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Letteratura scientifica selezionata sul tema "Glenelg"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 7 febbraio 2022

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Articoli di riviste sul tema "Glenelg"

1

Rawson, J. R., D. A. Carswell e D. Smallwood. "Garnet-bearing olivine-websterite within the Eastern Glenelg Lewisian of the Glenelg Inlier, NW Highlands". Scottish Journal of Geology 37, n. 1 (maggio 2001): 27–34. http://dx.doi.org/10.1144/sjg37010027.

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2

Anderson, J. A. C., e C. M. Gray. "Geological affinities of the Glenelg river complex, western Victoria". Australian Journal of Earth Sciences 41, n. 2 (aprile 1994): 141–55. http://dx.doi.org/10.1080/08120099408728122.

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3

Ii, Hiroyuki, John Sherwood e Nick Turoczy. "Salinization of the Glenelg River in Southwest Victoria, Australia". SIL Proceedings, 1922-2010 30, n. 10 (aprile 2010): 1515–19. http://dx.doi.org/10.1080/03680770.2009.11902367.

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4

STRACHAN, R. A., e P. J. TRELOAR. "A Grenville Sm/Nd age for the Glenelg eclogite". Nature 314, n. 6013 (aprile 1985): 754. http://dx.doi.org/10.1038/314754a0.

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5

SANDERS, I. S. "A Grenville Sm/Nd age for the Glenelg eclogite (reply)". Nature 314, n. 6013 (aprile 1985): 754–55. http://dx.doi.org/10.1038/314754b0.

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6

Lind, P. R., B. J. Robson, B. D. Mitchell e T. G. Matthews. "Can sand slugs in rivers deliver conservation benefits? The biodiversity value of tributary junction plug wetlands in the Glenelg River, Australia". Marine and Freshwater Research 60, n. 5 (2009): 426. http://dx.doi.org/10.1071/mf08175.

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Abstract (sommario):

Restoration works are carried out to alleviate human impacts and improve habitats within ecosystems. However, human impacts may also create new (anthropogenic) habitat for species to exploit. A dilemma arises when proposed restoration works would remove anthropogenic habitat and the assemblages it supports. Sediment input into the Glenelg River has formed tributary junction plug wetlands at confluences. Sand slug removal is proposed as part of river rehabilitation, but would also drain plug wetlands. We sampled four plug wetland, four river run and three river pool sites to determine whether plug wetlands influence water quality and add to the biodiversity of macroinvertebrates in the Glenelg River. Water quality and macroinvertebrate diversity were similar in plug wetlands, river runs and river pools. Assemblages were distinct among all sites, regardless of type, so there was no characteristic ‘plug-wetland fauna’. Therefore, although removal of plug wetlands would not cause a dramatic loss of invertebrate biodiversity, it would destroy anthropogenic habitat that supports a similar range of species to natural habitats in a river subject to multiple degrading processes. Gains from rehabilitation should be weighed against the value of anthropogenic habitat and the extent of similar habitat lost elsewhere in the ecosystem.

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7

Irving, A. D., K. F. Raphael, P. M. Rennison, R. Lewis, C. D. Cruickshank e R. A. Rengifo. "The Elgin, Franklin, Glenelg and West Franklin fields, Blocks 22/30b, 22/30c, 29/4d, 29/5b and 29/5c, UK North Sea". Geological Society, London, Memoirs 52, n. 1 (2020): 436–46. http://dx.doi.org/10.1144/m52-2018-47.

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AbstractThe Elgin, Franklin, Glenelg and West Franklin fields lie approximately 240 km (150 miles) east of Aberdeen in Blocks 22/30b, 22/30c, 29/4d, 29/5b and 29/5c of the UK Central Graben. Franklin was discovered in 1985, Elgin in 1991, Glenelg in 1999 and West Franklin in 2003. Elgin is a complex faulted anticline comprising four panels, while the others are simpler, tilted fault block structures. The main reservoir is the Upper Jurassic Fulmar Formation shoreface sandstone, although the Middle Jurassic Pentland and Triassic Skagerrak formations have also been produced on Franklin. Initial pressure was c. 1100 bar (16 000 psi), with a reservoir temperature of around 190°C (375°F). Production wells are drilled from four wellhead platforms; all connected to a central process, utilities and quarters facility above Elgin. Gas and condensate production started in 2001 from six wells on each of Elgin and Franklin, with the plateau being extended by satellite and infill wells. The project remains the world's largest high-pressure–high-temperature development, requiring continued innovations in geoscience, drilling, completion and operations. Cumulative production at end 2017 is 886 Mboe, with estimated ultimate recovery around 1300 Mboe.

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Davis, Wendy. "The End of an Era: Sixteen Years of the Adelaide Theological Library". ANZTLA EJournal, n. 12 (20 maggio 2015): 2–6. http://dx.doi.org/10.31046/anztla.vi12.278.

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Presented at the End of an Era dinner held 12th November, 2013 at the Glenelg Golf Club. The dinner marks the departure of Catholic Theological College from the Adelaide College of Divinity. Catholic Theological College ceases to exist from 2014. Catholic postgraduate students will continue their studies through the Australian Catholic University, and most staff of CTC will become part of the ACU faculty.

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9

Turner, S. P., C. J. Adams, T. Flöttmann e J. D. Foden. "Geochemical and geochronological constraints on the Glenelg River Complex, western Victoria". Australian Journal of Earth Sciences 40, n. 3 (giugno 1993): 275–92. http://dx.doi.org/10.1080/08120099308728080.

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10

Nicholson, Geoff, Gregory P. Jenkins, John Sherwood e Andy Longmore. "Physical environmental conditions, spawning and early-life stages of an estuarine fish: climate change implications for recruitment in intermittently open estuaries". Marine and Freshwater Research 59, n. 8 (2008): 735. http://dx.doi.org/10.1071/mf07197.

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Significant variation in the egg and larval survival and juvenile recruitment of estuarine fishes has been linked to fluctuating environmental conditions. This present study compared the distribution and abundance of black bream (Acanthopagrus butcheri) eggs and yolk-sac larvae between two microtidal estuaries of different flow regimes, where the riverine flow into the Glenelg estuary was around eight times the flow volume into the Hopkins estuary. Samples were collected monthly from September to November at sites along each estuary where vertical profiles of temperature, salinity and dissolved oxygen (DO) were measured, and vertically stratified sampling of black bream eggs and yolk-sac larvae was conducted using a Schindler sampler. Salt wedge formation was apparent in both estuaries, with significant de-oxygenation of deeper, saline waters. Eggs occurred in a wide range of DO levels but yolk-sac larvae were less common at the lowest levels. Most eggs and yolk-sac larvae were collected in salinities greater than 10. Results suggested that egg mortality was higher in the Hopkins than the Glenelg estuary, which may be associated with the hypoxic conditions characteristic of low-flow conditions. The results have significant implications in terms of climate change that is predicted to lead to warmer, drier conditions in south-eastern Australia, potentially increasing stratification and subsequent hypoxic zones.

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Tesi sul tema "Glenelg"

1

Richardson, Paul Anthony. "Fort Glenelg : the fort that never was /". Title page, contents and introduction only, 1987. http://web4.library.adelaide.edu.au/theses/09AR/09arr521.pdf.

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2

Schlapp, Julia Emily, e julia schlapp@rmit edu au. "Modelling Fertiliser Use in the Glenelg Hopkins Catchment". RMIT University. Mathematics and Geospatial Science, 2009. http://adt.lib.rmit.edu.au/adt/public/adt-VIT20090602.144534.

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The improvement of water quality in the streams of the Glenelg Hopkins catchment is a priority of the Glenelg Hopkins regional strategy. A major source of water pollution in the region is linked to agricultural activities as high nutrient levels from runoff have the potential to increase the incidence of blue-green algae in the waterways. Land use change, reduced rainfall, more frequent extreme rainfall events and higher temperatures associated with climate change are likely to exacerbate this trend. Water testing data of the Total Phosphorus (TP) levels in the Hopkins River and at other sites within the Hopkins Catchment indicate increasing incidence of TP above the Environment Protection Authority's target levels for extended periods of each year. Earlier research indicated that phosphorus in runoff increases when pasture fertility increases and that fertiliser management practices should be considered as an element of preventative action for reducing nutrient pollution. During our research, a survey was undertaken in the Hopkins River catchment, to determine the current management of phosphorus (P) fertilisers on grazing and mixed enterprise farms, the attitude of farmers to natural resource management and their understanding of nutrient pollution. The survey also gathered information on the way farmers made fertiliser management decisions. If cooperation relating to phosphorus fertiliser application could be facilitated between groups of farmers, it may be possible to reduce nutrient runoff into the Hopkins waterways. Cooperative game theory has successfully been used worldwide in the resolution of environmental problems where there is an economic impact to the decision making process. In this project, the amount of phosphorus applied per hectare was used in a cooperative game theory model assessing the potential for cooperative action on phosphorus management by groups of farmers, based on the trade off between the economic cost of pollution to the region waterways and the economic production benefits to the individual. The outcome of this work was individual optimal strategies for fertiliser application, allowing individual farmers to reduce their impact of agricultural production on the health of the catchment. Involving the farmer groups, while undertaking the project, raised awareness amongst the farming population of the regional nutrient pollution caused by runoff from agricultural land, and enlisted their assistance towards adopting a cooperative approach to the problem. In addition, the results have been mapped using a Geographical Information System (GIS) for visual presentation and to demonstrate the use of this process in natural resource management with the farmer groups.

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3

Salt, Christopher James. "Metamorphic and structural history of Glenelg, NW Scotland". Thesis, University of Edinburgh, 1995. http://hdl.handle.net/1842/11358.

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The Glenelg peninsular in NW Scotland contains Lewisian type rocks occurring east of the Moine thrust that have been metamorphosed and deformed along with the Moine rocks. These Lewisian rocks can be split into two facies, the Eastern Lewisian and the Western Lewisian, always separated by a thin strip of highly deformed Moine rocks. The Western Lewisian contains no recognisable meta-sediments, only a variety of meta-igneous rocks. Eclogite is rare, only occurring at one locality as pods within otherwise deformed amphibolite facies rocks. These eclogites exhibit broadly similar textures to the Eastern Lewisian eclogites, but have a slightly different chemistry, being more Si rich and Ca poor. They are formed under similar conditions of about 760°C, 15 Kb, but only one metamorphic event has been distinguished. Many of the amphibolites of the Western Lewisian have similar textures and chemistry as partly retrogressed Western Lewisian eclogite. These rocks were deformed to produce a weak fabric prior to the intrusion of further basic material that is texturally and chemically different to the eclogites. All of these rocks were then deformed and metamorphosed by the syn-Moine deformation as outlined above for the Eastern Lewisian. It is suggested that the Eastern and Western Lewisian rocks share a common history of initial high-pressure metamorphism, then the intrusion of granitic melt prior to further high pressure metamorphism. This was followed by deformation and partial retrogression before the intrusion of basic and ultrabasic dykes. The Lewisian rocks were then exhumed and the Moine rocks deposited onto them prior to further deformation and metamorphism. Radiometric dating suggests that the high pressure metamorphism occurred at approximately 1050 Ma (Grenville), but field and petrographic evidence suggests that the Lewisian rocks have undergone a similar history to the Scourian rocks of the main Lewisian outcrop and that Grenville ages for the rocks date initial syn- Moine metamorphism.

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4

Storey, Craig Darryl. "Tectono-metamorphic evolution of the Glenelg-Attadale Inlier, northwest Scotland". Thesis, University of Leicester, 2002. http://hdl.handle.net/2381/30451.

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The Glenelg-Attadale Inlier (GAI) is the largest tract of exposed basement rocks underlying the Moine Supergroup of northwest Scotland. The GAI is divided into two distinct crustal units, the Western Unit (WU) and the Eastern Unit (EU). The WU comprises dominantly Late Archaean acid gneisses of Tonalite-Trondhjemite-Granodiorite (TTG) affinity, cut by basic sheets. The WU underwent high-pressure granulite facies metamorphism and concomitant partial melting producing trondhjemites in the period 2600-2800 Ma ago. The WU underwent pervasive reworking at c.1750 Ma, possibly under eclogite facie conditions. A third event at c.1000 Ma affected the WU and involved amphibolite facies metamorphism and possibly eclogite facies metamorphism. The EU comprises mixed orthogneiss and paragneiss. Late Archaean trondhjemitic gneisses are intercalated with a Proterozoic volcano-sedimentary succession comprising marble, calc-pelite, pelite, manganiferous sediments and basic rocks. The EU underwent reworking at c.1440 to 1490 Ma, concomitant with the Pinwarian orogeny in North America and the Hallandian event in Scandinavia, suggesting a link. Eclogite facies metamorphism at c.1080 Ma occurred with the EU, at conditions of c.20kbar and 750Â°C. The EU was subsequently retrogressed and exhumed by 20-25km into the mid-crust at amphibolite facies by c.1000 Ma. The exhumation process was facilitated by ductile shearing at amphibolite facies. This major orogenic event in the period c.1080 to 1000 Ma is correlated with the Grenvillian-Sveconorwegian orogeny in north America and Scandinavia. The Moine Supergroup was deposited between c.1000 Ma and 870 Ma and was subsequently interleaved with the GAI by a process combining folding and ductile shearing at amphibolite facies. This interleaving process occurred in the period c.1000 to 670 Ma. The area underwent Caledonian folding and ductile shearing in the period c.440 to 425 Ma, prior to intrusion of the syn- to post-tectonic Ratagain Granite Complex.

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5

Quinn, Jason Matthew. "The adequacy of project based EIA for a complex coastal development : the Glenelg/West beach study". Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09ENV/09envq44.pdf.

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6

Rawson, John Robert. "Origin and metamorphic evolution of high pressure rocks in the Glenelg-Attadale inlier of the Caledonian Moine Thrust Nappe, Northwest Scotland". Thesis, University of Sheffield, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.397495.

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7

Lupton, Allison. "A collection and examination of the music and dance tradition supported by the Fiddlefern Dancers and the Glenelg Full Moon Country Dance Band in Owen Sound, Ontario". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape15/PQDD_0005/MQ34936.pdf.

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8

CHERMETTE, BRUNO. "Les fractures de la berge posterieure de la glene de l'omoplate : a propos de cinq observations". Lyon 1, 1989. http://www.theses.fr/1989LYO1M148.

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9

BAREA, CHRISTOPHE. "Modelisation 3d par la methode des elements finis d'une articulation scapulo-humerale. Application a l'etude des contraintes sur une epaule saine et avec differents types de glenes prothetiques". Toulouse 3, 1998. http://www.theses.fr/1998TOU30103.

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Un recent consensus affirme que la glene prothetique presente un role important dans la survie d'une prothese totale d'epaule. Malgre un faible taux de revision, de nombreuses radiographies montrant des pertes osseuses ou des demineralisations posent le probleme de la duree de vie a long terme de la fixation de l'implant dans l'os. Ceci demontre la necessite de developper un implant aboutissant a une stabilite de l'interface prothese-os avec un remodelage a long terme de l'omoplate. L'objectif de notre etude consiste a analyser le comportement biomecanique de l'epaule humaine saine et prothesee. Une technique ultrasonore nous a permis de determiner un atlas des proprietes mecaniques anisotropes de l'os spongieux glenoidien a partir de 11 paires omoplates cadaveriques. Ces donnees ont ete integrees dans les modelisations numeriques des modeles elements finis tridimensionnels ont ete developpes a partir de coupes tomodensitometriques. Par la suite, des calculs lineaires et non-lineaires ont ete effectues. Des etudes experimentales in vitro ont ete effectuees permettant de valider les resultats des calculs numeriques. Ainsi, ces etudes nous ont apporte de nouveaux elements pour une meilleure comprehension des problemes poses par la fixation des protheses d'epaule.

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Pain, Frédéric. "Analyse de l'influence d'une glène cimentée à deux plots sur les résultats d'une prothèse totale d'épaule, à partir des résultats radio-cliniques d'une série de 70 prothèses". Bordeaux 2, 2001. http://www.theses.fr/2001BOR23017.

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Libri sul tema "Glenelg"

1

Holman, Don. Ghost of Glenelg. Markdale, Ont: Always Press, 1995.

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2

MacDonald, Norman. The parish of Glenelg. [Inverness]: [Highland Libraries], 1992.

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3

Wildgoose, Martin. Archaeological watching brief: Lionachan,Moyle,Glenelg. Broadford,Isle of Skye: the author, 2002.

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4

Victoria. Office of the Auditor-General. Community planning services in Glenelg Shire Council: 1998-2005. [Melbourne]: Victorian Govt. Printer, 2005.

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5

Whitelock, Derek A. Down the Bay!: A history and appreciation of Glenelg, Brighton and Holdfast Bay. Brighton, S. Aust: City of Holdfast Bay, 2001.

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6

Dewar, Donald Keith. A genealogy study of the Dewar's of Glengarry, Ontario: The MacLoers of Galder Glenelg. Thorold, Ont: D.K. Dewar, 1997.

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7

ALTA Copper Conference (2000 Glenelg Beach, South Australia). ALTA 2000 Copper-6: Technical sessions : October 2-3, 2000, Stamford Grand Hotel, Glenelg Beach, Adelaide, South Australia. Castlemaine: ALTA Metallurgical Services, 2000.

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8

ALTA Copper Conference (2000 Glenelg Beach, South Australia). ALTA 2000 Copper-6: Technical sessions : October 2-3, 2000, Stamford Grand Hotel, Glenelg Beach, Adelaide, South Australia. Castlemaine: ALTA Metallurgical Services, 2000.

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9

Bain-Fallon Memorial Lectures (18th 1996 Glenelg, Australia). Equine neurology and nutrition: Proceedings of the 18th Bain-Fallon Memorial Lectures 22-26 July, 1996, Glenelg, South Australia. Artarmon, N.S.W: Australian Equine Veterinary Association, 1996.

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10

Bond, Head Francis. Canada: Copy of an explanatory memorandum addressed by Sir Francis Head to Lord Glenelg, dated the 21st of May last. [London: HMSO, 2001.

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Capitoli di libri sul tema "Glenelg"

1

"Glenlea Organic Rotation: A Long-Term Systems Analysis". In Managing Energy, Nutrients, and Pests in Organic Field Crops, 237–60. CRC Press, 2014. http://dx.doi.org/10.1201/b16044-19.

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2

Carkner, Michelle, Keith Bamford, Joanne Thiessen Martens, Sarah Wilcott, April Stainsby, Katherine Stanley, Calvin Dick e Martin H. Entz. "Building capacity from Glenlea, Canada's oldest organic rotation study". In Long-Term Farming Systems Research, 103–22. Elsevier, 2020. http://dx.doi.org/10.1016/b978-0-12-818186-7.00007-2.

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Atti di convegni sul tema "Glenelg"

1

Gordon, William, Iain Pittman, Mervyn Rydlewicz e John Ligertwood. "HP/HT WCCL Technology Aids Successful Deployment Perforating Operations on the Glenelg Field". In SPE/ICoTA Coiled Tubing and Well Intervention Conference and Exhibition. Society of Petroleum Engineers, 2008. http://dx.doi.org/10.2118/113835-ms.

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Rapporti di organizzazioni sul tema "Glenelg"

1

Rainbird, R. H., D. A. Hodgson e C. W. Jefferson. Bedrock and surficial geology, Glenelg Bay, District of Franklin, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194766.

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2

Avery, M. P. Vitrinite Reflectance [Ro] of Dispersed Organics From Shell Petro-canada Et Al., Glenelg J-48. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131305.

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3

Berger, B., D. Blaney, J. Bridges, A. Cousin, O. Forni, O. Gasnault, J. Lasue et al. POSSIBLE ALTERATION OF ROCKS OBSERVED BY CHEMCAM ALONG THE TRAVERSE TO GLENELG IN GALE CRATER ON MARS. Office of Scientific and Technical Information (OSTI), aprile 2013. http://dx.doi.org/10.2172/1077020.

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4

Karim, A., G. Pe-Piper e D. J. W. Piper. Distribution of diagenetic minerals in Lower Cretaceous sandstones and their relationship to stratigraphy and lithofacies: Glenelg, Thebaud and Chebucto fields, offshore Scotian Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2008. http://dx.doi.org/10.4095/225621.

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5

Rainbird, R. H., W. Darch, C. W. Jefferson, R. Lustwerk, M. Rees, K. Telmer e T A Jones. Preliminary stratigraphy and sedimentology of the Glenelg Formation, lower Shaler Group and correlatives in the Amundsen Basin, Northwest Territories: relevance to sediment-hosted copper. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132854.

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6

Pe-Piper, G., D. J. W. Piper, A. D. Vaughan, J. Shannon e S. Ingram. Sedimentary petrology of Lower Cretaceous rocks of the southwestern Sable sub-basin (North Triumph B-52, Alma K-85 and Glenelg N-49 wells), Scotian basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/216681.

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7

Salem, H. S. Detailed quantitative analyses of physical properties (measured and deduced) at one meter depth increments for the interval 355-5141 m (4786 m) of the Glenelg J-48 well in the Sable Island area, offshore Nova Scotia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/183956.

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