Relevant bibliographies by topics / Geology Western Australia Carnarvon Basin

Academic literature on the topic 'Geology Western Australia Carnarvon Basin'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Contents

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Geology Western Australia Carnarvon Basin.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Geology Western Australia Carnarvon Basin"

1

Kear, B. P., J. A. Long, and J. E. Martin. "A review of Australian mosasaur occurrences." Netherlands Journal of Geosciences 84, no. 3 (September 2005): 307–13. http://dx.doi.org/10.1017/s0016774600021089.

Full text
Abstract:
AbstractMosasaurs are rare in Australia with fragmentary specimens known only from the Cenomanian-lower Turonian Molecap Greensand (Perth Basin), Campanian - lower Maastrichtian Korojon Calcarenite (Carnarvon Basin), and upper Maastrichtian Miria Formation (Carnarvon Basin), Western Australia. These units were laid down during a near-continuous marine inundation of the western margin of the Australian landmass (which followed separation from India in the Valanginian and genesis of the Indian Ocean) in the Early-Late Cretaceous. The Australian mosasaur record incorporates evidence of derived mosasaurids (mainly plioplatecarpines); however, as yet no specimen can be conclusively diagnosed to genus or species level. The fragmentary nature of the remains provides little basis for direct palaeobiogeographic comparisons. However, correlation with existing data on associated vertebrates, macroinvertebrates and microfossils suggests that the Western Australian mosasaur fauna might have been transitional in nature (particularly following palaeobiogeographic separation of the northern and southern Indian Oceans during the mid-Campanian), potentially sharing elements with both northern Tethyan and austral high-latitude regions.
APA, Harvard, Vancouver, ISO, and other styles
2

Beardsmore, Graeme. "High-resolution Heat-Flow Measurements in the Southern Carnarvon Basin, Western Australia." Exploration Geophysics 36, no. 2 (June 2005): 206–15. http://dx.doi.org/10.1071/eg05206.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Percival, I. G., and P. M. Cooney. "PETROLEUM GEOLOGY OF THE MERLINLEIGH SUB-BASIN, WESTERN AUSTRALIA." APPEA Journal 25, no. 1 (1985): 190. http://dx.doi.org/10.1071/aj84017.

Full text
Abstract:
Esso's recent drilling program in the Merlinleigh Sub-basin, onshore Carnarvon Basin, represents the culmination of the first phase of concerted exploration activity in the area since the WAPET era of the 1960s. The region is unusual among Australian petroleum provinces in having excellent exposures of reservoir, source and seal rocks of Palaeozoic age. While both Esso wells (Burna 1 and Gascoyne 1) failed to encounter hydrocarbons in the primary Wooramel Group play, encouraging potential still exists. The reservoir in the Wooramel Group play is the Early Permian Moogooloo Sandstone, a fluviodeltaic to nearshore sheet-sand facies with porosities to 23 per cent and permeabilities in excess of 100 millidarcys. Likely hydrocarbon sources are siltstones in the overlying Byro Group, with total organic carbon contents averaging 3 per cent, and calcilutites in the subjacent Callytharra Formation with similar organic content. Locally, the Jimba Jimba Calcarenite Member (Billidee Formation) and the Cordalia Sandstone also provide rich source units. The least certain aspects of the Early Permian play are fault and top seal, and reservoir quality at depth. Notwithstanding the relatively shallow depths to source strata in the area, vitrinite reflectance analyses from drill cores indicate that maturation is attained as shallow as 900 m on the folded and faulted western margin of the sub-basin, and at an approximate depth of 1200 m in the depocentre beneath the Kennedy Range. This can be related to high regional heat flow, and to erosion of some 1500-2000 m of sediments prior to the regional Early Cretaceous transgression.Older plays which have been identified in the area remain to be adequately evaluated. Potential reservoir sands are present in the Silurian Tumblagooda Sandstone, the Middle and Late Devonian Nannyarra and Munabia Sandstones, and the Early Carboniferous Williambury Formation. Possible source rocks include carbonates of Middle Devonian and Early Carboniferous age. One of the objects of current research has been to locate areas where seal, provided by the glacigene Lyons Formation of Late Carboniferous-Early Permian age, is sufficiently thin to permit economic drilling.
APA, Harvard, Vancouver, ISO, and other styles
4

Lever, Helen. "Cyclic sedimentation in the shallow marine Upper Permian Kennedy Group, Carnarvon Basin, Western Australia." Sedimentary Geology 172, no. 1-2 (November 2004): 187–209. http://dx.doi.org/10.1016/j.sedgeo.2004.08.004.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Wyrwoll, Karl-Heinz, Trevor Stoneman, Greg Elliott, and Peter Sandercock. "Geoecological setting of the Carnarvon Basin, Western Australia: geology, geomorphology and soils of selected sites." Records of the Western Australian Museum, Supplement 60, no. 1 (2000): 29. http://dx.doi.org/10.18195/issn.0313-122x.61.2000.029-075.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

McHarg, Sam, Chris Elders, and Jane Cunneen. "Origin of basin-scale syn-extensional synclines on the southern margin of the Northern Carnarvon Basin, Western Australia." Journal of the Geological Society 176, no. 1 (August 24, 2018): 115–28. http://dx.doi.org/10.1144/jgs2018-043.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Shragge, Jeffrey, David Lumley, Julien Bourget, Toby Potter, Taka Miyoshi, Ben Witten, Jeremie Giraud, et al. "The Western Australia Modeling project — Part 2: Seismic validation." Interpretation 7, no. 4 (November 1, 2019): T793—T807. http://dx.doi.org/10.1190/int-2018-0218.1.

Full text
Abstract:
Large-scale 3D modeling of realistic earth models is being increasingly undertaken in industry and academia. These models have proven useful for various activities such as geologic scenario testing through seismic finite-difference (FD) modeling, investigating new acquisition geometries, and validating novel seismic imaging, inversion, and interpretation methods. We have evaluated the results of the Western Australia (WA) Modeling (WAMo) project, involving the development of a large-scale 3D geomodel representative of geology of the Carnarvon Basin, located offshore of WA’s North West Shelf (NWS). Constrained by a variety of geologic, petrophysical, and field seismic data sets, the viscoelastic WAMo 3D geomodel was used in seismic FD modeling and imaging tests to “validate” model realizations. Calibrating the near-surface model proved to be challenging due to the limited amount of well data available for the top 500 m below the mudline. We addressed this issue by incorporating additional information (e.g., geotechnical data, analog studies) as well as by using soft constraints to match the overall character of nearby NWS seismic data with the modeled shot gathers. This process required undertaking several “linear” iterations to apply near-surface model conditioning, as well as “nonlinear” iterations to update the underlying petrophysical relationships. Overall, the resulting final WAMo 3D geomodel and accompanying modeled shot gathers and imaging results are able to reproduce the complex full-wavefield character of NWS marine seismic data. Thus, the WAMo model is well-calibrated for use in geologic and geophysical scenario testing to address common NWS seismic imaging, inversion, and interpretation challenges.
APA, Harvard, Vancouver, ISO, and other styles
8

Lever, Helen. "Climate Changes and Cyclic Sedimentation in the Mid-Late Permian: Kennedy Group, Carnarvon Basin, Western Australia." Gondwana Research 7, no. 1 (January 2004): 135–42. http://dx.doi.org/10.1016/s1342-937x(05)70312-9.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Thompson, Mark. "THE DEVELOPMENT GEOLOGY OF THE TUBRIDGI GAS FIELD." APPEA Journal 32, no. 1 (1992): 44. http://dx.doi.org/10.1071/aj91005.

Full text
Abstract:
The Tubridgi Gas Field is located in the south of the Barrow Sub-basin, onshore in the Carnarvon Basin, Western Australia. The accumulation was discovered by Pan Pacific Petroleum NL in June 1981 with the drilling of the Tubridgi-1 well. Subsequent to Tubridgi-1, eight appraisal wells have been drilled, six of which were successful. The latest wells, Tubridgi-7 and-8, drilled in September 1990 by current operator Doral Resources NL, have enabled geological and petrophysical models for the field to be refined. These models were utilised for reserve determinations which were used to negotiate gas supply contracts and secure project financing to ensure the fields successful commercial development. Tubridgi gas is trapped within a broad, low relief, northeast-trending anticlinal closure. Reservoirs for the accumulation are the Middle to Upper Triassic Mungaroo Formation, Upper Cretaceous Flacourt Formation of the Barrow Group and Birdrong Sandstone of the Cretaceous Winning Group. All three units exhibit porosities averaging 29-30 per cent, with permeabilities of 3-16 D in the Mungaroo and Flacourt Formations and 157 mD in the Birdrong Sandstone. Vertical seal for the accumulation is the Muderong Shale of the Winning Group.The Tubridgi Gas Field is the first onshore Carnarvon Basin hydrocarbon accumulation to be commercially developed. Gas production into the Dampier-to-Bunbury Natural Gas Pipeline commenced on 26 September 1991 and within one month had reached contract volumes averaging 22 MMCFD (623 000 m3/d). Field life is anticipated to be ten years.
APA, Harvard, Vancouver, ISO, and other styles
10

LINDSTRÖM, SOFIE. "Palynofloral patterns of terrestrial ecosystem change during the end-Triassic event – a review." Geological Magazine 153, no. 2 (September 1, 2015): 223–51. http://dx.doi.org/10.1017/s0016756815000552.

Full text
Abstract:
AbstractA review of the palynofloral succession at the well-documented Triassic–Jurassic boundary sites – Kuhjoch (Austria), St Audrie's Bay (UK), Stenlille (Denmark), Astartekløft (Greenland), Sverdrup Basin (Arctic Canada), Northern Carnarvon Basin (Western Australia), Southeast Queensland (eastern Australia) and New Zealand – show all sites experienced major to moderate re-organization of the terrestrial vegetation during the end-Triassic event. The changes led to subsequent taxonomic losses of between 17% and 73% of the Rhaetian pre-extinction palynoflora. The majority of the typical Rhaetian taxa that disappear are so far not known fromin situoccurrences in reproductive structures of macrofossil plant taxa. From an ecological perspective, the most dramatic changes occurred in the Sverdrup Basin, Stenlille, Kuhjoch and Carnarvon Basin, where the pre- and post-extinction palynofloras were fundamentally different in both composition and dominance. These changes correspond to ecological severity Category I of McGheeet al.(2004), while the remaining sites are placed in their Subcategory IIa because there the pre-extinction ecosystems are disrupted, but recover and are not replaced post-extinction. Increased total abundances of spores on both hemispheres during the extinction and recovery intervals may indicate that environmental and/or climatic conditions became less favourable for seed plants. Such conditions may include expected effects of volcanism in the Central Atlantic Magmatic Province, such as acid rain, terrestrial soil and freshwater acidification due to volcanic sulfur dioxide emissions, fluctuating ultraviolet flux due to ozone depletion caused by halogens and halocarbon compounds, and drastic changes in climatic conditions due to greenhouse gas emissions.
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Geology Western Australia Carnarvon Basin"

1

Van, Ruth Peter John. "Overpressure in the Cooper and Carnarvon Basins, Australia /." Title page, abstract and table of contents only, 2003. http://web4.library.adelaide.edu.au/theses/09PH/09phv275.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

McHarg, Sam. "Tectonostratigraphic evolution of the Dampier Sub-basin, Northern Carnarvon Basin, Western Australia." Thesis, Curtin University, 2018. http://hdl.handle.net/20.500.11937/70560.

Full text
Abstract:
The complex interaction of Mesozoic fault orientation and basin scale features of the segmented Lewis Trough and en echelon Rankin Fault Zone suggest oblique reactivation of Carboniferous and Permian aged faults, somewhat at odds with the general perception of NW oriented extension associated with separation of Argoland from the NW shelf at this time. Mesozoic fault patterns observed suggest prolonged extension initiating in the Rhaetian, under an E-W oriented extensional regime.
APA, Harvard, Vancouver, ISO, and other styles
3

Couzens, Mark Anthony. "Early cretaceous sequence stratigraphic architecture, Enderby Terrace, Carnarvon Basin, Western Australia /." Title page, abstract and contents only, 2003. http://web4.library.adelaide.edu.au/theses/09SB/09sbc872.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Marlow, Alison. "Facies distribution within the M. australis section on the Enderby Terrace, Carnarvon Basin, Western Australia." Adelaide : [s.n.], 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbm347.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Mack, Daniel Aaron. "Seismic and stratigraphic interpretation of the Candace Terrace and Preston Shelf, Northern Carnarvon Basin, Western Australia /." Title page, contents and abstract only, 1993. http://web4.library.adelaide.edu.au/theses/09SM/09smm153.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Draper, Paul Christopher. "Secondary migration fairways and hydrocarbon potential of the Southern Enderby Terrace, Northern Carnarvon Basin, Western Australia /." Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbd766.pdf.

Full text
Abstract:
Thesis (B. Sc.(Hons.))--University of Adelaide, National Centre for Petroleum Geology and Geophysics, 1995.
Two folded maps in pocket inside back cover. Includes bibliographical references (leaves 130-135).
APA, Harvard, Vancouver, ISO, and other styles
7

Quinn, Matthew J. "Glaucony as an environmental indicator, with examples from the Cretaceous of the Northern Carnarvon Basin, Western Australia /." Title page, contents and abstract only, 1997. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bq72.pdf.

Full text
Abstract:
Thesis (B. Sc.(Hons.))--University of Adelaide, National Centre for Petroleum Geology and Geophysics, 1998?
Eleven enclosures in six pockets inserted through text. Includes bibliographical references (leaves 52-54).
APA, Harvard, Vancouver, ISO, and other styles
8

Quintavalle, Marco. "Lower to Middle Ordovician palynomorphs of the Canning Basin, Western Australia /." [St. Lucia, Qld.], 2004. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe18370.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Suwarna, Nana. "Petrology of Jurassic coal, Hill River area, Perth Basin, Western Australia." Thesis, Curtin University, 1993. http://hdl.handle.net/20.500.11937/675.

Full text
Abstract:
The Early Jurassic coal samples for the study were obtained from CRA Exploration Pty Ltd. (CRAE), drilled in the Gairdner and Mintaja Blocks, Gairdner Range of the Hill River Area, northern Perth Basin, Western Australia. The area is located approximately 280 km north of Perth. The coal measures subcrop in a half- graben bounded by the Lesueur-Peron Fault in the west, and the Warradarge Fault in the east. The coal occurs within the shallow sequence of the Cattamarra Member which is also described as the Cattamarra Coal Measures of the Cockleshell Gully Formation. Six sub-seams of seam G, namely G1 to G6, from the six drill cores, were examined for petrological and geochemical investigation. The coal predominantly comprises of banded, dull banded, and dull lithotypes, with minor bright banded, bright and fusainous types. Based on maceral analyses, the dominant maceral groups are vitrinite and inertinite, whilst the exinite and mineral matter are in minor contents. The vitrinite content has a range between 47.2% to 73.0%, and it is composed mainly of telocollinite and desmocollinite. The inertinite is dominated by semifusinite, fusinite, and inertodetrinite, and it has a range from 10.4% to 24.8%. The exinite group varies between 7.2% to 20.8% in content, and it is represented by sporinite, cutinite, alginite and resinite.The mineral matter dominated by clays and pyrite, ranges between 4.5% to 20.6%. The microlithotype analyses shows that the vitrite plus clarite content varies from 47.0% to 70.0%, intermediates between 8.0% to 26.0%, whilst inertite plus durite content is relatively low, varying from 6.55% to 14.0%. The maximum reflectance of vitrinite has a value between 0.47% and 0.53%, which represents rank at sub-bituminous level based on the Australian rank values and corresponding to the sub-bituminous A and B rank of the ASTM classification and to the metalignitous type of the Pareek classification. On the basis of carbon and hydrogen content, the coal is categorised as per-hydrous meta- to ortho-lignitous type. The trace elements As, B, Be, Cd, Co, Cr, Cu, Ga, Mn, Mo, Ni, Pb, Sr, Th, U, V, Y, Zn, and Zr, are spectrographically analysed in the coal ash. The B content in the coal supports the presence of marine influence during peat deposition in the basin. On the basis of lithotype, maceral, microlithotype, trace element distribution, pyrite and total sulphur in the coal, the depositional environment for coal and the coal measures, is interpreted as an upper to lower delta type within a regressive phase of marine transgression.
APA, Harvard, Vancouver, ISO, and other styles
10

Iasky, Vickie Clare. "Seismic sequence stratigraphy and facies characterisation of the G and H units within the Goodwyn Field Northern Carnarvon Basin Western Australia /." Title page, abstract and table of contents only, 2004. http://web4.library.adelaide.edu.au/theses/09SB/09sbi118.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Books on the topic "Geology Western Australia Carnarvon Basin"

1

Hocking, R. M. Geology of the Carnarvon Basin, Western Australia. Perth: State Print. Division, 1987.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
2

Hocking, R. M. Geology of the Carnarvon Basin, Western Australia. Perth: Western Australia Geological Survey, 1987.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
3

Lockwood, A. M. Geophysical investigation of the Bernier Ridge and surrounding area, Southern Carnarvon Basin, Western Australia. East Perth, W.A: Dept. of Industry and Resources, 2003.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
4

Mory, A. J. A summary of the geological evolution and petroleum potential of the Southern Carnarvon Basin Western Australia. Perth: Western Australia Geological Survey, 2003.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
5

Driscoll, Neal. Tectonic and stratigraphic evolution of the Carnarvon Basin, Northwest Australia. East Perth, WA: Minerals and Energy Research Institute of Western Australia, 1996.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
6

Thorne, A. M. Geology of the Ashburton Basin, Western Australia. Perth: Geology Survey of Western Australia, 1991.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
7

Geology of the Jillawarra area, Bangemall Basin, Western Australia. Perth: Geological Survey of Western Australia, 1995.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
8

1953-, Mory A. J., Blundell K. A. 1966-, and Geological Survey of Western Australia., eds. The geophysical interpretation of the Woodleigh impact structure, Southern Carnarvon Basin, Western Australia. Perth, W.A: Geological Survey of Western Australia, 2001.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
9

Darragh, Thomas A. Maastrichtian Bivalvia (excluding Inoceramidae) from the Miria Formation, Carnarvon Basin, north western Australia. Perth, W.A: Western Australian Museum, 1991.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
10

Payne, A. L. An inventory and condition survey of rangelands in the Carnarvon Basin, Western Australia. Perth: Department of Agriculture, 1987.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Book chapters on the topic "Geology Western Australia Carnarvon Basin"

1

Eriksson, Kenneth A., William S. F. Kidd, and Bryan Krapez. "Basin Analysis in Regionally Metamorphosed and Deformed Early Archean Terrains: Examples from Southern Africa and Western Australia." In Frontiers in Sedimentary Geology, 371–404. New York, NY: Springer New York, 1988. http://dx.doi.org/10.1007/978-1-4612-3788-4_19.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Neubauer, M., R. Hillis, R. King, and S. Reynolds. "The contemporary stress field of the offshore Carnarvon Basin, North West Shelf, Western Australia." In Rock Mechanics: Meeting Society's Challenges and Demands, 705–11. Taylor & Francis, 2007. http://dx.doi.org/10.1201/noe0415444019-c87.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

"Geology of the Admiral Bay Carbonate-Hosted Zinc-Lead Deposit, Canning Basin, Western Australia." In Carbonate-Hosted Lead-Zinc Deposits, 330–49. Society of Economic Geologists, 1996. http://dx.doi.org/10.5382/sp.04.24.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Semeniuk, Vic, and Margaret Brocx. "The Onshore Southern Carnarvon Basin in Coastal Western Australia during the Quaternary: Tectonic Setting and Facies-Complicated Heterogeneous Stratigraphic Patterns." In Geochemistry [Working Title]. IntechOpen, 2020. http://dx.doi.org/10.5772/intechopen.92866.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Geology Western Australia Carnarvon Basin"

1

Zhang, Yujin, Henry A. Salisch, Hla Shwe, and Christoph Arm. "Permeability evaluation in a glauconite‐rich formation in the Carnarvon Basin, Western Australia." In SEG Technical Program Expanded Abstracts 1997. Society of Exploration Geophysicists, 1997. http://dx.doi.org/10.1190/1.1886147.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Gibson, Helen, Ray Seikel, Desmond FitzGerald, Mike Middleton, and Ameed Ghori. "3D geology, temperature, heat flow and thermal gradient modeling of the north Perth Basin, Western Australia." In SEG Technical Program Expanded Abstracts 2011. Society of Exploration Geophysicists, 2011. http://dx.doi.org/10.1190/1.3627424.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Yao, Jianfeng, Xiang Li, Kai Zhao, and Hui Zhang. "Full-Waveform Inversion and Least-Squares Migration to Improve Images in Northern Carnarvon Basin." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21292-ms.

Full text
Abstract:
Abstract Northern Carnarvon Basin is located in North West Shelf of Western Australia. The basin has over 10km sediments and owns both oil-prone and gas-prone sediments and is the current largest oil and gas producing basin in Australia. A geological section through this basin is shown in Figure 1, the complex geological settings from shallow to deep leads to significant processing challenges. In the vintage processing, the seismic image at reservoir level is deteriorated due to the presence of following geological complexities: 1) rugose water bottom, 2) shallow frequent canyons or channel systems, 3) shallow spatial-variant Tertiary carbonates, and 4) shallow gas chimneys and other geo-bodies. These complex overburdens plus limited small-angle coverage of primary reflections from narrow azimuth (NAZ) streamer surveys make it very difficult for ray-based reflection tomography to resolve the shallow velocity. As a result, the target image suffers from large well mis-ties, low signal-to-noise ratio (S/N) and severe event undulations. In addition, shallow fast-velocity layers cause severe illumination issues for deep targets which are compounded by limited offsets of NAZ surveys. Furthermore, localised absorption effects from gas pockets lead to dimming amplitudes for events beneath them. To deal with these issues, we propose to use time-lag full wave-form inversion (TLFWI) to resolve the velocity of complex overburdens and least-squares Q prestack depth migration (LS Q-PSDM) to compensate for illumination issues and absorption effects for the latest reprocessing. In the following sections, application procedure and results of these two technologies will be discussed. Seismic inversion was also conducted to assist the processing and analysis of the final result.
APA, Harvard, Vancouver, ISO, and other styles

Reports on the topic "Geology Western Australia Carnarvon Basin"

1

Picard, Kim, Scott L. Nichol, Riko Hashimoto, Andrew Carroll, George Bernadel, Leonie Jones, Justy Siwabessy, et al. Seabed environments and shallow geology of the Leveque Shelf, Browse Basin, Western Australia. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.010.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Nicholas, W. A., A. G. Carroll, L. Radke, M. Tran, F. J. F. Howard, R. Przeslawski, J. Chen, P. J. W. Siwabessy,, and S. L. Nichol. Seabed Environments and Shallow Geology of the Leveque Shelf, Browse Basin, Western Australia: GA0340 - Interpretative report. Geoscience Australia, 2016. http://dx.doi.org/10.11636/record.2016.018.

Full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Geology Western Australia Carnarvon Basin' for particular source types:
Journal articles Dissertations / Theses Books
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography