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Добірка наукової літератури з теми "Fitzroy Trough"

Автор: Grafiati
Опубліковано: 10 грудня 2022
Оновлено: 28 січня 2023

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Статті в журналах з теми "Fitzroy Trough"

1

Begg, John. "STRUCTURING AND CONTROLS ON DEVONIAN REEF DEVELOPMENT ON THE NORTH-WEST BARBWIRE AND ADJACENT TERRACES, CANNING BASIN." APPEA Journal 27, no. 1 (1987): 137. http://dx.doi.org/10.1071/aj86013.

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The major terraces flanking the southern margin of the Fitzroy Trough have had a complex history of development involving at least four major episodes of structuring with varying degrees of intensity from the Mid-Late Ordovician Rodingan Movement through to the Latest Triassic-Early Jurassic Fitzroy Movement. Extensive salt tectonism associated with the massive evaporite deposits of the Silurian Carribuddy Formation has also had a profound effect on structuring in these areas.Despite sparse well control, seismic recognition of the resultant structural styles has provided the basis for more comprehensive modelling of the main controls on sedimentation than has previously been possible.In particular, a complex sub-surface distribution of stacked Devonian carbonate platform and reef complexes can now be recognised, having similar morphologies to the spectacular outcrop on the northern side of the Fitzroy Trough. In addition to broad platform areas, individual peninsula developments, isolated atolls and extensive inter-reef seaways were present at both Pillara and Nullara cycle levels, largely controlled by faulting initiated in the Mid-Devonian and influenced in some cases by salt diapirism.Identification of the carbonate and associated palaeogeographic trends will provide direction for future exploration efforts in this wildcat area.
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2

Gaede, Oliver, Moritz Ziegler, and Oliver Heidbach. "Building a 3D Geomechanical Model for the Fitzroy Trough." ASEG Extended Abstracts 2019, no. 1 (November 11, 2019): 1–4. http://dx.doi.org/10.1080/22020586.2019.12073133.

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3

Strand, Julian, Antoine Vaslin, and Laurent Langhi. "Fault-seal potential of the Palaeozoic in the northwest Canning Basin." APPEA Journal 52, no. 1 (2012): 427. http://dx.doi.org/10.1071/aj11034.

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As part of a Geological Survey of Western Australia organised review of the Canning Basin involving UWA and CSIRO, the fault-seal potential for the northwest Canning Basin has been analysed. This study has two foci: firstly identifying potential for fault-bound hydrocarbon reservoirs in the Early Permian (Poole Sandstone and Upper Grant Group). Secondly, James Price Point, 55 km north of Broome, is the chosen location for an LNG facility to service the northern North West Shelf gas fields. As such, the study aims to highlight potential CO2 sequestration reservoir sequences occurring inside 200 km of James Price Point, the economically feasible distance for CO2 delivery to an injection site. Historically, hydrocarbon exploration drilling in the Fitzroy Trough targeted anticlinal structures, which proved unsuccessful due to localised, but significant, erosion of the Permian sequence including the Noonkanbah Formation top-seal on anticlinal crests. Given there is potential for untested, fault-bound traps to exist, which might provide an alternative to the anticlinal traps, it will be useful to identify the distribution of shale-rich, top-seal and fault-seal prone sequences, and where these occur at suitable reservoir depths. The study shows the Early Permian sequences on the flanking terraces of the Fitzroy Trough commonly have suitable top-seal and fault-seal prone sediments. In wells analysed in the Fitzroy Trough itself, the Early Permian sequence is poorly represented, but Permo-Carboniferous sediments observed indicate some sealing potential might exist there. Moving south onto the Broome Platform and into the Wiluna Sub-basin, the Early Permian sequences still display some sealing potential, but Ordovician units might provide more suitable targets for sequestration in these areas.
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4

Harrison, Paul, Chris Swarbrick, Jim Winterhalder, and Mark Ballesteros. "The petroleum prospectivity of the Oobagooma Sub-basin and adjacent Leveque Platform, North West Shelf, Australia." APPEA Journal 56, no. 2 (2016): 563. http://dx.doi.org/10.1071/aj15069.

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The Oobagooma Sub-basin of the Roebuck Basin includes the offshore extension of the onshore Fitzroy Trough of the Canning Basin. Together with the Leveque Platform, it covers an area of approximately 50,000 km2, yet only 14 exploration wells have been drilled in the area to date, five of which were drilled in the past 30 years. The sub-basin contains sediments ranging in age from Ordovician to Recent. This study examines the petroleum prospectivity of a region that is one of the least explored on Australia’s North West Shelf. Recent exploration drilling has revived interest in the area, with the 2014 Phoenix South–1 oil discovery in the offshore Bedout Sub-basin and the 2015 Ungani Far West–1 oil discovery in the onshore Fitzroy Trough. The two most significant source rock sequences relevant to the Oobagooma Sub-basin are the Carboniferous Laurel Formation and the Jurassic section. The former interval is part of a proven petroleum system onshore and is the source of the gas discovered at Yulleroo and oil at Ungani and Ungani Far West. A thick Jurassic trough to the north of the Oobagooma Sub-basin is believed to be the source of the oil and gas in Arquebus–1A and gas in Psepotus–1. Hydrocarbon charge modelling indicates significant expulsion occurred during both the Cretaceous and Tertiary from both source intervals. Trap timing is generally favourable given that inversion structures formed in several episodes during the Late Jurassic to Late Tertiary. The Early Triassic, now proven to be oil prone in the Phoenix South area (Molyneux et al, 2015), provides an additional (albeit less likely) source for the Oobagooma Sub-basin. These rocks are thin to absent within the Oobagooma Sub-basin, so long-distance migration would be required from deep troughs to the west.
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5

Drummond, B. J., M. A. Etheridge, P. J. Davies, and M. F. Middleton. "HALF-GRABEN MODEL FOR THE STRUCTURAL EVOLUTION OF THE FITZROY TROUGH, CANNING BASIN, AND IMPLICATIONS FOR RESOURCE EXPLORATION." APPEA Journal 28, no. 1 (1988): 76. http://dx.doi.org/10.1071/aj87008.

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The Fitzroy Trough is a north-west/south-east trending rift along the north-east margin of the Canning Basin. The major crustal extension in the trough occurred in the Middle Devonian to Early Carboniferous. Most idealised cross-sections show down-to-trough normal faults bounding both sides of the trough. In contrast, we show the trough to have a half- graben style, with one side a hinge zone or flexure, and the other side bounded by normal faults. Thus, the basin has marked structural asymmetry. The sense of asymmetry switches several times along strike with the hinged margin on the north-eastern margin in some places and the south-west margin in others. The switching in asymmetry occurs at transfer faults. This structural style is expected in extensional tectonic models where the extension occurs on a detachment surface and is typical of many continental and passive margin rifts. The asymmetry of the Palaeozoic structure has implications for resource exploration because of its influence on facies development in and subsequent structural evolution of the trough. Quite different syn-rift clastic and carbonate facies are expected on faulted and hinged margins of a half-graben. Post-rift subsidence will also be somewhat asymmetric, influencing the carbonate reef geometry in particular. Mesozoic deformation in the basin reactivated many of the Palaeozoic normal and transfer faults, and induced reverse slip up basement surfaces on the hinged margin segments.
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6

O'Brien, P. E., J. F. Lindsay, K. Knauer, and M. J. Sexton. "Sequence stratigraphy of a sandstone‐rich Permian glacial succession, Fitzroy Trough, Canning Basin, Western Australia." Australian Journal of Earth Sciences 45, no. 4 (August 1998): 533–45. http://dx.doi.org/10.1080/08120099808728410.

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7

Drummond, B. J., M. J. Sexton, T. J. Barton, and R. D. Shaw. "The Nature of Faulting Along the Margins of the Fitzroy Trough, Canning Basin, and Implications for the Tectonic Development of the Trough." Exploration Geophysics 22, no. 1 (March 1991): 111–15. http://dx.doi.org/10.1071/eg991111.

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8

Shelokov, Valeri, Robert Hull, Tony Rudge, and Perry Richmond. "Petrophysical analysis of the unconventional reservoirs of the Lennard Shelf and Fitzroy Trough in Canning Basin, Australia." APPEA Journal 61, no. 2 (2021): 714. http://dx.doi.org/10.1071/aj20087.

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A US operator with a commitment to future drilling, stimulation and testing of unconventional wells has initiated a new evaluation to better define and understand the hydrocarbon plays along the northern margin of the Canning Basin’s Lennard Shelf and Fitzroy Trough. The goal of the evaluation is to determine the commercial viability of the region. In this paper, an integrated petrophysical hybrid model that has been calibrated to core data is highlighted. From this model, multiple play types were identified, including an unconventional siltstone-shale play, a conventional basin-centred tight gas play and a fractured tight gas play with potential analogs to North American unconventional plays. Six primary lithofacies were identified through the integration of thin section analyses, core descriptions, logs and petrophysical models. The results were calibrated to high-resolution formation image data to better understand the thin-bedded nature of these plays. The lithofacies were also utilised for defining core poro/perm transforms. Furthermore, an integrated descriptive mud log algorithm was utilised to define the types of hydrocarbons, including wetness, balance and ratios as the hydrocarbons’ fingerprints. Significant gas influxes were noted at the intervals with highly permeable beds, at swarms of fractures and faults, as well as within the organic rich layers. In this study, a pressure top seal for the Laurel Formation was defined as well as the highlights of one well, which includes 11 zones and over 389m of net pay behind pipe. The significance of this work is that it highlights a path forward for unconventional development that, if economically viable, would provide increased energy independence for Australia.
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9

Wyrwoll, Karl-Heinz, Jennifer Hopwood, and N. L. McKenzie. "The Holocene paleohydrology and climatic history of the Northern Great Sandy Desert - Fitzroy trough: With special reference to the northwest Australian monsoon." Climatic Change 33, no. 1 (May 1996): 135–38. http://dx.doi.org/10.1007/bf00140518.

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10

Al-Hinaai, Jalal, and Jonathan Redfern. "Tectonic and climatic controls on the deposition of the Permo-Carboniferous Grant Group and Reeves Formation in the Fitzroy Trough, Canning Basin, Western Australia." Marine and Petroleum Geology 59 (January 2015): 217–31. http://dx.doi.org/10.1016/j.marpetgeo.2014.08.016.

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Дисертації з теми "Fitzroy Trough"

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Thomas, M. C. "Erskine Sandstone Formation: a provenance and geochronological study within the Fitzroy Trough, Western Australia." Thesis, 2012. http://hdl.handle.net/2440/95492.

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This item is only available electronically.
The Erskine Sandstone Formation is located in the Fitzroy Trough, within the northern Canning Basin, Western Australia. The provenance evolution of the onshore Triassic sandstone of the Erskine Sandstone Formation has not previously been researched. Field work was conducted predominantly at two areas, the Erskine Range, the type section of the Sandstone, and the May River outcrops which include the Pinnacle Rock outcrop. Field work in the area showed a transitional boundary between the underlying Blina Shale and the Erskine Sandstone Formation making identification of the boundary zones difficult. Through the use of U-Pb zircon analysis on samples taken from the Erskine Range and the May River, this study suggests the two outcrops have differing sources. Samples taken from the Erskine Range contain Permian aged sediments which are not present in the May River samples. The significant presence of Mesoproterozoic sediments in the May River samples which are not reflected in the Erskine Range samples further suggests different sources. The large presence of Palaeoproterozoic sediments in both the Erskine Range and the May River outcrops suggests the uranium rich King Leopold Ranges is a possible source. These sediments, combined with the presence of reductants in the Erskine Sandstone Formation suggest the possibility of sandstone-hosted uranium mineralisation within the Fitzroy Trough. Other possible sediment sources include the Musgrave Block and Arunta Inlier, located to the south, and suggest a complex detrital history of the Fitzroy Trough.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2012
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Книги з теми "Fitzroy Trough"

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Rasmussen, Birger. Assessment of base-metal prospectivity in sedimentary basins based on the association between hydrocarbon and metalliferous brine migration: A feasibility study based on the Fitzroy Trough/Lennard Shelf, Western Australia. East Perth, WA: Minerals and Energy Research Institute of Western Australia, 1997.

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Частини книг з теми "Fitzroy Trough"

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Braun, Jean, and Russell Shaw. "Extension in the Fitzroy Trough, western Australia: An example of reactivation tectonics." In Structure and Evolution of the Australian Continent, 157–74. Washington, D. C.: American Geophysical Union, 1998. http://dx.doi.org/10.1029/gd026p0157.

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Тези доповідей конференцій з теми "Fitzroy Trough"

1

Feijth, Jurriaan, Carlos Cevallos, Tony Rudge, and Peter Edwards. "Basin Architecture From Gravity Gradiometer and Seismic Data, South-Western Margin of the Fitzroy Trough and Gregory Sub-Basin, Canning Basin, Western 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/ice2015-2210815.

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