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Academic literature on the topic 'Wyandra'

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Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Wyandra"

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Lonergan, T. P., P. G. Ryles, S. T. McClure, and D. W. McMillan. "THE TARBAT-IPUNDU OIL FIELD, A CASE STUDY IN IDENTIFYING BYPASSED OIL." APPEA Journal 38, no. 1 (1998): 36. http://dx.doi.org/10.1071/aj97002.

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Since 1995 the Tarbat-Ipundu Field has developed from a marginal 200 BOPD (31.8 kL/d) field with perceived limited growth potential to a developing resource with production up to 3,000 BOPD (476.9 kL/d). This increase was achieved through the efforts of a dedicated multidisciplinary team and an aggressive 'fit for purpose' drilling and evaluation program.The Tarbat-Ipundu Field is located in PL 52 of ATP 299P in southwestern Queensland, approximately 115 km to the northeast of the Jackson Oil Field. The field was discovered by Hartogen Energy Ltd in 1986 with the drilling of Ipundu 1 which came on-line at 100 BOPD (15.9 kL/d) from the Wyandra Sandstone and the Murta Member. The discovery well was followed by the drilling of Tarbat-1 in 1988 on a subculmination to the north. Tarbat-1 encountered oil in the Wyandra Sandstone but watered out after producing 17 KSTB (2,702 kL) of oil. During 1991 a further four wells were drilled in the Ipundu Field by the then operator, Ampolex Pty Ltd. Two of these wells were plugged and abandoned. In January 1994 the field was producing at 220 BOPD (34.9 kL/d) after a total production of 350 KSTB.The Santos Group acquired a majority interest and Operatorship of the Tarbat-Ipundu Field in 1994. An integrated geological and engineering evaluation of Tarbat-1, incorporating experience gained in other parts of the Eromanga Basin, indicated the potential for bypassed oil in the Hutton Sandstone. Similarly, additional potential was recognised in the Wyandra Sandstone and Murta Member in the Tarbat-Ipundu wells. To evaluate this potential Tarbat-2 was drilled in August 1995 at a location 315 m to the northwest of Tarbat-1. Drill stem tests in Tarbat-2 resulted in flows of 2,037 BOPD (323.8 kL/d) from a 26 m gross hydrocarbon column in the Hutton Sandstone and 770 BOPD (122.4 kL/d) from a 14 m gross hydrocarbon column in the Wyandra Sandstone.An aggressive appraisal and development program followed the drilling of Tarbat-2 which has resulted in the drilling of an additional 25 wells. Proved and Probable Oil in Place estimates have increased from 5.2 MMSTB (0.826 ML) in 1994 to 44.2 MMSTB (7.02 ML) in 1997. As at June 1997 the field produces oil from the WyandraSandstone, Murta Member and Hutton Sandstone of the Eromanga Basin. A combined oil offtake of up to 3,000 BOPD (476.9 kL/d) has been achieved from the field. Continued field development is planned for 1998.The successful 're-discovery' of the Tarbat-Ipundu Field illustrates the potential benefit of a systematic review and integration of all existing data via a multidisciplinary team. The increasing cost of new data acquisition makes it imperative that the existing data is thoroughly evaluated prior to the investment of further exploration capital. The Tarbat-Ipundu Field demonstrates the potential to add significant new reserves from focussed targeting and evaluation of potential bypassed hydrocarbon accumulations.
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Newton, C. B. "THE TINTABURRA OILFIELD." APPEA Journal 26, no. 1 (1986): 334. http://dx.doi.org/10.1071/aj85029.

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The Tintaburra oilfield, discovered in December 1983 with the drilling of Tintaburra 1, is situated within Petroleum Lease 29 (previously within Authority to Prospect 299P Part 2) on the southeast margin of the Eromanga Basin, Queensland.Tintaburra 1 recorded the first flow of oil from the Cretaceous Wyandra Sandstone Member of the Cadnaowie Formation in the Eromanga Basin and established the presence of oil columns in the Murta Member and Hutton Sandstone. The Hutton Sandstone produced 1750 barrels of 44° API gravity oil per day on drill stem test.The results of six successful appraisal wells show the field to be a simple structural accumulation at the top Hutton level. The top Hutton accumulation is believed to be full to fault-independent closure. The hydrocarbons are trapped on the western upthrown side of the Tertiary reverse faulted Tintaburra Anticline. Approximately 80 per cent of reserves are reservoired in the top Hutton.The discovery extended the productive limits of the Eromanga Basin 100 km to the north and east from theJackson oilfield, and highlighted the potential of Tertiary structures, previously thought by many to be non-prospective.Channelling at the 'C' horizon (base Wallumbilla Formation) extends across the southern part of the field, complicating depth mapping by virtue of the large velocity contrasts between channel and host sediments. Velocity and raypath distortion below the channel are major geophysical complexities that have been successfully overcome, allowing more accurate location of appraisal wells.Appraisal drilling, combined with high quality seismic data, has identified the nature of the Early Cretaceous submarine channelling, and has identified new channel-related plays. 'C' horizon channelling imparts a strong stratigraphic component to the Murta and Wyandra accumulations. Integrated core and log studies indicate that every reservoir within fault-independent closure, and overlain by a laterally continuous effective seal, contains oil. Facies variations within the top Hutton/base Birkhead interval have important implications for trap integrity and are generally not resolvable seismically.The high API gravity, low pour point Wyandra and Murta crudes are distinct from the waxy, paraffinic Hutton crudes, and geochemical analysis of the oils and source rocks indicates a probable Eromanga-sequence origin for all the crudes.
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Torkington, J., and M. I. Micenko. "A STRATIGRAPHIC ANALYSIS OF THE TALGEBERRY OILFIELD." APPEA Journal 28, no. 1 (1988): 113. http://dx.doi.org/10.1071/aj87011.

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ATP 299P(2) is located in the south-west Queensland portion of the Jurassic Cretaceous Eromanga Basin. Exploration drilling within the permit has resulted in the discovery of several oil pools which are stratigraphically controlled. Appraisal drilling at the Talgeberry Oilfield demonstrated this point when Talgeberry-2, drilled at a structurally higher location, failed to encounter either of the producing sands in Talgeberry-1. Oil is currently being produced from the Wyandra Sandstone and Birkhead Formation in Talgeberry-1 and from the Murta Member in Talgeberry-2.Depositional models are presented for each of the producing reservoirs at the Talgeberry Field, based upon dipmeter interpretation. An integrated seismic stratigraphic study was also undertaken on the Birkhead Formation reservoir.Oil production at Talgeberry is currently confined to distributary channel sands or near-shore distributary mouth bar sands. Distal facies of the distributary mouth bar have been intersected and, while containing oil, have been found to be generally tight.Dipmeter interpretation has proven valuable in determining depositional environment but is limited in defining the a real extent of the reservoir. Seismic-stratigraphic studies are able to define the reservoir geometry better and lead to a more comprehensive understanding of the depositonal environment.
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Healy, Donald T. "Wyandot of Kansas." Raven: A Journal of Vexillology 3 (1996): 230. http://dx.doi.org/10.5840/raven1996/19973/4136.

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St-Onge, N., and K. M. Labelle. "Wyandot Nation of Kansas." Journal of American History 98, no. 4 (February 19, 2012): 1230–31. http://dx.doi.org/10.1093/jahist/jar646.

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Steckley, John. "En Ascensione Domini: Jesus triomphant le jour de son ascension comparé a un capitaine victorieux (à patre pierson) [On Ascension Day: Jesus triumphant the day of his ascension compared to a victorious captain]." Ethnohistory 69, no. 2 (April 1, 2022): 223–32. http://dx.doi.org/10.1215/00141801-9522207.

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Context This text was written in Wendat by Belgian Jesuit Father Philippe Pierson (1642–1688), who came to North America in 1666. From 1673 to 1683, he lived and worked with the Wyandot community in what is now the city of St. Ignace near the tip of the Upper Peninsula, Michigan, on the shores of Lake Huron. It is the first part (Potier 1920:539) of a four-page text incorporated into the voluminous collection of copying, editing, and writing of another Belgian Jesuit, Father Pierre Potier (1708–1781), who worked with the Wyandot in the Detroit area from 1744 until his death in 1781. His collection was eventually published as an Ontario Archive Report, which represents the culmination of the Jesuits more than century and a half work with the Wendat/Wyandot people and their language. Although Pierson lived with the Wyandot, he had been trained in the Wendat dialect among those people in their community Wendake, then referred to as Lorette, a little outside of what is now the city of Quebec. The Wyandot are a closely related people, whose communities at the time of first contact with the French were west of the territory of the Wendat, and close to the southern shores of Georgian Bay, Lake Huron. The French labelled them Petun because of their involvement in the tobacco trade. The Wendat called them Etionnontateronnon ‘people where there is a mountain or hill,’ owing to their proximity to Blue Mountain and other hills of the Niagara Escarpment. Both peoples were driven out of their homeland mid-17th century through European-allied struggles with the English-connected Haudenosaunee ‘they extend a house,’ known to English and French then as the Iroquois. The translation into English and linguistic analysis are my own, based on what I have learned about the language for over 45 years of work. The inspiration to dedicate my research to the study of an Indigenous language came from Fred Wheatley, an Anishinaabe elder. He ‘lost his tongue’ through his experience in residential schools but regained it from his grandmother. He then dedicated his life to passing on that teaching to others, including me. When I learned that the Wendat people had ‘lost their tongue,’ but that the language was well-recorded and analysed in Jesuit writing, I knew what my life’s work would be.
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Kelly, Mckelvey. "Forty Narratives in the Wyandot Language." Ethnohistory 69, no. 1 (January 1, 2022): 123–24. http://dx.doi.org/10.1215/00141801-9404283.

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Garrad, Charles. "The Route and Purpose of Champlain’s Journey to the Petun in 1616." Ontario History 107, no. 2 (July 24, 2018): 159–78. http://dx.doi.org/10.7202/1050633ar.

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The route taken by Samuel de Champlain and party in 1616, during which he encountered Cheveux-relevés-Odawa and Petun-Wyandot peoples, and also some visiting Neutrals, is again considered. Previous conclusions are confirmed. That Champlain’s purpose was to proceed to the Neutrals, and possibly further to China, and his reasons for not doing so, are suggested.
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Kenneth C. Carstens. "The Eighteenth-Century Wyandot: A Clan-Based Study." Michigan Historical Review 40, no. 2 (2014): 133–34. http://dx.doi.org/10.1353/mhr.2014.0042.

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Walsh, Martin W. "The "Heathen Party": Methodist Observation of the Ohio Wyandot." American Indian Quarterly 16, no. 2 (1992): 189. http://dx.doi.org/10.2307/1185429.

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Dissertations / Theses on the topic "Wyandra"

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Root, Robert Sinclair. "The application of high-resolution sequence stratigraphy to reservoir characterisation and development : Wyandra Sandstone Member, Cadna-Owie Formation, Eromanga Basin, Southwest Queensland / y Robert Sinclair Root." Thesis, Queensland University of Technology, 2001. https://eprints.qut.edu.au/37092/1/37092_Root_2001.pdf.

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Early sequence stratigraphic models emphasised the use of sequence stratigraphic surfaces for identifying and constraining the stratigraphic position of reservoir intervals at large scales (100s-1 000s of metres) using mostly seismic reflection data. In contrast, reservoir development focuses on resolving small­scale, largely lateral changes in reservoir quality and distribution where the stratigraphic position of the reservoir interval is generally already well defined. Also, due to the scale of analysis, the database for reservoir development studies commonly consists exclusively of well data (i.e. fullhole cores, wireline logs and image logs); fluid flow properties can be measured directly using the same data types that are employed to identify and map key surfaces. Despite well documented successes of the sequence stratigraphic approach at exploration scales, little information exists regarding the utility of sequence stratigraphic approach for reservoir development. This study investigates the utility of the sequence stratigraphic approach for aiding reservoir development of the Wyandra Sandstone Member at Tarbat-lpundu Field, Southwest Queensland. A sequence stratigraphic framework was constructed for the Wyandra Sandstone Member using a database of core, wireline suites, image logs, palynological data and modern analogues. The utility of the sequence stratigraphic framework for reservoir development was then evaluated using petrography and measurements of fluid flow properties from conventional core analysis and wireline logs. The Wyandra Sandstone Member is a -20m thick, volcaniclastic sandstone sheet that forms a fining-upward succession. Despite relative lithologic homogeneity, the sandstone sheet is characterised by severe variations in fluid flow properties stemming from complex patterns of diagenetic porosity/permeability occlusion and enhancement. A grain size control on the occurrence and intensity of secondary dissolution suggests that an understanding of grain size distribution within the_ Wyandra Sandstone Member is central to resolving reservoir heterogeneity. Sequence stratigraphic divisions of the Wyandra Sandstone Member indicate that it formed in response to a high-order regressive - transgressive cycle driven by glacio-eustatic fluctuation coupled with variation in the rate of basin subsidence from the Barremian to the Aptian. Seventy-three percent of reservoir rock within the Cadna-owie Formation is confined to the lower, fluvially dominated portion of the Wyandra Sandstone Member that is interpreted to represent a lowstand systems tract. However, the identification of the lowstand systems tract, in itself, is of limited value for reservoir development. Several uneconomic development wells have intersected low permeability sandstone within the lowstand systems tract. The largely lateral variations in reservoir properties within the lowstand systems tract of the Wyandra Sandstone Member stem from the partitioning of medium- to very coarse-grained sandstone to channelised fluvial distributary deposits. Although sandstone of fluvial distributary deposits show a range of fluid flow properties (0.01->1000mD), secondary dissolution of chemically unstable framework grains, authigenic clay and carbonate cement occurs preferentially in areas of intense channel amalgamation. These areas are interpreted as major fluvial axes similar to those that occur at the 'fan apex' of modern depositional systems of the Great Artesian Basin and modern transverse depositional systems occurring along strike-slip faults. The position of the major fluvial axes are interpreted to be controlled by localised changes in the style of basement faulting and related patterns of differential compaction in the overlying cover units. Mapping sequence stratigraphic surfaces, as distinct from lithologic surfaces, in the Cadna-owie Formation defines linkages of contemporaneous depositional systems. Consequently, the sequence stratigraphic divisions are compatible with studies of modern depositional systems, whereas lithologic divisions of the Cadna­owie Formation generally are not. As a result, a variety of analyses conducted with respect to sequence stratigraphic divisions, and particularly the utilisation of modern analogues, improves our understanding of the sedimentological processes operative during deposition of the Wyandra Sandstone Member. It is hoped that the conclusions stemming from this study provide a basis for more accurately accessing the development risk at Tarbat-lpundu Field.
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Martelle, Holly Anne. "Huron potters and archaeological constructs researching ceramic micro-stylistics /." online access from Digital Dissertation Consortium access full-text, 2002. http://libweb.cityu.edu.hk/cgi-bin/er/db/ddcdiss.pl?NQ69090.

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Mack, John Joseph. "At the Tip of the Prairie Peninsula: Flora and Natural History of Prairie Remnants in the Sandusky Plains of Crawford, Marion and Wyandot Counties, Ohio." The Ohio State University, 2002. http://rave.ohiolink.edu/etdc/view?acc_num=osu1396352347.

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Magee, Kathryn Claire. "Dispersed, But Not Destroyed: Leadership, Women, and Power within the Wendat Diaspora, 1600-1701." The Ohio State University, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=osu1306236416.

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Catalano, Joshua Casmir. "The Commemoration of Colonel Crawford and the Vilification of Simon Girty: How Politicians, Historians, and the Public Manipulate Memory." Bowling Green State University / OhioLINK, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1429202111.

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Bron, Katherine Ann. "Impact Sedimentation of the Tookoonooka and Talundilly marine impact structures, Australia: an impact reservoir generated by cratering in a petroleum basin." Thesis, 2015. http://hdl.handle.net/2440/115482.

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Tookoonooka and Talundilly are two large meteorite impact structures buried in the sedimentary rocks of central Australia, and are among the largest impact structures known on Earth. They are shown to be a rare example of an ancient marine impact event and are also an extremely rare terrestrial example of a probable binary impact event. A preserved marine impact ejecta horizon, interpreted to span a vast area of the continent and corresponding to the extent of a Cretaceous epicontinental sea, is used to biostratigraphically constrain the impact age to the Barremian-Aptian boundary (125 +/- 1 Ma) in the Lower Cretaceous. Evidence is presented that the Wyandra Sandstone Member petroleum reservoir overlying the horizon is, in part, a binary impact tsunamiite. Analyses of drill core, subsurface drilling data, and geological outcrops over >805,000 km² show that the base of the Wyandra Sandstone Member is an impact horizon: a widespread scour surface that is attributed to impact-related excavation and tsunami scour mechanisms. The impact horizon is underlain by seismites and overlain by very poorly sorted sediment with highly polymictic exotic clasts, imbricated pebbles, and intraformational cobble rip-up clasts. Exotic clasts are predominantly interpreted as impactoclasts, and include complex accretionary and armoured impactoclasts of vapour plume origin, shock-metamorphosed lithic fragments, and altered melt impactoclasts. Some lithic fragments resemble basement lithologies from the Tookoonooka and Talundilly target rock sequences. The stratigraphy of the Wyandra Sandstone Member contains elements characteristic of impact tsunami deposition including ejecta entrained in high flow regime bedforms, pebble to boulder-sized clasts, >16m thick beds, and cyclic sedimentation of tsunami couplets, across five depositional realms. These elements are in stark contrast to the persistently low-energy nature of the ambient sedimentation and overlying quiescent marine shales, but are consistent with the intense seismicity, high energy seiche action and rapid deposition expected from a marine impact in a mostly enclosed basin. A dual impact source is indicated, based on sediment distribution patterns in combination with the proximity of the impact structures in age and location. The Wyandra Sandstone Member records both marine impact depositional processes as well as the waning of the event; the upper part of the Wyandra returns to background depositional energies and intense bioturbation and is conformably overlain by transgressive marine shales. The Tookoonooka-Talundilly impact event may be an extreme prototype, as very few doublet craters, marine craters, impact tsunamiites, or economic impactites are individually known or preserved on Earth, yet this crater pair may represent all four. This impact crater pair provides a model for binary marine impact sedimentation and highlights the significance of ancient impact sediments to petroleum basins. Sedimentation patterns evidence a dual crater source even in a marine impact scenario where reworking and burial complicate the interpretation of depositional indicators; observations suggest that Tookoonooka-Talundilly may be the largest doublet crater discovered on Earth.
Thesis (Ph.D.) (Research by Publication) -- University of Adelaide, Australian School of Petroleum, 2015.
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Campbell, Jennifer. "The Huron of the Kawartha Lakes : faunal exploitation strategies as indicators of change during the Pre, Proto and Historic Periods /." 2004.

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Books on the topic "Wyandra"

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Marnie, Hill, ed. Wyandot County. Charleston, S.C: Arcadia, 2011.

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Pour une autohistoire amérindienne: Essai sur les fondements d'une morale sociale. Québec: Presses de l'Université Laval, 1989.

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Sioui, Georges E. Pour une histoire amérindienne de l'Amérique. [Québec]: Presses de l'Université Laval, 1999.

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Brébeuf, Mr. de (Georges), 1617-1661 and Cummins Bryan David 1953-, eds. The first French-Huron dictionary by Father Jean de Brébeuf and his Jesuit Brethren. Lewiston, N.Y: Edwin Mellen Press, 2010.

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Heidenreich, Conrad. Huronia: A history and geography of the Huron Indians, 1600-1650. [s.l: s.n.], 1988.

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Bland, Bill. Yourowquains, a Wyandot Indian queen: The story of Caty Sage. Elk Creek, Va: Historical Publications, 1992.

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Lainey, Jonathan C., and Louis-Jacques Dorais. Wendat et Wyandot d'hier et d'aujourd'hui: Eonywa'ndiyonhratehkwih chia' ekwäa'tatehkwih : actes du premier Congrès d'études wendat et wyandot, Wendake, Québec, 13 au 16 juin 2012. Wendake, Québec: Les éditions Hannenorak, 2013.

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Barbeau, Marius. Huron and Wyandot mythology: With an appendix containing earlier published records. Ottawa: Government Printing Bureau, 1990.

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Sioui, Georges E. Les Wendats, une civilisation méconnue. Sainte-Foy, Québec, Canada: Presses de l'Université Laval, 1994.

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A Huron-English/English-Huron dictionary (listing both words and noun and verb roots). Lewiston, N.Y: Edwin Mellen Press, 2007.

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Book chapters on the topic "Wyandra"

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Smith, B. M., M. E. Deptuck, and K. L. Kendell. "Upper Cretaceous Mass Transport Systems Above the Wyandot Formation Chalk, Offshore Nova Scotia." In Submarine Mass Movements and Their Consequences, 619–30. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-3071-9_50.

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Finkenbine, Roy E. "The Underground Railroad in “Indian Country”." In Fugitive Slaves and Spaces of Freedom in North America, 70–92. University Press of Florida, 2018. http://dx.doi.org/10.5744/florida/9780813056036.003.0004.

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From the establishment of the Greenville Treaty Line in 1795 to Wyandot removal in 1843, northwest Ohio constituted a “land apart” from the waves of white settlement that overwhelmed the eastern part of the Old Northwest. Native Americans—primarily Shawnee, Ottawa, and Wyandot—constituted the dominant population there, in what was often referred to as “Indian Country.” This region lay astride the primary northbound routes traversed by fugitive slaves from Kentucky, western Virginia, and beyond, heading to Canada via the Detroit River borderland or the western half of Lake Erie, and freedom seekers were frequently assisted by Native Americans. This chapter explores two regions in particular. One is the stretch of Ottawa villages along the Maumee River, where runaways were welcomed and protected, then taken to Fort Malden, Upper Canada, each year when Ottawa warriors went to receive their annual payment of goods for fighting on the British side during the War of 1812. The other is the Wyandot Grand Reserve at Upper Sandusky, which sponsored a maroon village of fugitive slaves called Negro Town for four decades. These two case studies serve as a point of departure for arguing that “Indian Country” was a unique space of freedom.
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"William Walker, Jr., Wyandot, 1800–1874." In Changing Is Not Vanishing, 64–66. University of Pennsylvania Press, 2011. http://dx.doi.org/10.9783/9780812200065.64.

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"Front Matter." In Forty Narratives in the Wyandot Language, i—viii. McGill-Queen's University Press, 2020. http://dx.doi.org/10.2307/j.ctv1gm00gk.1.

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"APPENDIX B:." In Forty Narratives in the Wyandot Language, 674–76. McGill-Queen's University Press, 2020. http://dx.doi.org/10.2307/j.ctv1gm00gk.9.

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"[Introduction]." In Forty Narratives in the Wyandot Language, 1–8. McGill-Queen's University Press, 2020. http://dx.doi.org/10.2307/j.ctv1gm00gk.4.

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"[Introduction]." In Forty Narratives in the Wyandot Language, 55–68. McGill-Queen's University Press, 2020. http://dx.doi.org/10.2307/j.ctv1gm00gk.6.

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"Translating the Stories." In Forty Narratives in the Wyandot Language, 69–648. McGill-Queen's University Press, 2020. http://dx.doi.org/10.2307/j.ctv1gm00gk.7.

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"Table of Contents." In Forty Narratives in the Wyandot Language, ix—xii. McGill-Queen's University Press, 2020. http://dx.doi.org/10.2307/j.ctv1gm00gk.2.

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"The Stories in English Based on the Re-Translations." In Forty Narratives in the Wyandot Language, 9–54. McGill-Queen's University Press, 2020. http://dx.doi.org/10.2307/j.ctv1gm00gk.5.

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Reports on the topic "Wyandra"

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Wade, J. A. Lithostratigraphy 7: Dawson Canyon and Wyandot formations. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210644.

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MacLean, B. C. Structure and isopach 6: depth to Wyandot Formation and oceanic horizon A*. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210678.

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MacLean, B. C. Structure and isopach 11: isopach map of Wyandot Formation to Petrel Marker. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210681.

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