maturity in high altitude populations for the remaining species. Females were generally older than males for all species and in the case of longer-lived species (i.e. Mixophyes spp.) also tended to be older when breeding for the first time. The large overlap of body sizes of individuals of different ages demonstrates that body size is a poor indicator of age in these species. This is the first study to estimate average lifetime fecundity for more than one amphibian species and/or population. The results suggest that the absence of significant altitudinal variation in the average lifetime fecundity of different populations is due to tradeoffs made by females (current reproduction vs. survival). There was no significant altitudinal variation in annual survival and recapture rates in any of the species, and generally there was no difference in the survival and recapture rates of males and females in each population. Within a year, monthly survival and recapture rates were more variable at low than high altitudes and this was attributed to the longer breeding season of low altitude populations. The results did not support previous studies that suggested there was a size bias in survival and recapture rates. The shorter breeding seasons, slower growth and development rates, older age at maturity and greater longevity found in the high altitude study populations will result in increased generation time in those populations. In turn, increased generation time can cause high altitude populations to be less resilient (i.e. population takes longer to return to equilibrium after a disturbance away from equilibrium) (Pimm et al. 1988, Pimm 1991) and ultimately more vulnerable or prone to extinction or decline. The majority of unexplained global amphibian declines have occurred at high altitudes in tropical and subtropical areas. These latitudinal patterns may be explained by the narrow range of environmental tolerances exhibited by tropical organisms resulting in mountains being effectively higher in the tropics. Consequently, high altitude tropical species are likely to be even more vulnerable than temperate species occurring at similar altitudes. Further work on the effects of geographic variation, especially interactions between altitude and latitude are needed to evaluate the hypotheses for the causes of these declines and disappearances.
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Parker, Nathaniel Ryan. "Assessing the effectiveness of water sensitive urban design in Southeast Queensland". Thesis, Queensland University of Technology, 2010. https://eprints.qut.edu.au/34119/1/Nathaniel_Parker_Thesis.pdf.
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Water Sensitive Urban Design (WSUD) systems have the potential mitigate the hydrologic disturbance and water quality concerns associated with stormwater runoff from urban development. In the last few years WSUD has been strongly promoted in South East Queensland (SEQ) and new developments are now required to use WSUD systems to manage stormwater runoff. However, there has been limited field evaluation of WSUD systems in SEQ and consequently knowledge of their effectiveness in the field, under storm events, is limited. The objective of this research project was to assess the effectiveness of WSUD systems installed in a residential development, under real storm events. To achieve this objective, a constructed wetland, bioretention swale and a bioretention basin were evaluated for their ability to improve the hydrologic and water quality characteristics of stormwater runoff from urban development. The monitoring focused on storm events, with sophisticated event monitoring stations measuring the inflow and outflow from WSUD systems. Data analysis undertaken confirmed that the constructed wetland, bioretention basin and bioretention swale improved the hydrologic characteristics by reducing peak flow. The bioretention systems, particularly the bioretention basin also reduced the runoff volume and frequency of flow, meeting key objectives of current urban stormwater management. The pollutant loads were reduced by the WSUD systems to above or just below the regional guidelines, showing significant reductions to TSS (70-85%), TN (40-50%) and TP (50%). The load reduction of NOx and PO4 3- by the bioretention basin was poor (<20%), whilst the constructed wetland effectively reduced the load of these pollutants in the outflow by approximately 90%. The primary reason for the load reduction in the wetland was due to a reduction in concentration in the outflow, showing efficient treatment of stormwater by the system. In contrast, the concentration of key pollutants exiting the bioretention basin were higher than the inflow. However, as the volume of stormwater exiting the bioretention basin was significantly lower than the inflow, a load reduction was still achieved. Calibrated MUSIC modelling showed that the bioretention basin, and in particular, the constructed wetland were undersized, with 34% and 62% of stormwater bypassing the treatment zones in the devices. Over the long term, a large proportion of runoff would not receive treatment, considerably reducing the effectiveness of the WSUD systems.
8
Morrison, Fiona Clare. "Altitudinal Variation in the Life History of Anurans in Southeast Queensland". Thesis, Griffith University, 2002. http://hdl.handle.net/10072/366730.
Pełny tekst źródłaStreszczenie:
Global declines and disappearances of amphibians from high altitude, pristine habitats have been reported in recent years. To date the cause of many of these declines and/or disappearances has not been identified. Although it is well documented that life history characteristics of temperate amphibians are influenced by altitude (due to systematic variation of temperature with altitude), little work has been carried out on the effects of altitude on Australian anurans. This lack of ecological data is a major impediment to identifying the causal factors responsible for amphibian declines. Due to differences in life history characteristics, high altitude populations may be less resilient than their lowland counterparts and subsequently may be more vulnerable to extinction. Consequently, the main aim of this study was to determine whether altitude influenced life history characteristics and ultimately population resilience of anurans in the southeast Queensland region. Six anuran species; Litoria chloris, L. lesueuri, L. pearsoniana (Anura: Hylidae), Mixophyes fasciolatus, M. fleayi and M. iteratus (Anura: Myobatrachidae) were studied over three field seasons (1997-1999) in 18 sites of varying altitude (100-950m) in the southeast Queensland region. The life history characteristics examined were: activity and breeding season length, fecundity and egg size, number of clutches produced per season, tadpole growth and development rates, longevity, age at maturity, reproductive life span, average lifetime fecundity, survival and recapture rates. The data were collected using a combination of field-based surveys (body sizes, clutch sizes, and survival and recapture rates), museum specimen dissections (clutch and egg sizes), reciprocal transplant field experiments (tadpole growth and development rates) and skeletochronology (longevity, age at maturity, reproductive lifespan and average lifetime fecundity). On average, high altitude populations of all species had shorter breeding and activity seasons than low altitude populations (up to 10 weeks less in some cases). The magnitude of the difference in breeding season length varied among years depending on the average temperature and rainfall for the year; i.e. differences appeared greater in warmer and wetter years. Within a population males had longer breeding and activity seasons than females. Although breeding season length varied with altitude, the number of nights that individuals were active within the breeding season did not vary; i.e. low altitude populations were not active for more nights despite having a longer breeding season. This result was attributed to the absence of a relationship between individual activity and environmental variables (air temperature, rainfall, etc.) in many of the populations. Generally, intraspecific clutch size did not vary significantly with altitude. This result was due to the absence of a significant relationship between female body size and altitude (as clutch size is proportional to female body size). Egg size also did not vary with altitude however, suggesting egg size may be canalized (i.e. fixed) in these species. Results also suggest that females of these species only produce one clutch of eggs per season. Interspecific differences in reproductive characteristics largely reflected differences in reproductive mode, larval habitat and female body size. Altitude negatively influenced growth and development rates in L. chloris and development rates in L. pearsoniana. Tadpoles raised at high altitudes were also generally larger at each Gosner Development Stage in both species. The results of the reciprocal transplant experiments suggested that most of the variation in growth and development rates was due to environmental factors (water temperature) rather than genetic or maternal factors. Altitude or genetic factors did not significantly affect tadpole survival in either species. The results suggest that tadpoles occurring at high altitudes take longer to reach metamorphosis and do so at a larger size than their lowland counterparts. With the exception of L. lesueuri, skeletochronology was suitable for age estimation in the study species. Altitude had a significant effect on the age at maturity or longevity in some of the species, however there were trends toward older individuals and older ages at maturity in high altitude populations for the remaining species. Females were generally older than males for all species and in the case of longer-lived species (i.e. Mixophyes spp.) also tended to be older when breeding for the first time. The large overlap of body sizes of individuals of different ages demonstrates that body size is a poor indicator of age in these species. This is the first study to estimate average lifetime fecundity for more than one amphibian species and/or population. The results suggest that the absence of significant altitudinal variation in the average lifetime fecundity of different populations is due to tradeoffs made by females (current reproduction vs. survival). There was no significant altitudinal variation in annual survival and recapture rates in any of the species, and generally there was no difference in the survival and recapture rates of males and females in each population. Within a year, monthly survival and recapture rates were more variable at low than high altitudes and this was attributed to the longer breeding season of low altitude populations. The results did not support previous studies that suggested there was a size bias in survival and recapture rates. The shorter breeding seasons, slower growth and development rates, older age at maturity and greater longevity found in the high altitude study populations will result in increased generation time in those populations. In turn, increased generation time can cause high altitude populations to be less resilient (i.e. population takes longer to return to equilibrium after a disturbance away from equilibrium) (Pimm et al. 1988, Pimm 1991) and ultimately more vulnerable or prone to extinction or decline. The majority of unexplained global amphibian declines have occurred at high altitudes in tropical and subtropical areas. These latitudinal patterns may be explained by the narrow range of environmental tolerances exhibited by tropical organisms resulting in mountains being effectively “higher” in the tropics. Consequently, high altitude tropical species are likely to be even more vulnerable than temperate species occurring at similar altitudes. Further work on the effects of geographic variation, especially interactions between altitude and latitude are needed to evaluate the hypotheses for the causes of these declines and disappearances.Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Environmental and Applied Science
Science, Environment, Engineering and Technology
Full Text
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Mohd, Abdullah Maizah. "Ecological Studies of the Mangrove-Associated Meiofauna in Southeast Queensland, Australia". Thesis, Griffith University, 2016. http://hdl.handle.net/10072/367507.
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Meiofauna are ubiquitous but poorly-studied components of soft-bottom marine communities around the world, including mangroves. However, information on the ecological role of the meiofauna in subtropical intertidal habitats is scarce compared to knowledge of the benthic macrofauna. The dynamic environmental conditions and heterogeneous sediments of mangroves present challenges to understanding the structure of mangrove meiofaunal assemblages at various spatial and temporal scales. This study was designed to elucidate the ecological role of the meiofauna in mangroves by studying their three main ecological elements: 1) assemblages structure; 2) top-down interaction with macrofauna; and 3) bottom-up interaction in terms of nutrient utilisation.
Firstly, how meiofaunal assemblage respond to estuarine sediment conditions was described by analysing the assemblages associated with different mangrove species (Avicennia marina, Rhizophora stylosa and Aegiceras corniculatum) at three locations in sub-tropical Southeast Queensland, Australia. Secondly, the significance and nature of top-down control on the density of meiofauna based on their interactions with deposit- feeding crabs was investigated in a mangrove and the adjoining sandflat.Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
Griffith School of Environment
Science, Environment, Engineering and Technology
Full Text
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Felemban, Ohood Othman. "Infection Prevention and Control Programs in Community-Based Home Visiting Nursing in Southeast Queensland, Australia: A Case Study". Thesis, Griffith University, 2015. http://hdl.handle.net/10072/367412.
Pełny tekst źródłaStreszczenie:
In Australia, healthcare settings are required to obtain and maintain formal accreditation by the Australian Council on Health Care Standards. One area of this accreditation is infection prevention and control. In addition to accreditation, healthcare settings are required to appoint an infection control professional to coordinate the local infection control programs. In addition to these requirements, healthcare settings in Queensland are required by law to implement an infection control management plan and take reasonable precautions to minimise the risk of Healthcare-Associated Infections [HAIs] through the identification of the infection risks and measures to be taken to prevent or minimise these risks. Such efforts must be consistent with relevant national infection control guidelines for healthcare settings. The National Health and Medical Research Council [NHMRC] published the Australian Guidelines for the Prevention and Control of Infection in Healthcare in which they established six key elements of a successful infection prevention and control program. The NHMRC guidelines are considered to be fundamental because they are based on the best available evidence and address the critical aspects of infection prevention and control in healthcare settings. The NHMRC guidelines are hospital-based. Donabedian’s theory was used as a conceptual structure for this study. The structure, processes and outcome strategies of infection prevention and control programs in CBHVN was explored in each organisation. The findings reveal that infection prevention and control programs were informally structured in CBHVNThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Nursing and Midwifery
Griffith Health
Full Text
Książki na temat "Southeast Queensland"
1
Steele, J. G. Aboriginal pathways: In southeast Queensland and the Richmond River. St. Lucia: University of Queensland Press, 1987.
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2
Kite, Suzanne. The Duunidjawu language of southeast Queensland: Grammar, texts and vocabulary. Canberra, A.C.T., Australia: Pacific Linguistics, Research School of Pacific and Asian Studies, The Australian National University, 2004.
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3
Roger, Ford. Indigenous peoples of southeast Queensland: An annotated guide to ethno-historical sources. Woolloongabba, Qld: FAIRA Aboriginal Corporation, 1998.
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4
Reed, L. The keeping place: An annotated bibliography and guide to the study of the Aborigines and Aboriginal culture in Northeast New South Wales and Southeast Queensland. Lismore, N.S.W: North Coast Institute for Aboriginal Community Education, 1988.
Znajdź pełny tekst źródłaCzęści książek na temat "Southeast Queensland"
1
Dunn, Ryan J. K., Nathan J. Waltham, Nathan P. Benfer, Brian A. King, Charles J. Lemckert i Sasha Zigic. "Gold Coast Broadwater: Southern Moreton Bay, Southeast Queensland (Australia)". W Estuaries of the World, 93–109. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-7019-5_6.
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2
Davidson, James, i Samuel Bowstead. "Going with the Flow: Building Resilience in Southeast Queensland". W Sustainable Coastal Design and Planning, 351–67. Boca Raton, FL : Taylor & Francis, 2018.: CRC Press, 2018. http://dx.doi.org/10.1201/9780429458057-25.
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3
Hubble, Thomas, Jody Webster, Phyllis Yu, Melissa Fletcher, David Voelker, David Airey, Samantha Clarke i in. "Submarine Landslides and Incised Canyons of the Southeast Queensland Continental Margin". W Submarine Mass Movements and their Consequences, 125–34. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-20979-1_12.
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4
Dickson, T., R. L. Aitken i P. W. Moody. "Crop response to amendments on two high manganese soils in southeast Queensland". W Plant-Soil Interactions at Low pH: Principles and Management, 549–53. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0221-6_84.
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5
YANG, SHU-QING. "FEASIBILITY STUDY OF COASTAL RESERVOIR FOR WATER SUPPLY TO SOUTHEAST QUEENSLAND, AUSTRALIA". W Asian And Pacific Coasts 2011, 415–23. WORLD SCIENTIFIC, 2011. http://dx.doi.org/10.1142/9789814366489_0047.
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6
Connors, Libby. "Women, Children and Violence in Aboriginal Law: Some Perspectives From the Southeast Queensland Frontier". W Past Law, Present Histories. ANU Press, 2012. http://dx.doi.org/10.22459/plph.09.2012.07.
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Spearritt, Peter. "The water crisis in Southeast Queensland: How desalination turned the region into carbon emission heaven". W Troubled Waters: Confronting the Water Crisis in Australia’s Cities. ANU Press, 2008. http://dx.doi.org/10.22459/tw.06.2008.02.
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Wang, X., Y. Khoo i C. Wang. "Risk-based cost/benefit assessment and decision-making for residential housing adapting to increasing risks under storm-tide inundation due to sea level rise in Southeast Queensland, Australia". W Safety, Reliability, Risk and Life-Cycle Performance of Structures and Infrastructures, 1559–64. CRC Press, 2014. http://dx.doi.org/10.1201/b16387-228.
Pełny tekst źródłaStreszczenia konferencji na temat "Southeast Queensland"
1
Kelly, Joshua T., Sarah McSweeney, Sarah McSweeney, James Shulmeister, James Shulmeister, Allen Gontz i Allen Gontz. "THE IMPACT OF CLIMATE CHANGE ON SHORELINE DYNAMICS ALONG SOUTHEAST QUEENSLAND, AUSTRALIA". W GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-318345.
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2
Flottman, Thomas, Sam Brooke-Barnett, Rod Trubshaw, Sai-Krishna Naidu, Elliot Kirk-Burnnand, Pijush Paul, Seth Busetti i Peter Hennings. "Influence of in Situ Stresses on Fracture Stimulation in the Surat Basin, Southeast Queensland". W SPE Unconventional Resources Conference and Exhibition-Asia Pacific. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/167064-ms.
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3
Cinar, Yildiray, Jacques Sayers, Peter Ross Neal i William Guy Allinson. "Geo-engineering and Economic Assessment of a Potential Carbon Capture and Storage Site in Southeast Queensland, Australia". W Asia Pacific Oil and Gas Conference and Exhibition. Society of Petroleum Engineers, 2007. http://dx.doi.org/10.2118/108924-ms.
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4
Gontz, Allen, Daniel Ellerton, James Shulmeister, Joshua T. Kelly, Adrian McCallum, Patrick A. Hesp, Graziela Minot da Sliva, Talitha Santini, Kevin Welsh i Tammy Rittenour. "STRATIGRAPHIC ARCHITECTURE OF THE FRASER ISLAND DUNE COMPLEX, SOUTHEAST QUEENSLAND, AUSTRALIA USING HIGH-RESOLUTION GROUND PENETRATING RADAR". W GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303721.
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Gontz, Allen, Daniel Ellerton i Graziela Miot da Silva. "EVIDENCE OF TOPOGRAPHIC STEERING OF WINDS IN A SMALL, COASTAL BLOWOUT, SOUTHEAST QUEENSLAND – APPLICATIONS OF GPR AND PALAEOCLIMATE". W GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-322775.
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Gontz, Allen, Daniel Ellerton, James Shulmeister i Adrian McCallum. "GPR FACIES FROM THE WORLD’S LONGEST CONTINUALLY ACTIVE COASTAL SAND DUNE SYSTEM, GREAT SANDY COAST, SOUTHEAST QUEENSLAND AUSTRALIA – EVIDENCE FOR CHANGE". W 115th Annual GSA Cordilleran Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019cd-329540.
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