Relevant bibliographies by topics / Tasmania – Discovery and exploration

Academic literature on the topic 'Tasmania – Discovery and exploration'

Author: Grafiati
Published: 10 December 2022
Last updated: 29 January 2023

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Journal articles on the topic "Tasmania – Discovery and exploration"

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Tsang, Leah, Nicholas Carlile, Terry O’Dwyer, Mark Eldridge, Greta Frankham, and Hank Bower. "A recent specimen of a Tasmanian Boobook Ninox leucopsis recovered on Lord Howe Island." Australian Field Ornithology 39 (2022): 143–57. http://dx.doi.org/10.20938/afo39143157.

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On 11 July 2019, during the Rodent Eradication Program on Lord Howe Island using aerial and ground rodentbaiting, the recovery of dead non-target birds included a recently dead boobook Ninox sp. found on a resident’s property. Two Tyto species were also recovered. Despite automated sound-recording equipment stationed within the forests of the Island, no records of Ninox vocalisations were made before discovery of the boobook specimen; however, two instances of Ninox owl calls were reported anecdotally within The Settlement. There was speculation from some Island residents that the recovered boobook could have been an individual of the extinct endemic subspecies, the Lord Howe Boobook N. novaeseelandiae albaria. The boobook was forwarded to the Australian Museum for further visual scrutiny, collection of morphometric data, DNA analysis, and preparation for the Australian Museum collection. There was overlap in plumage and morphological measurements between both the Tasmanian Boobook (N. leucopsis) and the nominate Tasman Morepork from New Zealand (N. n. novaeseelandiae), but the specimen was distinct from the larger Australian mainland N. boobook. DNA analysis provided conclusive evidence that the bird was a male N. leucopsis, exhibiting an overall clean-white spotted pattern and darker brown coloration. The occurrence of a Ninox species on Lord Howe Island is the first record in more than 50 years and should prompt further exploration of the dispersal and possible migration of boobooks from Tasmania.
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Heath, N. M. "GIPPSLAND—NEW POTENTIAL FROM A MATURE BASIN." APPEA Journal 43, no. 1 (2003): 223. http://dx.doi.org/10.1071/aj02011.

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It is now 39 years since the first gas was discovered in Bass Strait’s Gippsland Basin. Advances in exploration and production technology mean that today Australia’s longest producing offshore basin is also one of Australia’s most prospective. Gippsland is now producing around 160,000 barrels of crude and 570 million cubic feet of gas per day. To date it has produced more than 3.5 billion barrels of oil and 5 trillion cubic feet of gas and the value of the infrastructure in place is estimated to be around A$16 billion.Australia’s evolving energy market means that gas demand continues to grow. Following the re-structuring of energy markets in southeastern Australia and the installation of new pipeline infrastructure, Gippsland gas now flows to Victoria, NSW, Tasmania and will supply into South Australia from 2004. To meet this growing demand the Esso/BHPBilliton joint venture partners are investing heavily and utilising a vast array of 3D exploration technology to unlock new opportunities. In 2002 they conducted the largest 3D survey ever undertaken in Bass Strait and expect to conduct another in early 2003. A program of exploration drilling is expected to commence in late 2003. With expanded market opportunities and a gas resource base of more than 5 trillion cubic feet, the future looks bright for Gippsland.
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Eshaghi, Esmaeil, Anya M. Reading, Michael Roach, Mark Duffett, Daniel Bombardieri, Matthew J. Cracknell, John L. Everard, Grace Cumming, and Stephen Kuhn. "Inverse modeling constrained by potential field data, petrophysics, and improved geologic mapping: A case study from prospective northwest Tasmania." GEOPHYSICS 85, no. 5 (July 28, 2020): K13—K26. http://dx.doi.org/10.1190/geo2019-0636.1.

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The Heazlewood-Luina-Waratah area is a prospective region for minerals in northwest Tasmania, Australia, associated with historically important ore deposits related to the emplacement of granite intrusions and/or ultramafic complexes. The geology of the area is poorly understood due to the difficult terrain and dense vegetation. We have constructed an initial high-resolution 3D geologic model of this area using constraints from geologic maps and geologic and geophysical cross sections. This initial model is improved upon by integrating results from 3D geometry and physical property inversion of potential field (gravity and magnetic) data, petrophysical measurements, and updated field mapping. Geometry inversion reveals that the Devonian granites in the south are thicker than previously thought, possibly connecting to deep sources of mineralization. In addition, we identified gravity anomalies to the northeast that could be caused by near-surface granite cupolas. A newly discovered ultramafic complex linking the Heazlewood and Mount Stewart Ultramafic Complexes in the southwest also has been modeled. This implies a greater volume of ultramafic material in the Cambrian successions and points to a larger obducted component than previously thought. The newly inferred granite cupolas and ultramafic complexes are targets for future mineral exploration. Petrophysical property inversion reveals a high degree of variation in these properties within the ultramafic complexes indicating a variable degree of serpentinization. Sensitivity tests suggest maximum depths of 2–3 km for the contact aureole that surrounds major granitic intrusions in the southeast, whereas the Heazlewood River complex is likely to have a deeper source up to 4 km. We have demonstrated the value of adding geologic and petrophysical constraints to 3D modeling for the purpose of guiding mineral exploration. This is particularly important for the refinement of geologic structures in tectonically complex areas that have lithology units with contrasting magnetic and density characteristics.
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Moore, A. M. G., H. M. J. Stagg, and M. S. Norvick. "DEEP-WATER OTWAY BASIN: A NEW ASSESSMENT OF THE TECTONICS AND HYDROCARBON PROSPECTIVITY." APPEA Journal 40, no. 1 (2000): 66. http://dx.doi.org/10.1071/aj99005.

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The northwest-trending Otway Basin in southeast Australia formed during the separation of Australia and Antarctica between the latest Jurassic and the Early Cainozoic. A new, deep-seismic data set shows that the basin comprises two temporally and spatially overlapping rift components:the mainly Late Jurassic to mid-Cretaceous, east-west trending, inner Otway Basin—comprising the onshore basin and most of the continental shelf basin; andthe northwest–southeast to north–south trending depocentres beneath the outer shelf and continental slope, extending from eastern South Australia to the west coast of Tasmania, and a relatively minor and ill-defined sub-basin underlying the continental rise in water depths greater than about 4,500 m. This rift system was most active from the mid-Cretaceous to Palaeogene, and was strongly affected by sinistral strike-slip motion as Australia and Antarctica separated.The continental slope elements contain the bulk of the sediment volume in the basin. From northwest to southeast, these elements comprise the Beachport and Morum Sub-basins, the north-south trending Discovery Bay High, and the Nelson Sub-basin which appears to be structurally and stratigraphically continuous with the Sorell Basin off west Tasmania.The reflection character of the crust and upper mantle varies widely across the basin, and there is a strong correlation between that character and the basin configuration. It appears that accommodation space beneath the slope basin was created largely by extension and removal of most of the laminated deep continental crust.There is encouragement for hydrocarbon exploration in the deep-water basin. Firstly, there are indications of diagenesis related to fluid flow in and above the strongly faulted Cretaceous section in the Morum Sub-basin. As an Early Cretaceous petroleum system is already proven beneath the continental shelf, this suggests that the same system is also active in deep-water. Secondly, existing sample data suggest that a second, Late Cretaceous petroleum system could be active where any source rocks are sufficiently deeply buried; this condition would probably be met in the Nelson Sub-basin.
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Frieling, Joost, Emiel P. Huurdeman, Charlotte C. M. Rem, Timme H. Donders, Jörg Pross, Steven M. Bohaty, Guy R. Holdgate, Stephen J. Gallagher, Brian McGowran, and Peter K. Bijl. "Identification of the Paleocene–Eocene boundary in coastal strata in the Otway Basin, Victoria, Australia." Journal of Micropalaeontology 37, no. 1 (February 13, 2018): 317–39. http://dx.doi.org/10.5194/jm-37-317-2018.

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Abstract. Detailed, stratigraphically well-constrained environmental reconstructions are available for Paleocene and Eocene strata at a range of sites in the southwest Pacific Ocean (New Zealand and East Tasman Plateau; ETP) and Integrated Ocean Discovery Program (IODP) Site U1356 in the south of the Australo-Antarctic Gulf (AAG). These reconstructions have revealed a large discrepancy between temperature proxy data and climate models in this region, suggesting a crucial error in model, proxy data or both. To resolve the origin of this discrepancy, detailed reconstructions are needed from both sides of the Tasmanian Gateway. Paleocene–Eocene sedimentary archives from the west of the Tasmanian Gateway have unfortunately remained scarce (only IODP Site U1356), and no well-dated successions are available for the northern sector of the AAG. Here we present new stratigraphic data for upper Paleocene and lower Eocene strata from the Otway Basin, southeast Australia, on the (north)west side of the Tasmanian Gateway. We analyzed sediments recovered from exploration drilling (Latrobe-1 drill core) and outcrop sampling (Point Margaret) and performed high-resolution carbon isotope geochemistry of bulk organic matter and dinoflagellate cyst (dinocyst) and pollen biostratigraphy on sediments from the regional lithostratigraphic units, including the Pebble Point Formation, Pember Mudstone and Dilwyn Formation. Pollen and dinocyst assemblages are assigned to previously established Australian pollen and dinocyst zonations and tied to available zonations for the SW Pacific. Based on our dinocyst stratigraphy and previously published planktic foraminifer biostratigraphy, the Pebble Point Formation at Point Margaret is dated to the latest Paleocene. The globally synchronous negative carbon isotope excursion that marks the Paleocene–Eocene boundary is identified within the top part of the Pember Mudstone in the Latrobe-1 borehole and at Point Margaret. However, the high abundances of the dinocyst Apectodinium prior to this negative carbon isotope excursion prohibit a direct correlation of this regional bio-event with the quasi-global Apectodinium acme at the Paleocene–Eocene Thermal Maximum (PETM; 56 Ma). Therefore, the first occurrence of the pollen species Spinizonocolpites prominatus and the dinocyst species Florentinia reichartii are here designated as regional markers for the PETM. In the Latrobe-1 drill core, dinocyst biostratigraphy further indicates that the early Eocene (∼ 56–51 Ma) sediments are truncated by a ∼ 10 Myr long hiatus overlain by middle Eocene (∼ 40 Ma) strata. These sedimentary archives from southeast Australia may prove key in resolving the model–data discrepancy in this region, and the new stratigraphic data presented here allow for detailed comparisons between paleoclimate records on both sides of the Tasmanian Gateway.
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Baillie, P. W. "PETROLEUM EXPLORATION IN TASMANIA IN 1985." APPEA Journal 26, no. 2 (1986): 74. http://dx.doi.org/10.1071/aj85054.

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Baillie, P. W., and N. J. Russell. "VITRINITE PALAEOTHERMOMETRY OF OFFSHORE EXPLORATION WELLS, TASMANIA." APPEA Journal 29, no. 1 (1989): 130. http://dx.doi.org/10.1071/aj88016.

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Over the last three decades organic metamorphism (coalification), as indicated by changes in vitrinite reflectivity, has been regarded as a function of both temperature and heating duration. This temperature- time concept of coalification has been developed into sophisticated computer programs to model the palaeo- geothermal history of sedimentary basins. However, several papers, published over the last six years, have presented evidence to support the view that, for heating times in excess of 0.001- 1 Ma, vitrinite reflectivity constitutes an absolute palaeogeothermometer. This proposition is broadly supported by a comparison between corrected bottom- hole temperature (BHT) and vitrinite reflectivity data from offshore petroleum exploration wells drilled in Tasmanian waters. Most of the corrected BHT/vitrinite reflectivity data pairs plot on, adjacent to or between two of the published vitrinite temperature/reflectance trends. Although these data indicate that some formations are at, or near, maximum palaeotemperature, there is clear evidence to suggest that many samples, in particular those from formations in the deeper well sections, have cooled significantly below maximum palaeotemperature. It appears that present- day geothermal gradients for some of the wells, based on corrected BHT data, are much less than maximum palaeogeothermal gradients inferred from the vitrinite depth/reflectance relationship.
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Leaman, L. E. "Exploration Significance of Gravity Surveys, Rosebery Mine, Tasmania." Exploration Geophysics 22, no. 1 (March 1991): 231–34. http://dx.doi.org/10.1071/eg991231.

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Bendall, M. R., J. K. Volkman, D. E. Leaman, and C. F. Burrett. "RECENT DEVELOPMENTS IN EXPLORATION FOR OIL IN TASMANIA." APPEA Journal 31, no. 1 (1991): 74. http://dx.doi.org/10.1071/aj90007.

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Recent work on oil seeps, organic geochemistry, geophysics, structural geology and palaeontology suggests that there is considerable potential for onshore petroleum in Tasmania.Archival research has shown that hydrocarbon seeps were commonly reported in the first half of this century and that wildcats produced gas (at Port Sorell in the north) and oil (at Johnson's Well on Bruny Island, in the south). Almost all of the 270 historical hydrocarbon occurrences lie on lineaments revealed independently by gravity and magnetic surveys. The thermal maturity of conodonts from Ordovician and Siluro-Devonian carbonates suggests that much of the pre-Upper Carboniferous beneath the Tabberabberan unconformity is within the oil and gas windows.Organic geochemistry reveals a very close similarity between hydrocarbons from Ordovician limestones, those from the drill site at Bruny Island and with tar samples from the Tasmanian coast, but little similarity with the Permian Tasmanite Oil Shale, or with the Gippsland crudes and botryococcane-rich South Australian bitumens. The predominance of C27 steranes in Tasmanian bitumens suggests a widespread algal source and the abundant diasteranes imply a clay or silt-rich source that extends across much of Tasmania.Recent geophysical and structural work suggests that a thin skinned interpretation of Tasmania's structure is reasonable. Most sightings of hydrocarbons are associated with either faults or fractures which have post-Jurassic displacements or with intersections of major high angle faults with thrusts. The delineation of reservoirs within the thrust sheets is a priority.
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Kriwoken, Lorne K., and John W. Williamson. "Hobart, Tasmania: Antarctic and Southern Ocean connections." Polar Record 29, no. 169 (April 1993): 93–102. http://dx.doi.org/10.1017/s0032247400023548.

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abstractThis paper describes the historical and contemporary associations between Hobart (Tasmania, Australia) and Antarctica and the Southern Ocean. This association is traced from the sealing and whaling industry, through early exploration and scientific expeditions, to contemporary issues of institutional and educational development and tourism. I is argued that this polar link has placed Hobart at the centre of some important Antarctic and Southern Ocean developments.
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Dissertations / Theses on the topic "Tasmania – Discovery and exploration"

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Haase, Kenneth W. "Invention and exploration in discovery." Thesis, Massachusetts Institute of Technology, 1990. http://hdl.handle.net/1721.1/14257.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Electrical Engineering and Computer Science, 1990.
Includes bibliographical references (leaves 159-161).
by Kenneth William Haase Jr.
Ph.D.
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Riembau, Marc. "Exploration of the higgs sector after its discovery." Doctoral thesis, Universitat Autònoma de Barcelona, 2018. http://hdl.handle.net/10803/663947.

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El descobriment del bosó de Higgs és la culminació d’una recerca que ha durat 40 anys, i completa un marc teòric sota el qual gairebé totes del dades obtingudes de col·lisionadors de partícules poden ser explicades consistentment. Simultàniament, i paradoxalment, l’aparent con rmació d’una separacó d’escales entre l’electrofeble i la que suposadament estabilitza la masa del bosó de Higgs posa el relleu el problema de la jerarquia. En la recerca d’una descripció del món que simpli qui els patrons i simetries del Model Estàndard, l’exploració de l’escala dels TeVs i en particular l’estudi del bosó de Higgs tindran un paper central. En aquesta tesi presentem les possibilitats que el LHC i futurs col·lisionadors proveiran, amb énfasi en la determinació de l’auto-acoblament del bosó de Higgs. També considerarem l’estudi de la producció de bosons electrofebles com a eina per entendre les interaccions dels bosons de Golstone que formen part del doblet de Higgs, mostrant la seva rellevància al combinar-ho amb les dades del pol de la Z i altres cerques al LHC. Finalment, ens centrem en com el moment dipolar elèctric de l’electró posa fortes restriccions en models on el bosó de Higgs és descrit com un estat compost.
The discovery of the Higgs boson culminates a 40-year long hunt and completes a theoretical framework under which almost all collider data can be consistently explained. At the same time, paradoxically, the con rmation of an apparent mass gap above the electroweak scale exacerbates the problem of the electroweak hierarchy. In the search of a description of the world that simpli es the patterns and symmetries of the Standard Model, the exploration of the TeV scale and in particular the study of the Higgs boson will play a central role. In this thesis we explore the possibilities that the LHC and future colliders will bring, with particular emphasis on the determination of the Higgs self-coupling. We also consider the pair production of electroweak bosons as a probe of the Goldstone interactions in the Higgs doublet, and show its relevance as a way to improve the Z pole measurements and its interplay with other LHC searches. Finally, we focus on how the electron’s electric dipole moment can set strong constraints on models where the Higgs arises as a composite state.
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Savovic, Jelena. "Exploration of dynamic combinatorial chemistry in enzyme-inhibitor discovery." Thesis, University of Bath, 2003. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.760840.

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Ross, Karen C. "“Awake:” An Animated Exploration of Self-Discovery Through Mindfulness." The Ohio State University, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=osu1471826821.

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Hedden, Chet. "A guided exploration model of problem-solving discovery learning /." Thesis, Connect to this title online; UW restricted, 1998. http://hdl.handle.net/1773/7683.

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Wu, Fei. "Knowledge discovery in time-series databases." Versailles-St Quentin en Yvelines, 2001. http://www.theses.fr/2001VERS0023.

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@Aborde trois problématiques dans le contexte de la base de données temporelles. Ils sont le problème de regroupement, la similarité et l'extraction des stratégies. Il reste encore des problèmes pour les travaux futurs. Par exemple, comment réaliser le regroupement graduel pour d'autres algorithmes. Il sera intéressant de grouper des séquences en se basant sur notre nouveau modèle. Mais les questions posées sont le choix d'un algorithme, ou il faut un nouvel algorithme carrément ? Pour construire une stratégie, ce sera aussi possible de pré-définir nos actions. Puis trouver les relations entre les actions et les indicateurs correspondants afin de générer des stratégies. . .
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St, Onge Joseph. "The Geography of Exploration: A Study in the Process of Physical Exploration and Geographical Discovery." DigitalCommons@USU, 2000. https://digitalcommons.usu.edu/etd/6581.

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Exploration has been a common literary topic throughout the history of humans. However, much of this historical tradition bas possessed a fairly narrow Ill focus, emphasizing the drama and heroics of an individual explorer or concentrating on a description of a particular exploration. There has been little attempt at understanding the process of exploration and placing this important process in context with the historic and geographic phenomena that both affect and are affected by it. In this thesis, the author has broken the process of exploration down into a theoretical structure that is presented in a holistic model. This model has then been applied to the history of 15th century Portuguese exploration to test its applicability and usefulness.
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Burlington, Michael Scott. "Search & exploration, efficient planar search for automated robotic discovery." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape3/PQDD_0031/MQ64328.pdf.

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Burlington, Scott M. Sc. "Search & exploration : efficient planar search for automated robotic discovery." Thesis, McGill University, 1999. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=30352.

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An agent is placed in an unknown environment and charged with the task of locating a lost object. What can the agent use as an efficient technique to find the object?
We propose a new algorithm for planar search. The algorithm stems from theoretical work on search games, in particular provably optimal search techniques on restricted domains. This thesis addresses the problem of efficiency in robotic search: having a mobile robot find a target object in an unknown environment with obstacles in an efficient manner. As a side-effect, the robot explores the environment.
Based on previous results, a formal description of the problem is presented along with an algorithm to solve it. This algorithm has good worst-case performance, in terms of its competitive ratio. We show experimental data validating the feasibility of our approach and typical results. Quantitative results are demonstrated showing the advantage of modified spiral search versus traditional approaches.
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Huffman, Ashley. "Discovery of Movement: An Exploration of Physical Activity through Architecture." University of Cincinnati / OhioLINK, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=ucin149130367713521.

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Books on the topic "Tasmania – Discovery and exploration"

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Binks, C. J. Explorers of Western Tasmania. Devonport Tasmania, Australia: Taswegia, 1989.

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Tasman, Abel Janszoon. The discovery of Tasmania: Journal extracts from the expeditions of Abel Janszoon Tasman and Marc-Joseph Marion Dufresne, 1642 & 1772. Hobart, Tasmania, Australia: St. David's Park Pub., 1992.

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McMahon, Libby. Exploring the South Land: Tasmania emerges from Terra Australis Incognita. [Lindisfarne, Tas.]: Maritime Museum of Tasmania by 40 Degrees South, 2006.

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An officer of the blue: Marc-Joseph Marion Dufresne, South Sea explorer, 1724-1772. Carlton, Vic: Melbourne University Press, 1994.

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Slot, B. Abel Tasman and the discovery of New Zealand. Amsterdam: O. Cramwinckel, 1992.

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Wells, William L. Immense enjoyment: The illustrated journals & letters of William L. Wells, 1884-1888 : the life of an early Quaker family in Tasmania. Devonport, Tas: Devon Historical Society, 1987.

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Plomley, N. J. B. The general: The visits of the expedition led by Bruny d'Entrecasteaux to Tasmanian waters in 1792 and 1793. Launceston: Queen Victoria Museum, 1993.

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D, Roeper V., and Wildeman Diederick, eds. Het journaal van Abel Tasman, 1642-1643. Den Haag: Nationaal Archief, 2006.

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Anderson, Grahame. The merchant of the Zeehaen: Isaac Gilsemans and the voyages of Abel Tasman. Wellington: Te Papa Press, 2001.

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Binks, C. J. Pioneers of Tasmania's west coast. Hobart [Tasmania]: Blubber Head Press, 1988.

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Book chapters on the topic "Tasmania – Discovery and exploration"

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Nürnberger, Andreas. "Exploration: Overview." In Bisociative Knowledge Discovery, 285–86. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-31830-6_19.

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Hsu, Chang Samuel, and Paul R. Robinson. "Exploration for Discovery." In Petroleum Science and Technology, 83–95. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-16275-7_6.

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Glyndwr, Williams. "Exploration and Discovery." In Handbook for History Teachers, 1037–40. London: Routledge, 2021. http://dx.doi.org/10.4324/9781032163840-182.

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Gibson, Michael R. "Exploration and Discovery." In Handbook for History Teachers, 451–58. London: Routledge, 2021. http://dx.doi.org/10.4324/9781032163840-57.

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Vedder, Heinrich. "Discovery and Exploration." In South West Africa in Early Times, 3–40. London: Routledge, 2022. http://dx.doi.org/10.4324/9780429025426-2.

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Mihelčić, Matej, and Tomislav Šmuc. "InterSet: Interactive Redescription Set Exploration." In Discovery Science, 35–50. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-46307-0_3.

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Leemans, Sander J. J. "Process Discovery and Exploration." In Business Process Management Workshops, 582–85. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-15895-2_52.

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Hochheiser, Harry, and Ben Shneiderman. "Interactive Exploration of Time Series Data." In Discovery Science, 441–46. Berlin, Heidelberg: Springer Berlin Heidelberg, 2001. http://dx.doi.org/10.1007/3-540-45650-3_38.

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Hoffman, Jeffrey A. "Exploration and Discovery in Space." In Leadership and Discovery, 121–41. New York: Palgrave Macmillan US, 2009. http://dx.doi.org/10.1057/9780230101630_8.

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Haun, Stefan, Tatiana Gossen, Andreas Nürnberger, Tobias Kötter, Kilian Thiel, and Michael R. Berthold. "On the Integration of Graph Exploration and Data Analysis: The Creative Exploration Toolkit." In Bisociative Knowledge Discovery, 301–12. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-31830-6_21.

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Conference papers on the topic "Tasmania – Discovery and exploration"

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Godber, Kate, John Bishop, and Roger Lewis. "Hot rocks down under: Exploration for enhanced geothermal power in Tasmania, Australia." In SEG Technical Program Expanded Abstracts 2007. Society of Exploration Geophysicists, 2007. http://dx.doi.org/10.1190/1.2793039.

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Kinkela, J., A. Dzunic, M. Urosevic, R. MacRae, and L. Webb. "Seismic Exploration for Volcanogenic Massive Sulphides - The Rosebery Zinc, Lead, Copper Mine, Tasmania." In 76th EAGE Conference and Exhibition - Workshops. Netherlands: EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20140518.

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Silic, J., E. T. Eadie, and D. J. Jack. "Application of time-domain electromagnetic methods in the discovery of the Hellyer ore deposit, Tasmania, Australia." In 1985 SEG Technical Program Expanded Abstracts. SEG, 1985. http://dx.doi.org/10.1190/1.1892699.

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Zudilova-Seinstra, Elena, Jean-Bernard Martens, and Tony Adriaansen. "Interactive data exploration and knowledge discovery." In the International Conference. New York, New York, USA: ACM Press, 2010. http://dx.doi.org/10.1145/1842993.1843099.

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Kellermann, Kenneth I., James M. Cordes, Ronald D. Ekers, Joseph Lazio, and P. Wilkinson. "The Exploration of the Unknown." In Accelerating the Rate of Astronomical Discovery. Trieste, Italy: Sissa Medialab, 2010. http://dx.doi.org/10.22323/1.099.0005.

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Cameron, Delroy, Pablo N. Mendes, Amit P. Sheth, and Victor Chan. "Semantics-empowered text exploration for knowledge discovery." In the 48th Annual Southeast Regional Conference. New York, New York, USA: ACM Press, 2010. http://dx.doi.org/10.1145/1900008.1900029.

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Frieder, Ophir. "Session details: Data exploration and discovery (KM)." In CIKM07: Conference on Information and Knowledge Management. New York, NY, USA: ACM, 2007. http://dx.doi.org/10.1145/3250805.

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Spurlock, Darren. "Space Exploration Systems Integration." In 1st Space Exploration Conference: Continuing the Voyage of Discovery. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2005. http://dx.doi.org/10.2514/6.2005-2541.

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Ardanuy, Philip, Richard Boehne, James Head, Tim Howard, Nick Powell, and Scott Kulinski. "Antarctic Exploration: Proxy for Safe, Sustainable Exploration of the Moon and Mars." In 1st Space Exploration Conference: Continuing the Voyage of Discovery. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2005. http://dx.doi.org/10.2514/6.2005-2506.

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Al-Bulushi, A. A. B., and M. E. S. Elshafie. "Using Stochastic Inversion for STOIIP Estimation of Sub-seismic Exploration Discovery." In Fourth EAGE Exploration Workshop. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201700219.

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Reports on the topic "Tasmania – Discovery and exploration"

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Lin, Xiao. Development and exploration of potential routes of discovery of new superconductors. Office of Scientific and Technical Information (OSTI), January 2013. http://dx.doi.org/10.2172/1226557.

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David Ebert, David Ebert. Looking for Lost Sharks: An Exploration of Discovery through the Western Indian Ocean. Experiment, June 2016. http://dx.doi.org/10.18258/7209.

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Lawley, C. J. M., and B A Kjarsgaard. Bottom-up mineral exploration: ore-element upgrading in the upper mantle and tools for its discovery. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2020. http://dx.doi.org/10.4095/323674.

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Mukherjee, S., M. Lisa, H. Petersen, M. Stephanov, and P. Sorensen. Proceedings of RIKEN BNL Research Center Workshop: Theory and Modeling for the Beam Energy Scan: From Exploration to Discovery. Office of Scientific and Technical Information (OSTI), March 2015. http://dx.doi.org/10.2172/1188213.

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Vesselinov, Velimir. Cloud Fusion of Big Data and Multi-Physics Models using Machine Learning for Discovery, Exploration and Development of Hidden Geothermal Resources. Office of Scientific and Technical Information (OSTI), April 2021. http://dx.doi.org/10.2172/1781345.

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Houlé, G., H. L. Gibson, L. Richan, V. Bécu, D. Corrigan, and L. Nadeau. A new nickel discovery in the Prince Albert Hills, Melville Peninsula, Nunavut: implications for Ni-Cu-(PGE) exploration in the Prince Albert Group. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2010. http://dx.doi.org/10.4095/287185.

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Houlé, G., H. L. Gibson, L. Richan, V. Bécu, D. Corrigan, and L. Nadeau. A new nickel discovery in the Prince Albert Hills, Melville Peninsula, Nunavut: implications for Ni-Cu-(PGE) exploration in the Prince Albert Group. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2012. http://dx.doi.org/10.4095/291526.

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Vesselinov, Velimir, Daniel O'Malley, Luke Frash, Bulbul Ahmmed, Adam Rupe, Satish Karra, Richard Middleton, et al. Geo Thermal Cloud: Cloud Fusion of Big Data and Multi-Physics Models using Machine Learning for Discovery, Exploration, and Development of Hidden Geothermal Resources. Office of Scientific and Technical Information (OSTI), May 2021. http://dx.doi.org/10.2172/1782607.

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Corriveau, L., J. F. Montreuil, O. Blein, E. Potter, M. Ansari, J. Craven, R. Enkin, et al. Metasomatic iron and alkali calcic (MIAC) system frameworks: a TGI-6 task force to help de-risk exploration for IOCG, IOA and affiliated primary critical metal deposits. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/329093.

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Australia's and China's resources (e.g. Olympic Dam Cu-U-Au-Ag and Bayan Obo REE deposits) highlight how discovery and mining of iron oxide copper-gold (IOCG), iron oxide±apatite (IOA) and affiliated primary critical metal deposits in metasomatic iron and alkali-calcic (MIAC) mineral systems can secure a long-term supply of critical metals for Canada and its partners. In Canada, MIAC systems comprise a wide range of undeveloped primary critical metal deposits (e.g. NWT NICO Au-Co-Bi-Cu and Québec HREE-rich Josette deposits). Underexplored settings are parts of metallogenic belts that extend into Australia and the USA. Some settings, such as the Camsell River district explored by the Dene First Nations in the NWT, have infrastructures and 100s of km of historic drill cores. Yet vocabularies for mapping MIAC systems are scanty. Ability to identify metasomatic vectors to ore is fledging. Deposit models based on host rock types, structural controls or metal associations underpin the identification of MIAC-affinities, assessment of systems' full mineral potential and development of robust mineral exploration strategies. This workshop presentation reviews public geoscience research and tools developed by the Targeted Geoscience Initiative to establish the MIAC frameworks of prospective Canadian settings and global mining districts and help de-risk exploration for IOCG, IOA and affiliated primary critical metal deposits. The knowledge also supports fundamental research, environmental baseline assessment and societal decisions. It fulfills objectives of the Canadian Mineral and Metal Plan and the Critical Mineral Mapping Initiative among others. The GSC-led MIAC research team comprises members of the academic, private and public sectors from Canada, Australia, Europe, USA, China and Dene First Nations. The team's novel alteration mapping protocols, geological, mineralogical, geochemical and geophysical framework tools, and holistic mineral systems and petrophysics models mitigate and solve some of the exploration and geosciences challenges posed by the intricacies of MIAC systems. The group pioneers the use of discriminant alteration diagrams and barcodes, the assembly of a vocab for mapping and core logging, and the provision of field short courses, atlas, photo collections and system-scale field, geochemical, rock physical properties and geophysical datasets are in progress to synthesize shared signatures of Canadian settings and global MIAC mining districts. Research on a metamorphosed MIAC system and metamorphic phase equilibria modelling of alteration facies will provide a foundation for framework mapping and exploration of high-grade metamorphic terranes where surface and near surface resources are still to be discovered and mined as are those of non-metamorphosed MIAC systems.
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Mills, Stephanie E., and Bear Jordan. Uranium and Vanadium Resources of Utah: An Update in the Era of Critical Minerals and Carbon Neutrality. Utah Geological Survey, September 2021. http://dx.doi.org/10.34191/ofr-735.

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Utah is the second largest vanadium producing state and the third largest uranium producing state in the United States. Carnotite, a primary ore mineral for both vanadium and uranium, was first discovered and used by Native Americans as a source of pigment in the Colorado Plateau hysiographic province of eastern Utah. Radioactive deposits have been ommercially mined in Utah since about 1900, starting with radium, followed by vanadium, and thenuranium. In 1952, the discovery of the Mi Vida mine in Utah’s Lisbon Valley mining district in San Juan County kicked off a uranium exploration rush across the Colorado Plateau. As a result, the United States dominated the global uranium market from the early 1950s to late 1970s. In the modern mining era, Utah is an important contributor to the domestic uranium and vanadium markets with the only operating conventional uranium-vanadium mill in the country, multiple uranium-vanadium mines on standby, and active uranium-vanadium exploration. Overall, Utah has produced an estimated 122 million lbs U3O8 and 136 million lbs V2O5 since 1904. Most of this production has been from the sandstone-hosted deposits of the Paradox Basin, with minor production from volcanogenic deposits and as byproducts from other operations across the state
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