Relevant bibliographies by topics / Bowen Basin

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Academic literature on the topic 'Bowen Basin'

Author: Grafiati
Published: 4 June 2021
Last updated: 26 January 2023

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Journal articles on the topic "Bowen Basin"

1

Benfell, Kathy E., B. Basil Beamish, Peter J. Crosdale, and K. A. Rodgers. "Combustion behaviour of Bowen Basin coals." Fuel Processing Technology 60, no. 1 (June 1999): 1–14. http://dx.doi.org/10.1016/s0378-3820(99)00037-5.

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Danis, Cara. "Sydney–Gunnedah–Bowen Basin deep 3D structure." Exploration Geophysics 43, no. 1 (March 2012): 26–35. http://dx.doi.org/10.1071/eg11043.

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Bell, R. M. "METHANE DRAINAGE POTENTIAL OF THE NORTHERN BOWEN BASIN." APPEA Journal 27, no. 1 (1987): 281. http://dx.doi.org/10.1071/aj86022.

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Large volumes of methane plus some other gases are generated during the coalification process. Under suitable conditions some of this gas is adsorbed within the microporosity of coals. The rate at which the gas can desorb is a function of the permeability, degree of fracturing or cleating, moisture content, geochemistry of the coals, and the pressure differential. Flow rates from coals are generally low but can be dramatically improved by artificial stimulation and techniques such as lateral drilling.Methane drainage or coal de-methanisation has been carried out for many years, primarily for safety reasons. The resource value of methane in coal seams is now being recognised and considerable research is being undertaken both overseas and in Australia.In the Northern Bowen Basin, several million tonnes of coal are mined each year. The main seams of the Permian Collinsville, Moranbah, German Creek, and Rangal Coal Measures are generally thick and laterally extensive. The area north of Blackwater probably contains more than 100 billion tonnes of coal from which several hundred billion m3 (several Bcf) methane could conceivably be recovered in those areas where the coals are too deep for commercial exploitation.The coals of the Northern Bowen Basin are considered to have better physical parameters for the commercial development of methane drainage projects than those of the central and southern Bowen Basin where methane drainage projects were undertaken several years ago. It is estimated that more than 85 million m3 (3 Bcf) of recoverable gas per square km could be present in some areas. This gas can probably be produced for less than $1.50/GJ (1 Mcft, a figure which compares favourably with many conventional natural gas sources.The Northern Bowen Basin is well-situated with respect to potential gas markets at Townsville and Gladstone. The gas could also be used as a chemical feedstock for products such as ammonia, fertilisers, explosives or synfuels, with the plants located close to the producing wells, thus significantly reducing gas transport costs.
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Beeston, J. W. "Coal rank variation in the Bowen Basin, Queensland." International Journal of Coal Geology 6, no. 2 (July 1986): 163–79. http://dx.doi.org/10.1016/0166-5162(86)90019-4.

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Babaahmadi, Abbas, Renate Sliwa, and Joan Esterle. "Post Jurassic shortening in the western Surat Basin relative to underlying basement depth and faulting." APPEA Journal 56, no. 2 (2016): 597. http://dx.doi.org/10.1071/aj15103.

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The Hutton-Wallumbilla (HWF), Merivale (MF), Kia Ora, and Injune faults are the major structures in the western Surat Basin, deforming Palaeozoic to Jurassic rock units. The authors present results from the interpretation of gridded gravity data and open-file seismic reflection data, which provide constraints on the geometry and kinematics of these faults. The interpretation of gravity data indicates that the HWF and MF are expressed by sharp lineaments in moderate to high-amplitude anomalies, indicating a deep-seated nature of the faults. The interpretation of seismic lines shows that the HWF and MF are northeast-dipping and east-dipping reverse blind faults, respectively. Some other faults also displaced and folded the rock units of the Bowen and Surat basins, such as the Kia Ora and Injune faults. The MF, Kia Ora, and the northern part of the HWF acted as normal faults during the early Permian and then have been inverted during the Late Permian–Triassic Hunter-Bowen Orogeny phases, especially during the early Late Triassic. The largest fault throws in the Bowen Basin successions are observed along the southern part of the HWF and its central splay, which are around 350 m and 480 m, respectively. The stratigraphic units of the Surat Basin above it have gently been folded over the major blind faults. The largest amount of shortening in the Surat Basin has taken place over the southern part of the HWF by 0.5%. The basement depth played an important role in the amount of contractional deformation in the Bowen and Surat basins. Where the basement is shallow, the amount of deformation along the faults in both the Bowen and Surat basins is higher.
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Riley, J. M. "THE RISE AND RISE OF COAL SEAM GAS IN THE BOWEN BASIN." APPEA Journal 44, no. 1 (2004): 647. http://dx.doi.org/10.1071/aj03032.

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The coal seam gas (CSG) industry has been active in Australia for almost three decades, with interest largely focussed on the Bowen and Sydney basins. Sporadic activity has also occurred in a number of other areas including the Galilee, Ipswich, Clarence–Moreton, Gunnedah, Gloucester, and Otway basins to name a few, with significant recent interest shown in the promising Surat Basin. Of these basins it is the Bowen Basin in eastern central Queensland which has continued to shine as the premier coal seam gas province in the country.From humble beginnings in the mid-1970s in the Moura area, CSG from the Bowen Basin now supplies around 20% of Queensland gas demand. Since the start of commercial production from the basin in 1996, production has grown to about 20 PJ per year from five separate fields, with three new fields under construction expected to more than double this volume over the next 2–3 years.The largest contribution to this growth will come from the Comet Ridge region which is proving itself to be a world class CSG deposit. The high-productivity fairway in the south of the region extends over an area about 80 km long and 20 km wide and includes the Tipperary Fairview field, and the Origin Energy Spring Gully project. In the last year proved and probable gas reserves have more than doubled to 1,500 PJ across the fairway, with upside recoverable gas estimated to be 4,700 PJ. The rapid rate of CSG reserves increase in the Bowen Basin demonstrates the key role this industry will play in the eastern Australia gas market.
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Draper, J. J., and C. J. Boreham. "GEOLOGICAL CONTROLS ON EXPLOITABLE COAL SEAM GAS DISTRIBUTION IN QUEENSLAND." APPEA Journal 46, no. 1 (2006): 343. http://dx.doi.org/10.1071/aj05019.

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Methane is present in all coals, but a number of geological factors influence the potential economic concentration of gas. The key factors are (1) depositional environment, (2) tectonic and structural setting, (3) rank and gas generation, (4) gas content, (5) permeability, and (6) hydrogeology. Commercial coal seam gas production in Queensland has been entirely from the Permian coals of the Bowen Basin, but the Jurassic coals of the Surat and Clarence-Moreton basins are poised to deliver commercial gas volumes.Depositional environments range from fluvial to delta plain to paralic and marginal marine—coals in the Bowen Basin are laterally more continuous than those in the Surat and Clarence-Moreton basins. The tectonic and structural settings are important as they control the coal characteristics both in terms of deposition and burial history. The important coal seam gas seams were deposited in a foreland setting in the Bowen Basin and an intracratonic setting in the Surat and Clarence-Moreton basins. Both of these settings resulted in widespread coal deposition. The complex burial history of the Bowen Basin has resulted in a wide range of coal ranks and properties. Rank in the Bowen Basin coal seam gas fields varies from vitrinite reflectance of 0.55% to >1.1% Rv and from Rv 0.35-0.6% in the Surat and Clarence-Moreton basins in Queensland. High vitrinite coals provide optimal gas generation and cleat formation. The commercial gas fields and the prospective ones contain coals with >60% vitrinite.Gas generation in the Queensland basins is complex with isotopic studies indicating that biogenic gas, thermogenic gas and mixed gases are present. Biogenic processes occur at depths of up to a kilometre. Gas content is important, but lower gas contents can be economic if deliverability is good. Free gas is also present. Drilling and production techniques play an important role in making lower gas content coals viable. Since the Bowen and Surat basins are in a compressive regime, permeability becomes a defining parameter. Areas where the compression is offset by tensional forces provide the best chances for commercial coal seam gas production. Tensional setting such as anticline or structural hinges are important plays. Hydrodynamics control the production rate though water quality varies between the fields.
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Draper, John, Atsushi Aoki, Nirou Okamoto, Hiroshi Karashima, Hideo Aoyama, Masayoshi Tanoue, Takao Aizawa, Ken-ichi Yamazaki, and Mark Covington. "Geophysical studies in the Bowen Basin: a collaborative approach." ASEG Extended Abstracts 2004, no. 1 (December 2004): 1–4. http://dx.doi.org/10.1071/aseg2004ab035.

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Godber, Kate E., James Reid, and Guy LeBlanc Smith. "Application of Airborne EM to Bowen Basin Coal Projects." ASEG Extended Abstracts 2012, no. 1 (December 2012): 1–4. http://dx.doi.org/10.1071/aseg2012ab205.

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Campbell, M. J., U. Shaanan, and C. Verdel. "Fold-interference patterns in the Bowen Basin, northeastern Australia." Australian Journal of Earth Sciences 64, no. 5 (June 18, 2017): 577–85. http://dx.doi.org/10.1080/08120099.2017.1334704.

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Dissertations / Theses on the topic "Bowen Basin"

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Pattison, Christopher Ian. "Igneous intrusions in the Bowen Basin." Thesis, Queensland University of Technology, 1990. https://eprints.qut.edu.au/35967/1/35967_Pattison_1990.pdf.

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Igneous intrusions, in the form of stocks, sills and dykes are abundant in the Bowen Basin. They are predominantly Early Cretaceous in age, exclusively epizonal in origin and range in composition from dolerite to granodioriteldacite. All rock units within the basin, up to and including the Clematis Group, are intruded to some degree. This study assesses the distribution, form, petrology and mode of emplacement of plutons, igneous sills and dykes occurring in the Bowen Basin, and considers their relationship to the prevailing structure. The tectonic implications of the findings are then assessed. Igneous sills occur in two geographically distinct domains, one in the northern Bowen Basin and the other in the central Bowen Basin. The sills emanated from pre-existing, north to north-northwest trending reverse faults, and preferentially intruded coal seams. The boundaries to sill intrusion are marked by major northeast trending basement structures. These basement structures occur at regular intervals throughout the basin, and correspond with the localisation of plutonic and dyke activity, anomalous structural disturbance, and changes in the gross structure of the basin. They are interpreted as transfer faults that were inherited from an Early Permian, basin-forming extensional episode. Petrological evidence indicates that the plutons and sills occurring in the northern Bowen Basin are petrogenetically related, and that a progressive variation in their chemistry occurs across the axis of the basin from east to west. Intrusions in the east belong to the calc-alka1ine rock suite, while those in the west belong to the syenitic suite. This transition is inte1preted in terms of increased crustal contamination as the magma migrated from a source area to the east along a buried, shallow-dipping detachment surface that extends under the basin. This detachment was inherited from the above mentioned extensional phase and is intimately linked to structures that penetrate up-section through the basin succession. Reactivation of the transfer faults during the Early Cretaceous initiated the emplacement of dykes, and the synchronous development of northeast trending normal and wrenchstyle faults. The dykes exhibit characteristics that indicate they were self-propagating, and can be regarded as good palaeostress indicators. This phase corresponded with a major compressional event that involved the reactivation of pre-existing thrust structures, deformation of the Folded Zone and eastern margins of the Nebo Synclinorium and Mimosa Syncline, and the rapid preferential uplift of the central Bowen Basin region.
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Al-Arouri, Khaled R. "Petroleum geochemistry, source rock evaluation and modelling of hydrocarbon generation in the southern Taroom Trough, with particular reference to the Triassic Snake Creek Mudstone /." Title page, abstract and contents only, 1996. http://web4.library.adelaide.edu.au/theses/09PH/09pha321.pdf.

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Best, Heidi Ann. "Sedimentology, sequence stratigraphy and reservoir potential of the Warrinilla Field, Bowen Basin /." Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bb561.pdf.

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Othman, Rushdy School of Biological Earth &amp Environmental Sciences UNSW. "Petroleum geology of the Gunnedah-Bowen-Surat Basins, Northern New South Wales : stratigraphy, organic petrology and organic geochemistry." Awarded by:University of New South Wales. School of Biological, Earth and Environmental Sciences, 2003. http://handle.unsw.edu.au/1959.4/20537.

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The three-dimensional thermal maturity pattern has been investigated and the hydrocarbon generation potential assessed for the Permian and Triassic sequences of the southern Bowen and northern Gunnedah Basins and the lower part of the overlying Jurassic Cretaceous Surat Basin sequence in northern New South Wales. An oil-source rock correlation also has been investigated in the Gunnedah Basin. Vitrinite reflectance measurements were conducted on 256 samples from 28 boreholes. A total of 50 of these samples were subjected to Rock-Eval pyrolysis analysis, and 28 samples extracted for additional organic geochemical studies (GCMS). A re-evaluation of the stratigraphy in the southern Bowen Basin and a stratigraphic correlation between that area and the northern Gunnedah Basin was also included in the study. An overpressured shaly interval has been identified as a marker bed within the lower parts of the Triassic Moolayember and Napperby Formations, in the Bowen and Gunnedah Basins respectively. Suppressed vitrinite reflectance in the Permian sequence was used as another marker for mapping the stratigraphic sequence in the southern Bowen Basin. The Permian sequence in the Bowen Basin thins to the south, and probably pinches out over the Moree High and also to the west. The coal-bearing Kianga Formation is present in the north and northeastern parts of the study area. A disconformity surface between Digby and Napperby Formations in the Gunnedah Basin is probably time-equivalent to deposition of the Clematis Group and Showgrounds Sandstone in the Bowen Basin. The Clematis Group is absent in the study area, and the Moolayember Formation considered equivalent to the Napperby Formation. Although in many cases core samples were not available, handpicking of coal or shaly materials from cuttings samples where geophysical log signatures identify these materials helped in reducing contamination from caved debris. Histogram plots of reflectance also helped where the target and caved debris were of similar lithology. Vertical profiles of the vitrinite reflectance identified suppressed intervals in the study area due to marine influence (Back Creek Group and Maules Creek Formation) and liptinite rich source organic matter (Goonbri Formation). The suppression occurs due to the perhydrous character of the preserved organic matter. High reflectance values were noted within intrusion-affected intervals, and two types of igneous intrusion profiles were identified; these are simple and complex profiles. An isoreflectance map for the non-suppressed interval at the base of the Triassic sequence in the southern Bowen Basin shows that the organic matter is mature more towards the east close to the Goondiwindi Fault, and also towards the west where the Triassic sequence directly overlies the basement. High values also occur over the Gil Gil Ridge in the middle, to the south over the Moree High, and to the north where the sequence is thicker. The reflectance gradient in the suppressed intervals is higher than in the overlying non-suppressed sequences, especially when the rank has resulted from burial depth. Tmax from Rock-Eval pyrolysis was found to be lower in the perhydrous intervals, and was high in mature and igneous intrusion-affected intervals. Based on the source potential parameters, the Permian Back Creek Group is a better source than the Kianga Formation, while the Goonbri Formation is better than the Maules Creek Formation. The Triassic Napperby Formation has a fair capacity to generate oil, and is considered a better source rock than the equivalent Moolayember Formation. The Jurassic Walloon Coal Measures is a better source than Evergreen Formation, and has the best source rock characteristics, but is immature. The Rock-Eval S1 value shows better correlation with extracted hydrocarbon compounds (saturated and aromatics) than the total extractable organic matter. This suggests that solvent extraction has a greater ability to extract NSO compounds than temperature distillation over the Rock-Eval S1 interval. Terrestrial organic matter is the main source input for the sequences studied. This has been identified from organic petrology and from the n-alkane distributions and the relatively high C29 steranes and low sterane/hopane ratios. The absence of marine biomarker signatures in the Permian marine influenced sequence, could be attributed to their dilution by overwhelming amounts of non-marine organic matter. A mainly oxic to suboxic depositional environment is inferred from trace amounts of 25-NH, BNH and TNH. This is further supported by relatively high pr/ph ratios. Although C29/C30 is generally regarded as an environmental indicator, high values were noted in intrusion-affected samples. The 22S and 20S ratios were inverted ????reaches pseudo-equilibrium???? in such rapidly heated, high maturity samples. The ratio of C24 tetracyclic terpane to C21-C26 tricyclic terpanes decreases, instead of increasing, within the Napperby Formation close to a major igneous intrusive body. The 22S ratio, which is faster in reaction than the other terpane and sterane maturity parameters, shows that the Permian sequence lies within the oil generation stage in the Bowen Basin, except for a Kianga Formation sample. The Triassic sequence is marginally mature, and the Jurassic sequence is considered immature. In the Gunnedah Basin, the Permian sequence in Bellata-1 and Bohena-1, and the Triassic sequence in Coonarah-1A, lie within the oil generation range. In the intrusion-affected high maturity samples, the ratio is reaches pseudo-equilibrium. This and other terpane and sterane maturity parameters are not lowered (suppressed) in the perhydrous intervals. The ???????? sterane ratio, however, is slowest in reaction to maturity, and variations in low maturity samples are mainly due to facies changes. Diasterane/sterane ratios, in the current study, increase with increasing TOC content up to 5% TOC, but decrease in rocks with higher TOC contents including coals. Highly mature samples, as expected, in both cases are anomalous with high ratios. Calculated vitrinite reflectance based on the method of Radke and Welte (1983), as well as MPI 1 and MPI 2, shows the best comparison to observed values. These aromatic maturity parameters are lowered within the reflectance-suppressed intervals. Oil stains in the Jurassic Pilliga Sandstone in the Bellata-1 well have been identified as being indigenous and not due to contamination. The vitrinite reflectance calculated to the oil stain suggests that the source rock should be within a late mature zone. Such high maturity levels are only recognised within intrusion-affected intervals. A close similarity between the oil stain sample and the intruded interval of the Napperby Formation is evident from the thermal maturity and biomarker content. Hydrocarbon generation and expulsion from the lower part of the Napperby Formation as a result of igneous intrusion effects is suggested as the source of the oil in this particular occurrence. Terpane and sterane maturity parameters increase with increasing burial depth in the intervals with suppressed (perhydrous) vitrinite reflectance. The generation maturity parameters also increase through intervals with perhydrous vitrinite, which suggests that hydrocarbons continue to be generated and the actual amount is increasing even though traditional rank ????????????stress???????????? maturity parameters are lowered. Accordingly, the Permian sequences in the lower part of the Bowen Basin are at least within the peak oil generation zone, and probably within late oil generation in the north and northeast of the study area. To generate significant amounts of hydrocarbon, however, the thickness of the shaly and coaly intervals in the Permian sequence is probably a critical parameter. In the Gunnedah Basin, a significant amount of hydrocarbon generation is probably only possible as a result of igneous intrusions.
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Gillam, Daniel J. "Structural and geomechanical analysis of naturally fractured hydrocarbon provinces of the Bowen and Amadeus Basins: onshore Australia /." Title page, table of contents and abstract only, 2004. http://web4.library.adelaide.edu.au/theses/09PH/09phg4758.pdf.

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Coffin, Lindsay M. "Sedimentology, Stratigraphy and Petrography of the Permian-Triassic Coal-bearing New Lenton Deposit, Bowen Basin, Australia." Thèse, Université d'Ottawa / University of Ottawa, 2013. http://hdl.handle.net/10393/23998.

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The Bowen Basin is one of the most intensely explored sedimentary basins in Australia and hosts one of the world’s largest coking coal deposits. This study focuses on the Lenton deposit in the north-central part of the Bowen Basin and targets the Rangal Coal Measures, which are the youngest (245 Ma), most areally extensive and least structurally deformed coal measures in the study area. Six lithofacies were identified from detailed bed-by-bed logging of two cores and stratigraphically-upward comprise peatmire deposits of the Permian Blackwater Group overlain unconformably by braided fluvial strata of the Triassic Rewan Group. Coal-bearing strata of the Blackwater Group form a large-scale drying up sequence showing a change from permanent to seasonal waterlogged conditions related to the onset of regional uplift. Sedimentation was then terminated and a regional erosion surface formed by uplift related to the Hunter Bowen Orogeny. This, then, was overlain by braided fluvial strata of the Triassic Rewan Group.
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McConachie, Bruce Alan. "A Geological study of the South Walker Creek coalfield and its setting within the Northern Bowen Basin, Queensland." Thesis, Queensland University of Technology, 1985. https://eprints.qut.edu.au/35971/1/35971_McConachie_1985_vol-1.pdf.

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The Rangal Coal Measures are the uppermost coal bearing formation of the late Permian Blackwater Group in the North Bowen Basin, Queensland. They are conformably overlain by the Early Triassic Rewan Group and themselves conformably overlie the tuffaceous Fort Cooper Coal Measures. Throughout the North Bowen Basin one or two important coal seams are present within the Rangal Coal Measures. At South Walker Creek these seams are high rank, low ash, inertinite-rich coals attaining individual thicknesses up to 12 metres. The South Walker Creek Coalfield is unique in the North Bowen Basin because it contains an extensive reserve of potential opencut coal with poor coking characteristics, and very limited prospect for use as an export steaming coal in current overseas markets. It would, however, be ideal for use in a dedicated power station. Based on work from two GSQ drillholes, limited outcrop information, and some 370 chip hole logs compiled into a computer data base, it has been possible to produce a detailed model of the South Walker Creek Coalfield. This model helps to place the Rangal Coal Measures within the structural setting of the region while at the same time providing a framework for detailed mine planning. In the South Walker Creek region, the Rangal Coal Measures consist of lithic sandstone, mudstone, and siltstone plus rare conglomerate, (all derived from a metamorphic and volcanic provenance to the north and east) and coal. From the cored drillhole data and observations of the sparse outcrop, it has been possible to identify several lithofacies which can be related to a flood plain environment. This interpretation is based on the lithology, texture, grainsize, internal bedding structures and vertical lithofacies exhibit erosional bases in core and deposits, other than intraformational associations. The sandstones outcrop, although pebble lag mudstones and peat "rip-up" clasts, are rare. Massive and fining upward sequences predominate with trough cross-bedding being common in outcrop. The sandstone/shale ratio is approximately equal throughout the South Walker Creek Coalfield. A lateral lithofacies distribution can be clearly interpreted from the South Walker Creek isopachs and cross-sections through the interseam material. These indicate relatively fixed sandstone channel positions and an anastomosing distribution pattern with substantial fine grained overbank deposits. Several faults in the area can be related to these paleochannel margins. Prodeltaic or marine sequences have not been recognised within the Rangal Coal Measures or within contemporaneous sequences throughout the South Walker Creek region. On the basis of the lithofacies present, a flood plain environment is suggested as the likely depositional setting. The most important coal seam at South Walker Creek represents a thick, low ash, widely distributed peat accummulation. This was terminated over much of the area by predominantly vertically accreted fluvial deposits up to 60 metres thick associated with an anastomosing channel system. Following this, widespread peat swamp conditions recurred. A possible mechanism to account for interseam sedimentation at South Walker Creek is avulsion initiated by levee breaching during a flood peak.
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Trueman, Jonathon David. "Stratigraphy and sedimentology of the Burdekin Delta, Queensland and comparisons with Permian coastal facies in the Denison Trough, SW Bowen Basin, Australia /." St. Lucia, Qld, 2002. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe17342.pdf.

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Butler, James Henry. "Cyclic Salinity Model for deposition of large-scale coal deposits." Thesis, Queensland University of Technology, 2015. https://eprints.qut.edu.au/84926/1/James%20Butler%20Thesis.pdf.

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Existing field data for Rangal coals (Late Permian) of the Bowen Basin, Queensland, Australia, are inconsistent with the depositional model generally accepted in the current geological literature to explain coal deposition. Given the apparent unsuitability of the current depositional model to the Bowen Basin coal data, a new depositional model, here named the Cyclic Salinity Model, is proposed and tested in this study.
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Rüping, Katherina B. "Quantifizierung von Bodentonmineralen auf der Basis einer Komplexen Mineralogischen Phasenanalyse /." Tönning [u.a.] : Der Andere Verlag, 2007. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=016441524&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA.

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Books on the topic "Bowen Basin"

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Parfrey, S. M. Biostratigraphy of the Barfield Formation, southeastern Bowen Basin, with a review of the fauna from the Ingelara and lower Peawaddy Formation, southwestern Bowen Basin. Brisbane, Australia: Queensland Dept. of Mines, 1988.

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Mallett, C. W. An illustrated field guide to the coal measure rocks of the Bowen Basin. Lucia, Qld: Division of Geomechanics, Institute of Minerals, Energy and Construction, 1989.

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Briggs, D. J. C. Permian Productidina and Strophalosiidina from the Sydney-Bowen Basin and New England orogen: Systematics and biostratigraphic significance. Canberra: Association of Australasian Palaeontologists, 1998.

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Fielding, C. R. Geology of the Bowen and Surat Basins, eastern Queensland. [Sydney]: Geological Society of Australia, 1996.

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Targan, Stephan R. Inflammatory bowel disease: Translating basic science into clinical practice. Chichester, West Sussex, UK: Wiley-Blackwell, 2010.

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R, Targan Stephan, Shanahan Fergus, and Karp Loren C, eds. Inflammatory bowel disease: Translating basic science into clinical practice. Chichester, West Sussex: Blackwell Pub., 2010.

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H, Goebell, ed. Inflammatory bowel disease: Progress in basic research and clinical implications. Dordrecht, Netherlands: Kluwer Academic Publishers, 1991.

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L, Sutherland, Axcan Pharma, Crohn's and Colitis Foundation of Canada., and Canadian Association of Gastroenterology, eds. Inflammatory bowel disease: Basic research, clinical implications, and trends in therapy. Dordrecht: Kluwer Academic Publishers, 1994.

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Turbyfill, Harold. Basic string maintenance: A teacher's guide. Fairfax, VA: American String Teachers Association [with National School Orchestra Association, 2005.

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F, Colombel J., ed. Inflammatory bowel disease: Translation from basic research to clinical practice. Dordrecht: Springer, 2004.

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Book chapters on the topic "Bowen Basin"

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Golding, S. D., K. D. Collerson, I. T. Uysal, M. Glikson, K. Baublys, and J. X. Zhao. "Nature and source of carbonate mineralization in Bowen Basin coals, Eastern Australia." In Organic Matter and Mineralisation: Thermal Alteration, Hydrocarbon Generation and Role in Metallogenesis, 296–313. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-015-9474-5_14.

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Golding, S. D., K. A. Baublys, M. Glikson, I. T. Uysal, and C. J. Boreham. "Source and Timing of Coal Seam Gas Generation in Bowen Basin Coals." In Coalbed Methane: Scientific, Environmental and Economic Evaluation, 257–69. Dordrecht: Springer Netherlands, 1999. http://dx.doi.org/10.1007/978-94-017-1062-6_15.

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Li, Ming, Yuxia Ma, Xiangwen Kong, Zhaohui Xia, and Houqin Zhu. "Seismic Application in Australia Bowen Basin CBM Well Drilling and Development Well Placement." In Proceedings of the International Field Exploration and Development Conference 2018, 485–94. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-7127-1_44.

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Smith, J. W. "The Development of an Understanding of the Origins of the Sydney and Bowen Basin Gases." In Coalbed Methane: Scientific, Environmental and Economic Evaluation, 271–77. Dordrecht: Springer Netherlands, 1999. http://dx.doi.org/10.1007/978-94-017-1062-6_16.

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Abbot, John, and Jennifer Marohasy. "Forecasting Monthly Rainfall in the Bowen Basin of Queensland, Australia, Using Neural Networks with Niño Indices." In AI 2016: Advances in Artificial Intelligence, 88–100. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-50127-7_7.

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Falkner, A., and C. Fielding. "Quantitative Facies Analysis of Coal-Bearing Sequences in the Bowen Basin, Australia: Applications to Reservoir Description." In The Geological Modelling of Hydrocarbon Reservoirs and Outcrop Analogues, 81–97. Oxford, UK: Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444303957.ch4.

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Cobb, M., D. L. Lopez, M. Glikson, and S. D. Golding. "Simulating the Conductive and Hydrothermal Maturation of Coal and Coal Seam Gas in the Bowen Basin, Australia." In Coalbed Methane: Scientific, Environmental and Economic Evaluation, 435–48. Dordrecht: Springer Netherlands, 1999. http://dx.doi.org/10.1007/978-94-017-1062-6_26.

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Antes, Günther, and Franz Eggemann. "Basic Signs and Interpretation." In Small Bowel Radiology, 31–58. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-82473-9_4.

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Haddock, Graham. "E42 Inflammatory Bowel Disease." In Basic Techniques in Pediatric Surgery, 371–74. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-20641-2_113.

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Sinha, Anand, and Sandeep Agarwala. "E17 Small Bowel Atresia." In Basic Techniques in Pediatric Surgery, 290–92. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-20641-2_88.

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Conference papers on the topic "Bowen Basin"

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Withcombe, Josh, and Cam Runge. "2022 SAPPHIRE PILOT DRILLING PROGRAMME NORTH BOWEN BASIN." In PESA Symposium Qld 2022. PESA, 2022. http://dx.doi.org/10.36404/kaoe7233.

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Although being one of the longest producing CSG basins in Australia, there has been little recent appraisal work in the North Bowen Basin. The Northern Bowen has the largest uncontracted gas resource on the east coast of Australia and if developed, would provide sufficient volumes to meet not only domestic gas requirements but also potential back fill for existing LNG plants in to the future. Blue Energy will provide an overview of their ongoing Sapphire appraisal program near Moranbah and their view on the future of the basin.
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Morales, R. H., and S. C. Davidson. "Analysis of the Hydraulic Fracturing Behavior in the Bowen Basin." In Low Permeability Reservoirs Symposium. Society of Petroleum Engineers, 1993. http://dx.doi.org/10.2118/25862-ms.

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Gilbert, Tonna, Saikat Mazumder, and Ehtesham Ali. "Post-Shutdown Recovery Behavior of Horizontal Coalbed Methane Wells in the Bowen Basin." In SPE Unconventional Resources Conference and Exhibition-Asia Pacific. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/167023-ms.

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Belushko, Irina, Henricus Herwin, and Francois Gouth. "Dynamic Behavior of a Multi-Layered Coal Seams Gas Reservoir in the Bowen Basin." In SPE Asia Pacific Oil & Gas Conference and Exhibition. Society of Petroleum Engineers, 2014. http://dx.doi.org/10.2118/171538-ms.

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Spain, Alister, and Ian Hollingsworth. "Selected properties of the incipient soils developing on coal mining wastes, Bowen Basin, Australia." In Mine Closure 2016. Australian Centre for Geomechanics, Perth, 2016. http://dx.doi.org/10.36487/acg_rep/1608_11_spain.

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Scott, Michael Andrew, Saikat Mazumder, and Jessica Jiang. "Permeability increase in Bowen Basin coal as a result of Matrix Shrinkage during primary depletion." In SPE Asia Pacific Oil and Gas Conference and Exhibition. Society of Petroleum Engineers, 2012. http://dx.doi.org/10.2118/158152-ms.

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Nicholls, Peter, Rodney Bresnehan, Brad Hayes, Kathleen Dorey, and William McDougall. "Unconventional Resource Potential of the Taroom Trough in the Southern Surat-Bowen Basin, Queensland, Australia." In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2210830.

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Li, M. "Coalbed Mathane Enrichment Rule and Sweet Spot Optimization-Case Study From Australia North Bowen Basin." In 82nd EAGE Annual Conference & Exhibition. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202010336.

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Connell, Luke D., Saikat Mazumder, Stephen Marinello, Regina Sander, Michael Camilleri, Zhejun Pan, and Deasy Heryanto. "Characterisation of Bowen Basin Coal Shrinkage and Geomechanical Properties and Their Influence on Reservoir Permeability." In SPE Asia Pacific Oil and Gas Conference and Exhibition. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/165822-ms.

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Wold, M., S. C. Davidson, B. Wu, S. K. Choi, and R. A. Koenig. "Cavity Completion For Coalbed Methane Stimulation - An Integrated Investigation And Trial In The Bowen Basin, Queensland." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 1995. http://dx.doi.org/10.2118/30733-ms.

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Reports on the topic "Bowen Basin"

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Shpigel, Nahum, Raul Barletta, Ilan Rosenshine, and Marcelo Chaffer. Identification and characterization of Mycobacterium paratuberculosis virulence genes expressed in vivo by negative selection. United States Department of Agriculture, January 2004. http://dx.doi.org/10.32747/2004.7696510.bard.

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Mycobacterium avium subsp. paratuberculosis (MAP) is the etiological agent of a severe inflammatory bowel disease (IBD) in ruminants, known as Johne’s disease or paratuberculosis. Johne’s disease is considered to be one of the most serious diseases affecting dairy cattle both in Israel and worldwide. Heavy economic losses are incurred by dairy farmers due to the severe effect of subclinical infection on milk production, fertility, lower disease resistance and early culling. Its influence in the United States alone is staggering, causing an estimated loss of $1.5 billion to the agriculture industry every year. Isolation of MAP from intestinal tissue and blood of Crohn's patients has lead to concern that it plays a potential pathogenic role in promoting human IDB including Crohn’s disease. There is great concern following the identification of the organism in animal products and shedding of the organism to the environment by subclinically infected animals. Little is known about the molecular basis for MAP virulence. The goal of the original proposed research was to identify MAP genes that are required for the critical stage of initial infection and colonization of ruminants’ intestine by MAP. We proposed to develop and use signature tag mutagenesis (STM) screen to find MAP genes that are specifically required for survival in ruminants upon experimental infection. This research projected was approved as one-year feasibility study to prove the ability of the research team to establish the animal model for mutant screening and alternative in-vitro cell systems. In Israel, neonatal goat kids were repeatedly inoculated with either one of the following organisms; MAP K-10 strain and three transposon mutants of K-10 which were produced and screened by the US PI. Six months after the commencement of inoculation we have necropsied the goats and taken multiple tissue samples from the jejunum, ileum and mesenteric lymph nodes. Both PCR and histopathology analysis indicated on efficient MAP colonization of all the inoculated animals. We have established several systems in the Israeli PI’s laboratory; these include using IS900 PCR for the identification of MAP and using HSP65-based PCR for the differentiation between MAV and MAP. We used Southern blot analysis for the differentiation among transposon mutants of K-10. In addition the Israeli PI has set up a panel of in-vitro screening systems for MAP mutants. These include assays to test adhesion, phagocytosis and survival of MAP to/within macrophages, assays that determine the rate of MAPinduced apoptosis of macrophages and MAP-induced NO production by macrophages, and assays testing the interference with T cell ã Interferon production and T cell proliferation by MAP infected macrophages (macrophage studies were done in BoMac and RAW cell lines, mouse peritoneal macrophages and bovine peripheral blood monocytes derived macrophages, respectively). All partners involved in this project feel that we are currently on track with this novel, highly challenging and ambitious research project. We have managed to establish the above described research systems that will clearly enable us to achieve the original proposed scientific objectives. We have proven ourselves as excellent collaborative groups with very high levels of complementary expertise. The Israeli groups were very fortunate to work with the US group and in a very short time period to master numerous techniques in the field of Mycobacterium research. The Israeli group has proven its ability to run this complicated animal model. This research, if continued, may elucidate new and basic aspects related to the pathogenesis MAP. In addition the work may identify new targets for vaccine and drug development. Considering the possibility that MAP might be a cause of human Crohn’s disease, better understanding of virulence mechanisms of this organism might also be of public health interest as well.
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