Dissertations / Theses on the topic 'Group Tracker'
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Till, Přemysl. "Nástroje pro počítání a monitorování osob." Master's thesis, Vysoké učení technické v Brně. Fakulta elektrotechniky a komunikačních technologií, 2021. http://www.nusl.cz/ntk/nusl-442531.
Full textWatkins, Laura Louise. "Tracer populations in the local group." Thesis, University of Cambridge, 2011. https://www.repository.cam.ac.uk/handle/1810/240582.
Full textBoinet, Pauline. "Adolescence scarifiée : traces et mouvements symboliques d'un groupe à médiation écriture." Thesis, Lyon, 2018. http://www.theses.fr/2018LYSE2004.
Full textThe specificity of adolescence is the coming to the fore of genitality. This involves both a metamorphosis of the body and a psychic reworking. The body is also a place of contradiction that sometimes attacks, sometimes it embellishes in a frenzied eroticism. Indeed, the contradiction can be translated in symptomatic form and manifest the clutter that the adolescent feels in front of his body that escapes him. He does not know how to identify what he feels, he does not know how to name it and he does not even know he does not know. Sometimes the relationship he has with his body is sufficiently paradoxical that he can't appropriate it. It is this strangeness that will cause a cleavage in the adolescent. The two perspectives that emanate from these positions are quite different as to the future of the subject. This work is a continuation of various research works on the adolescent problem. He reports on the establishment of a therapeutic group in writing in a Pediatric General Service, writing with teenagers who are scarifying themselves. It is by considering these scarifications as a body language at the heart of the adolescent and pubertal problem, and in view of the difficulties that these teenagers have to put words on the indescribable of their pain, that the group was created. The setting up of this one corresponds more generally to a reflection on the process of adolescence, of subjectivation, and the relation with the body, in particular through the work of symbolization in adolescence. We also question the place of our reflection, the mediation writing as a deposit of a trace on a support, which as well as the meeting of the blade on the skin, would come as a stop (Le Breton, 2002); the encounter with the sheet by analogy with the body would come to recreate and offer a container for psychic suffering. The group could be seen as a transitional space in Winnicott's sense, at the root of the creative and reassuring experience for the teenager. The body would then have a similar function in what it would incarnate a border between an inside and an outside. One of the functions of the scarificatory practice would then be to restore the limits of the Self in a fight against a possible collapse
Steiner, Beat A. "Cyclic homology and Hattori-Stallings traces for group-graded algebras /." Zürich : ETH, 2007. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=17164.
Full textSköldvall, Henning. "Able pupils in different groups : A comparative study of interaction in tracked and mixed-ability groups." Thesis, Stockholms universitet, Institutionen för språkdidaktik, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-88143.
Full textFelisberto, Valente Gustavo. "The Eulerian Bratteli Diagram and Traces on Its Associated Dimension Group." Thesis, Université d'Ottawa / University of Ottawa, 2020. http://hdl.handle.net/10393/40608.
Full textSondecker, Victoria L. "Kernel-trace approach to congruences on regular and inverse semigroups." Instructions for remote access. Click here to access this electronic resource. Access available to Kutztown University faculty, staff, and students only, 1994. http://www.kutztown.edu/library/services/remote_access.asp.
Full textSource: Masters Abstracts International, Volume: 45-06, page: 3173. Abstract precedes thesis as [2] preliminary leaves. Typescript. Includes bibliographical references (leaves 52-53).
Kenley, Stefania. "Du pastiche à l'original : traces et trajectoires de l'Independent Group (1952-1956)." Paris 8, 2005. http://www.theses.fr/2005PA082512.
Full textBetween 1952 and 1956, the Independent Group gathered at the Institute of Contemporary Arts (ICA), London, the leading figures of architecture such as Alison and Peter Smithson, Colin St John Wilson, of art, such as Richard Hamilton, Eduardo Paolozzi, William Turnbull, Nigel Henderson, or of history and criticism of art and architecture, such as Reyner Banham, Lawrence Alloway. The shifting and uncertain composition of the group and the absence of any joint publication, manifesto or programme, brings up the question of the IG as a genuine group, as well as the importance of the choice of the name Independent. The title From pastiche to Masterpiece indicates a method where the history of the group is examined through flash-backs, constructed from the available historical traces. Between 2002 and 2005, interviews and correspondence helped to clarify the meaning given by certain ex-members of the IG to the key notions of Pop art, such as collage, pastiche, "multiples", repetition, that made the question of the Original central to the research
Farrell, Amy Carissa. "Study skills of high school mathematics students compared by achievement within tracked groups /." Abstract, 2008. http://eprints.ccsu.edu/archive/00000522/01/1971ABSTR.htm.
Full textThesis advisor: Robin S. Kalder. "... in partial fulfillment of the requirements for the degree of Master of Science in Mathematics." Includes bibliographical references (leaves 23-25). Also available via the World Wide Web.
Lange, Torsten. "Tracing flow and salinization processes at selected locations of Israel and the West Bank - the Judea Group Aquifer and the Shallow Aquifer of Jericho." Doctoral thesis, Technische Universitaet Bergakademie Freiberg Universitaetsbibliothek "Georgius Agricola", 2013. http://nbn-resolving.de/urn:nbn:de:bsz:105-qucosa-100679.
Full textSemiaride und aride Gebiete stellen aufgrund des niedrigen oder ungünstig verteilten Niederschlagsdargebots eine besondere Herausforderung bezüglich Erkundung, Bereitstellung, nachhaltiger Nutzung und Schutz sich neu bildender, aber auch fossiler Wasserresourcen dar. Abgesehen von wenigen natürlichen oder künstlich angelegten Oberflächenreservoiren ist der poröse Untergrund dabei gleichzeitig Hauptspeicher und Transportmedium für Wasser und bietet einen Schutz gegen Verdunstung und bis zu einem gewissen Grade gegen oberflächig einwirkende Verunreinigungen. Diese Situation ist charakteristisch für den Nahen Osten und damit für die im Rahmen der vorliegenden Arbeit beschriebenen Teiluntersuchungsgebiete, die sich in Israel und der West Bank befinden. Die Arbeit behandelt drei Hauptthemen. Einerseits geht sie auf die Charakterisierung der Jungwasseranteile im Abfluß vier bedeutender Quellen des Wadi Qilts und Jerichos sowie in beprobten tiefen Brunnen dreier wichtiger Brunnenfelder ein. Alle diese Objekte entwässern bzw. entnehmen Wasser aus dem Oberen oder Unteren Judea Group Aquifer. Mit ca. 750 m Mächtigkeit stellt dieser eines der bedeutensten Grundwasserreservoire der Region dar und besteht hauptsächlich aus unterschiedlich stark verkarsteten und gestörten Kalkstein- und Dolomitformationen, welche zwischen dem Senon und Eozän in Form einer in sich weiter gegliederten, beid-seitig abtauchenden Doppelantiklinalstruktur herausgehoben wurde (Hebron und Ramallah bzw. Judea und Samaria Mountains). Die Grundwasserneubildung ist beschränkt auf die Zeit zwischen Oktober und April sowie auf die Kammlagen des Gebirges, wo die sonst bedeckten Schichten des Aquifers ausstreichen. Es wurde eine Strategie entwickelt, die eingesetzten Tracer auf ähnliche Weise mit Hilfe von Lumped Parameter-Modellen für alle Lokationen zu interpretieren und somit eine Vergleichbarkeit zu gewährleisten. Andererseits untersucht die Arbeit Versalzungsprozesse im Shallow Aquifer von Jericho und deren Abgrenzung untereinander. Mögliche Hauptquellen der Versalzung sind durch überhöhte Grundwasserentnahme verstärke Zuflüsse von Solen, die Lösung von Salzen aus der Lisan-Formation oder Formationswässer der Lisan-Formation, welche die Ablagerungen des Lisan-Sees, des Pleistozänen Vorgängers des heutigen Toten Meeres, repräsentieren. Eine Unterscheidung der Mechanismen hat dabei durchaus Bedeutung für die Festlegung geeigneter Gegenmaßnahmen. Demzufolge werden die ermittelten, aber auch weitere, potentielle hydrochemische Hauptindikatoren und Tracer benannt. Unsicherheiten sowohl hinsichtlich der Aufstellung einer Wasserbilanz, als auch einer unzureichend bekannten Geologie für das sehr kleinräumige Gebiet von Jericho werden diskutiert
Li, Wen-Wei. "Vers une formule des traces stable pour le groupe métaplectique." Phd thesis, Université Paris-Diderot - Paris VII, 2011. http://tel.archives-ouvertes.fr/tel-00606273.
Full textMcNeilly, David Andrew. "The trace spectrum of Fuchsian groups of signature (0;4;0)." Thesis, University of Cambridge, 1996. https://www.repository.cam.ac.uk/handle/1810/252179.
Full textMartins, Áudrea da Costa. "Linhas, vozes e tracks : a textura na composição musical de crianças." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2011. http://hdl.handle.net/10183/36016.
Full textThe present research is an approach to acoustic and electronic collective musical composition by music students aged between 10 and 12. It aims to analyze the several demonstrations which involve musical texture, pointing out the way those are attached to the conception of time and the processes of inference which grant musical creation activity. The subject-matter is composed by 16 regular students from public schools who attended workshop on composition guided by the researcher. The conception of such study places the research in the area of Jean Piaget´s Genetic Epistemology whose theoretical body gives support to investigation in Musical Education area. The data have been collected during the period of November 2010 to April 2011 in the researcher´s work environment in which she performed interviews based on the adopted theoretical reference. The decision-making during the compositional process meets support in the inferences and in the concepts of sequence, length and simultaneousness which are inherent in time concept. In spite of the differences as to the compositional approach and the sound results of the musical products, the textural manifestation in the acoustic and electronic pieces proved to be similar in many aspects. The musical texture, important structural dimension in music, is a fundamental parameter in the exercise of composition. It offers a wide rank for the experimenting and creating expression of its authors. So, this work can bring new approaches in the compositional practice in group in the classroom which will provide a better comprehension in the student’s musical production.
Green, Damon Antony. "Determination and behaviour of platinum group and associated trace-elements in ocean sediments." Thesis, Kingston University, 1996. http://eprints.kingston.ac.uk/20595/.
Full textCampbell, Leslie Ann. "Palaeoecology of the middle to late Cambrian Rogersville Shale, Conasauga Group, eastern Tennessee." Thesis, Boston College, 2008. http://hdl.handle.net/2345/351.
Full textThe Rogersville Shale of the Middle to Late Cambrian Conasauga Group was deposited on the margins of Laurentia, in what is now eastern Tennessee. Based on 21 thin section samples from the ORNL-Joy2, core five distinct microlithofacies are described, trace fossils characterized, and palynological data interpreted. This investigation concluded that the Rogersville Shale was deposited in a shallow, restricted marine or possibly estuarine environment that would have been exposed to terrestrial runoff. Previous work on the Conasauga Group placed deposition of the Rogersville Shale within an intercratonic basin in approximately 250m of water, perhaps significantly deeper. This investigation found that the Rogersville Shale was likely deposited in a lagoonal setting or restricted estuarine environment that had freshwater input
Thesis (MS) — Boston College, 2008
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Geology and Geophysics
Fedosov, Boris, Bert-Wolfgang Schulze, and Nikolai Tarkhanov. "On index theorem for symplectic orbifolds." Universität Potsdam, 2003. http://opus.kobv.de/ubp/volltexte/2008/2655/.
Full textLazareva, Olesya. "Detailed geochemical and mineralogical analyses of naturally occurring arsenic in the Hawthorn Group." [Tampa, Fla.] : University of South Florida, 2004. http://purl.fcla.edu/fcla/etd/SFE0000521.
Full textAl, Harbat Sadek. "Groupe de tresses affine, algèbre de Temperley-Lieb affine et trace de Markov." Paris 7, 2013. http://www.theses.fr/2013PA077204.
Full textIn this thesis we define a tower of affine Temperley-Lieb algebras of Type  on which we define a Markov trace and we show that there is a unique such trace. In order to do so, we work on four levels of type À : affine braid groups, affine Coxeter groups, affine Hecke algebras and affine Temperley-Lieb algebras On the braid level, we show that À-type affine braid group with n+1 generators surjects onto A-type affine braid group with n generators, we prove that this surjection cornes from a quotient on a certain subgroup and we define a closure of an element of this group which is to be called an affine link. On the Coxeter level, we study the À-type affine Coxeter group with n+1 generators, we give a full set of representatives of left cosets and double cosets of the À-type affine Coxeter group with n generators, then we classify fully commutative elements and we give a normal form for such elements. On the Hecke level, we define a tower of A-type affine Hecke algebras, we show that this tower is a tower of inclusions, and we show that this tower surjects onto the tower of A-type Hecke algebras. On the Temperley-Lieb level, we define a tower of Â-type affine Temperley-Lieb, we define a Markov trace as a collection of traces on this tower in its most general form (compatibrirty with affine links). We get the existence of such trace by showing that the mentioned tower surjects onto the tower of A-type Temperley-Lieb algebras and finally we show that this trace is unique by making use of the normal form of the fully commutative elements
Qi, Liang, and 漆亮. "Determination of trace platinum group elements in geological samples: application to Emeishan flood basalts in SWChina." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2007. http://hub.hku.hk/bib/B38791079.
Full textChan, Ping-Shun. "Invariant representations of GSp(2)." Columbus, Ohio : Ohio State University, 2005. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1132765381.
Full textQi, Liang. "Determination of trace platinum group elements in geological samples application to Emeishan flood basalts in SW China /." Click to view the E-thesis via HKUTO, 2007. http://sunzi.lib.hku.hk/hkuto/record/B38791079.
Full textRossin, David Alan Peter. "The development of a process trace methodology that effectively identifies the information needs of a management group." Thesis, University of Salford, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.245034.
Full textKunsevi-Kilola, Carine. "The effect of Rooibos on trace elements absorption and biochemical parameters-Amurine model." Thesis, Cape Peninsula University of Technology, 2014. http://hdl.handle.net/20.500.11838/1463.
Full textOver the past few decades, it has been shown that various critical diseases including heart disease, cancer, and diabetes associated with free radical generation and low endogenous antioxidant capacity, lead to oxidative stress and cell injury. In recent years, numerous studies have also reported that antioxidants, present in various beverages, vegetables and some foods have attracted a significant research interest due to their potential benefits to human health. However, epidemiological evidence shows a correlation between the intake of food rich in antioxidants and the reduced incidence of some mortality of chronic diseases, certain cancers and coronary heart disease. The aims of this study were to determine the effects of rooibos teas (fermented and unfermented) and green tea as a comparison on the biochemical parameters and the trace element absorption in a rat model. In this study 4 groups of experimental animals were used. All groups had ad libitum access to standard rat chow. Group A, the controls (11 animals), were fed with tap water; group B (11 animals) were fed with the liquid extract of fermented rooibos tea; group C (9 animals) were fed with the liquid extracts of unfermented rooibos and group D (9 animals) were fed with the liquid extract of green tea. All groups were fed for a period of 10 weeks. After the feeding period, the animals were sacrificed by euthanization with intraperitoneal injections of pentobarbital. Blood was sampled by cardiac puncture and centrifuged to obtain the serum. Some elemental analyses were performed with X-ray emission and backscattering. ICP-OES was used to determine the magnesium content. For X-ray emission, backscattering and ICP-OES analyses, 100 μL of each serum sample in a group were added to 2 mL freeze-drying tube. Of the combined specimen, 100 μL was used for the magnesium determination by ICP-OES. The remainder of the combined serum specimens for each group were freeze-dried at -80 ºC and then pressed into a pellet. The pellet was coated with carbon and analyzed using X-ray emission and backscattering. The elemental X-rays of P, S, Ca, Mn, Fe, Cu, Co, Zn, Mo, Ca and Se emitted were quantified to obtain the respective concentrations. Biochemical chemistry analyses were performed on each serum sample of each animal. The biochemical parameters tested for were total protein, albumin, globulin, total bilirubin, lactate dehydrogenase, blood urea nitrogen, uric acid, total cholesterol, aspartate aminotransferase, alanine aminotransferase, creatine phosphokinase and creatinine. The P concentration increased (p=0.028) when fed with the fermented rooibos tea liquid extract and S content increased when fed with the - the unfermented tea liquid extract (p=0.041). The concentrations of Cl and Cr were not affected (p>0.05) by any of tea liquid extracts. The unfermented rooibos tea liquid extract and the green tea indicated a decrease in the concentrations of Fe (p=0.031 and p=0.032, respectively) and Mn (p=0.041 and p=0.034, respectively). The concentrations of Fe, Zn and Cu in the serum increased when feeding with fermented rooibos tea liquid extract (p=0.024; p=0.030 and p=0.015, respectively) while Se, Mo and Mg concentrations were decreased by the liquid extracts of the fermented, unfermented and green teas (p=0.014, p=0.017 and p=0.011; p=0.024, p=0.026 and p=0.019; p=0.031, p=0.034 and p=0.025, respectively). Concerning the biochemical parameters, the total protein, globulin and the uric acid contents in the serum sample were slightly affected with the green tea extract (p=0.041, p=0.039 and p=0.047 respectively). The albumin, lactate dehydrogenase, blood urea nitrogen, the total cholesterol, the alanine aminotransferase and the aspartate aminotransferase concentrations were not affected (p>0) by any of the tea liquid extracts. However, the total bilirubin content was decreased (p=0.012) when feeding with the fermented rooibos group while the creatine phosphokinase and the creatinine contents were decreased (p=0.042 and p=0.033, respectively) when feeding with the unfermented rooibos tea liquid extract.
Reth, Margot. "New approaches for the mass spectrometric determination of trace concentrations and congener group patterns of chlorinated paraffins in biota /." Basel : [s.n.], 2006. http://edoc.unibas.ch/diss/DissB_7617.
Full textHaubold, Niko. "Compressed Decision Problems in Groups." Doctoral thesis, Universitätsbibliothek Leipzig, 2012. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-85413.
Full textHorak, Tracey Anne. "An analysis of the caesarean section rate at Mowbray Maternity Hospital using Robson's Ten group Classification System by Tracey Anne Horak." Master's thesis, University of Cape Town, 2012. http://hdl.handle.net/11427/3046.
Full textSuzuki, Miyu. "Quaternion distinguished representations and unstable base change for unitary groups." Kyoto University, 2020. http://hdl.handle.net/2433/253065.
Full textShin, Hyunshik. "Algebraic degrees of stretch factors in mapping class groups." Diss., Georgia Institute of Technology, 2014. http://hdl.handle.net/1853/51910.
Full textNaing, Thann. "Palaeoenvironmental studies of the Middle Triassic uppermost Narrabeen Group, Sydney Basin palaeoecological constraints with particular emphasis on trace fossil assemblages /." Phd thesis, Australia : Macquarie University, 1991. http://hdl.handle.net/1959.14/71228.
Full textThesis (PhD)--Macquarie University, School of Earth Sciences, 1991.
Bibliography: p. 596-630.
PART 1. INTRODUCTION AND METHODOLOGY -- General introduction -- Methodology -- Classification of ichnofacies and lithofacies as used in the present study -- Definition of trace fossil zones (intervals, subintervals and levels) -- General classification of the palaeoenvironments and summary overview of the stratigraphic and geographic distribution of palaeoenvironments in the study area -- PART 2. SYSTEMATIC ICHNOTAXONOMY -- Large dwelling-burrows -- U-shaped burrows -- Vertical cylindrical burrows -- Thalassinoides, Ophiomorpha, Spongeliomorpha and turn-arounds -- Pellets and ovoid-shaped structures -- Bedding-parallel feeding and/or dwelling structures -- Dendritic feeding-burrows -- Rosette-shaped structures -- Escape-structures -- Tracks, trails and resting-traces -- Body fossils and root-penetration structures -- Miscellaneous traces -- PART 3. SYNTHESIS AND CONCLUSIONS -- Trace fossil assemblages (suites) in intervals IC to IF and their distribution in the study area -- Interpretation of the palaeoenvironmental affinities of the trace fossil zones and depositional setting of the study area -- Palaeogeographic synthesis and conclusions.
The coastal exposures of the Triassic System in the Sydney Northshore area aggregate about 180 m in thickness and comprise the uppermost part of the Narrabeen Group (namely, in ascending stratigraphic order: the Bald Hill Claystone, the Garie Formation, and the Newport Formation, the latter divisible into Lower, Middle and Upper Members) and the overlying Hawkesbury Sandstone. With the exception of mainly allochthonous plant macrofossils and palynomorphs which occur sporadically and with varying abundance in the mudrock facies of these formations, environmentally-diagnostic body fossils are rare, and, where they occur, are nowhere unequivocally indicative of marine affinities. For this reasons, and because of the predominantly fluvial lithofacies characteristics exhibited by these formations throughout much of their stratigraphic extent and especially by their channel-form/channel-like sandstones lithosomes, most previous workers have interpreted these formations to be of fluvial or fluvio-lacustrine origin except possibly for several thin planar-and thinly-bedded fine-grained intervals encompassing the Garie and Newport Formations for which several lines of evidence, including lithofacies, equivocal palaeontological, and ichnological evidence, have prompted several workers to speculate a shallow- marine, possibility coastal lagoonal or estuarine origin. -- Although trace fossils occur in reasonable abundance at various stratigraphic levels within these uppermost Narrabeen Group rocks and particularly within the Newport Formation, they have hitherto received very little systematic study. A comprehensive study of this ichnofauna shows that it is relatively diverse, comprising almost 100 different ichnotaxa (including varietal categories) of predominantly invertebrate origin, and includes several new ichnogenera and ichnospecies among the more notable of which are: two large bioglyph-bearing dwelling-burrows of probable crustacean origin (Turimettichnus conaghani and T. webbyi) and one (Pytiniichnus trifurcatum) made either by a small reptile or an amphibian; a multi-stage spiral star-shaped feeding-trace (Helikospirichnus veeversi), probably made by a worm or worm-like deposit-feeder; several new species and varieties of Rhizocorallium (the first record of this ichnogenus in the Triassic of Australia); a new species and new variety of the saltatorial running vertebrate trackway Moodieichnus (an ichnogenus previously known only from the Late Permian of North America); and a new ichnogenus of vertical/steeply-inclined cylindrical branching dwelling-burrow (Barrenjoeichnus mitchelli). -- An alternating stratigraphic pattern of trace fossil abundance and diversity characterizes the upper Narrabeen Group strata in the Sydney Northshore area, and involves four relatively thin separate assemblage zones of relatively diverse ichnofauna and thicker intervening assemblage zones which lack ichnotaxo-nomic diversity. The assemblage zones of diverse trace fossils contain some elements in common to two or more zones, notably: Thalassinoides, Skolithos, Ophiomorpha, Chondrites, Rhizocorallium Palaeophycus, and Planolites, all of which are known to have unequivocal brackish- to shallow-marine palaeoecological affinities and which globally are characteristic of the Skolithos ichnofacies. Additionally, each of these four diverse assemblage zones is characterized by one or more particular index ichnogen-era which for convenience lend their name(s) to the zones as follows, in ascending stratigraphic order: Turimettichnus-Ophio-morpha assemblage zone; Skolithos-Diplocraterion assemblage zone; Helikospirichnus assemblage zone; and Rhizocorallium-Thalass inoides assemblage zone. The intervening ichnotaxonomically less-diverse and relatively impoverished assemblage zones are not similarly and separately named but are characterized by Barrenjoeichnus mitchelli and some species of Palaeophycus, Planolites and Skolithos as well as various plant-root petrification structures, all of which are here argued to have predominantly non-marine palaeoecological affinities. These latter assemblage zones can be referred to the Scoyenia-Teredolites ichnofacies. This stratigraphic pattern of alternating ichnologi-cally diverse and impoverished assemblage zones confirms the suggestions of previous workers (notably Bunny and Herbert, and Retallack) regarding the presence of brackish-/shallow-marine palaeoenvironmental influence in these Lower and Middle Triassic strata and allow for the first time the stratigraphic resolution of the marine strata into four marine tongues which are here named after their respective type localities. These are, in ascending order: The Turimetta Head Tongue (2 m to 3 m thick; extending from at least the middle part of the Bald Hill Clay-stone almost to the top of this formation); the St. Michaels Cave Tongue (4 m to 5 m thick; encompassing the Garie Formation and the lower part of the lower Member of the Newport Formation); the Bangalley Head Tongue (3 m to 5 m thick; extending from the uppermost part of the Lower Member into the lower part of the Middle Member of the Newport Formation); and the Palm Beach Tongue (3 m to 4 m thick; comprising the uppermost part of the Middle Member of the Newport Formation). The trace fossil assemblages in each of these marine tongues are indicative of a complex of brackish- to very shallow-marine low-energy palaeoenvi-ronments typical of modern coastal lagoons or estuaries and imply the presence of a protecting coeval topographic barrier of some kind to the east or southeast. This lagoon is herein called the Newport (Coastal) Lagoon and its development in the central-eastern part of the Sydney Basin coincides approximately with the geographic and depocentral axis of the basin which trends NW-SE and intersects the present coastline in the Sydney metropolitan area. The non-marine affinities of the impoverished and less-diverse trace fossil assemblages in the intervening and overlying strata are consistent with the fluvial/fluvio-lacustrine environmental interpretations of these thicker and predominantly sandstone-dominant intervals made by many other workers. Palaeocur-rent and petrographic data from these fluvial sediments show that the streams in which they formed debouched episodically into the Newport Lagoon variously from the northwest, west and southwest and were sourced variously from both the craton (Lachlan Fold Belt) to the southwest and the New England Orogen to the northeast.
With the exception of evidence of short-lived brackish-marine conditions at the base of the Narrabeen Group in the northeastern Sydney Basin and in the top of the Ashfield Shale in the Wianamatta Group (above the Hawkesbury Sandstone) in the central part of the basin, the Triassic System of the basin is dominated by fluvial/fluvio-lacustrine sediments and the presently described marine tongues of the Newport Lagoon in the uppermost Narrabeen Group are the only other presently known record of marine conditions during the Triassic history of the basin. The development of the Newport Lagoon in the geographic and depocentral axis of the basin attests to the presence of a mild short-lived marine transgression in the latest Early and early Middle Triassic at the end of a period of declining piedmont clastic alluviation from the coeval New England Orogen to the northeast and immediately prior to the onset of a new phase of fluvial sedimentation sourced from the craton to the southwest and manifested by the deposition of the Middle Triassic Hawkesbury Sandstone.
Mode of access: World Wide Web.
xxxv, 630 p. ill., maps
Clarke, Nerida, and n/a. "A study of the information needs and information-seeking behaviour of Australian accredited coaches in the sports of swimming and track and field." University of Canberra. Information, Language & Culture, 1995. http://erl.canberra.edu.au./public/adt-AUC20060628.150854.
Full textHa, Ngoc-Phu. "Théorie quantique des champs topologiques pour la superalgèbre de Lie sl(2/1)." Thesis, Lorient, 2018. http://www.theses.fr/2018LORIS505/document.
Full textThis text studies the quantum group Uξ sl(2|1) associated with the Lie superalgebra sl(2|1) and a category of finite dimensional representations. The aim is to construct the topological invariants of 3-manifolds using the notion of modified trace. We first prove that the category CH of the nilpotent weight modules over Uξ sl(2|1) is ribbon and that there exists a modified trace on its ideal of projective modules. Furthermore, CH possesses a relative G-premodular structure which is a sufficient condition to construct an invariant of 3-manifolds of Costantino-Geer-Patureau type. This invariant is the heart of a 1+1+1-TQFT (Topological Quantum Field Theory). Next Hennings proposed from a finite dimensional Hopf algebra, a construction of invariants which does not require to consider the category of its representations. We show that the unrolled H l l quantum group Uξ sl(2|1)/(e1 , f1 ) has a completion which is a topological ribbon Hopf algebra. We construct an invariant of 3-manifolds of Hennings type using this algebraic structure, a discrete Fourier transform, and the notion of G-integrals. The integral in a Hopf algebra is central in the construction of Hennings. The notion of modified trace in a category has recently been revealed to be a generalization of the integrals in a finite dimensional Hopf algebra. In a more general context of infinite dimensional Hopf algebras we prove the relation formulated between the modified trace and the G-integral
Pilourdault, Julien. "Scalable algorithms for monitoring activity traces." Thesis, Université Grenoble Alpes (ComUE), 2017. http://www.theses.fr/2017GREAM040/document.
Full textIn this thesis, we study scalable algorithms for monitoring activity traces. In several domains, monitoring is a key ability to extract value from data and improve a system. This thesis aims to design algorithms for monitoring two kinds of activity traces. First, we investigate temporal data monitoring. We introduce a new kind of interval join, that features scoring functions reflecting the degree of satisfaction of temporal predicates. We study these joins in the context of batch processing: we formalize Ranked Temporal Join (RTJ), that combine collections of intervals and return the k best results. We show how to exploit the nature of temporal predicates and the properties of their associated scored semantics to design TKIJ , an efficient query evaluation approach on a distributed Map-Reduce architecture. Our extensive experiments on synthetic and real datasets show that TKIJ outperforms state-of-the-art competitors and provides very good performance for n-ary RTJ queries on temporal data. We also propose a preliminary study to extend our work on TKIJ to stream processing. Second, we investigate monitoring in crowdsourcing. We advocate the need to incorporate motivation in task assignment. We propose to study an adaptive approach, that captures workers’ motivation during task completion and use it to revise task assignment accordingly across iterations. We study two variants of motivation-aware task assignment: Individual Task Assignment (Ita) and Holistic Task Assignment (Hta). First, we investigate Ita, where we assign tasks to workers individually, one worker at a time. We model Ita and show it is NP-Hard. We design three task assignment strategies that exploit various objectives. Our live experiments study the impact of each strategy on overall performance. We find that different strategies prevail for different performance dimensions. In particular, the strategy that assigns random and relevant tasks offers the best task throughput and the strategy that assigns tasks that best match a worker’s compromise between task diversity and task payment has the best outcome quality. Our experiments confirm the need for adaptive motivation-aware task assignment. Then, we study Hta, where we assign tasks to all available workers, holistically. We model Hta and show it is both NP-Hard and MaxSNP-Hard. We develop efficient approximation algorithms with provable guarantees. We conduct offline experiments to verify the efficiency of our algorithms. We also conduct online experiments with real workers and compare our approach with various non-adaptive assignment strategies. We find that our approach offers the best compromise between performance dimensions thereby assessing the need for adaptability
Black, Samson 1979. "Representations of Hecke algebras and the Alexander polynomial." Thesis, University of Oregon, 2010. http://hdl.handle.net/1794/10847.
Full textWe study a certain quotient of the Iwahori-Hecke algebra of the symmetric group Sd , called the super Temperley-Lieb algebra STLd. The Alexander polynomial of a braid can be computed via a certain specialization of the Markov trace which descends to STLd. Combining this point of view with Ocneanu's formula for the Markov trace and Young's seminormal form, we deduce a new state-sum formula for the Alexander polynomial. We also give a direct combinatorial proof of this result.
Committee in charge: Arkady Vaintrob, Co-Chairperson, Mathematics Jonathan Brundan, Co-Chairperson, Mathematics; Victor Ostrik, Member, Mathematics; Dev Sinha, Member, Mathematics; Paul van Donkelaar, Outside Member, Human Physiology
Fürst, Oliver [Verfasser]. "Trace-class properties of semi-groups associated with operator valued differential operators and their Witten index / Oliver Fürst." Bonn : Universitäts- und Landesbibliothek Bonn, 2021. http://d-nb.info/1239729677/34.
Full textCARBONARO, DANIELLE P. "Designing a Database and Pilot Testing to Properly Track Food Group Consumption in Overweight/Obese Postpartum Women Enrolled in a Dietary Intervention Study." University of Cincinnati / OhioLINK, 2008. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1218058036.
Full textFrau, Simona. "Fluoro-deoxy-carbohydrates as prosthetic groups for PET imaging : studies towards novel PET tracers for the cannabinoid system and angiogenesis-related receptors." Thesis, University of Aberdeen, 2015. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=225655.
Full textBurgun, Christophe. "Caractérisation et modélisation des besoins énergétiques d'un tracteur agricole : application à l'étude des performances en lien avec les lubrifiants du groupe motopropulseur." Paris 6, 2013. http://www.theses.fr/2013PA066824.
Full textLermen, Raquel Elisa. "Assinaturas icnológicas em depósitos glacigênicos do Grupo Itararé no RS." Universidade do Vale do Rio dos Sinos, 2006. http://www.repositorio.jesuita.org.br/handle/UNISINOS/4247.
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A revisão icnotaxonômica da paleoicnofauna Grupo Itararé no RS revelou a presença de uma icnofauna dominada por trilhas de artrópodes, com impressões de repouso e pistas de deslocamento intraestratal de artrópodes e escavações rasas de organismos vermiformes subordinadas, além de icnofábricas de Chondrites-Planolites-Palaeophycus. Duas novas icnoespécies, Cruziana intermittens n. isp. e Tonganoxichnus itararensis n. isp. foram diagnosticadas. A análise das assembléias icnofossilíferas evidenciou a presença duas paleoicnocenoses distintas: (i) Paleoicnocenose A, contendo trilhas de deslocamento de artrópodes e escavações rasas de artrópodes e de organismos vermiformes, vinculada à fácies de ritmitos; e (ii) Paleoicnocenose B, reunindo exclusivamente escavações mais profundas, vinculada à fácies de depósitos heterolíticos. Quatro suítes distintas são observadas na Paleoicnocenose A: (i) suíte MP, contendo Maculichna varia, Protichnites isp., Diplichnites gouldi e Diplopodichnus biformis, com Kouphichnium isp. subordinado, vinculada aos ritmitos do tipo A; (ii) suíte HT, composta por Helmithoidichnites tenuis e Treptichnus pollardi, com Nereites isp. e Tonganoxichnus itararensis n. isp. subordinados, vinculada com os ritmitos do tipo B; (iii) suíte CR, contendo Cruziana problematica, C. intermittens n. isp., Rusophycus carbonarius e Gluckstadtella cooperi, com H. tenuis subordinado, vinculada aos ritmitos do tipo C; e (iv) suíte Dg, monoespecífica para Diplichnites gouldi, preservada em palimpsesto sobre a suíte CR. A Paleoicnocenose B é formada por icnofábrica composta de Chondrites/Planolites, produzida em níveis intermediários do substrato, e Palaeophycus, em níveis mais superficiais. As assinaturas icnológicas registradas sugerem um sistema deposicional estuarino do tipo fiorde, com a zona mais proximal do estuário situada a ENE (região de Cachoeira do Sul) e a mais distal, a SSW (região ao sul de São Gabriel-sudoeste de Lavras do Sul). Os ritmitos do tipo B se concentrariam na região mais proximal, os ritmitos dos tipos A e C se desenvolveriam nas planícies laterais ao corpo d?água e os depósitos heterolíticos, próximos à desembocadura deste, junto ao mar, em águas salobras. O contexto das paleoicnocenoses A e B e seus vínculos faciológicos sugerem representar, respectivamente, uma Icnofácies Scoyenia atípica e uma Icnofácies Cruziana empobrecida. De acordo com o registro global, a presença de G. cooperi, M. varia, T. pollardi e T. itararensis n. isp. nos ritmitos permitem supor uma idade Carbonífero Superior para esses depósitos.
The ichnotaxonomic review of the trace fossils from Itararé Group (Paraná Basin, south of Brazil) in the Rio Grande do Sul State (southernmost Brazil) showed the presence of an ichnofauna dominated by arthropod trackways. Resting traces and intrastratal trails also made by arthropods and shallow burrows produced by soft-bodied organisms are subordinated, as well as a Chondrites-Planolites-Palaeophycus composite ichnofabic. Two new ichnospecies were diagnosed, Cruziana intermittens n. isp. e Tonganoxichnus itararensis n. isp. Two ichnocoenoses were differenciated: (i) Paleoichnocoenosis A, bearing arthropod trackways, resting traces, intrastratal trails and shallow burrows, related to the rhythmite facies; and (ii) Paleoichnocoenosis B, joining exclusively deeper burrows, related to the heterolithic deposit facies. Four distinct suites were observed in Paleoichnocoenosis A: (i) MP suite, having Maculichna varia, Protichnites isp., Diplichnites gouldi and Diplopodichnus biformis, with Kouphichnium isp. subordinated, and related to the rhythmites type A; (ii) HT suite, composed of Helmithoidichnites tenuis and Treptichnus pollardi, with Nereites isp. and Tonganoxichnus itararensis n. isp. subordinated, related to the rhythmites type B; (iii) CR suite, bearing Cruziana problematica, C. intermittens n. isp., Rusophycus carbonarius and Gluckstadtella cooperi, with H. tenuis subordinated, related to the rhythmites type C; and (iv) Dg suite, monospecific to Diplichnites gouldi, superimposed to the CR suite, in palimpsest preservation. The Paleoichnocoenosis B is formed by a composite ichnofabric of Chondrites and Planolites (deeper tier), and Palaeophycus (shallow tier). The recorded ichnological signatures suggest an estuarine, fjord-like depositional setting, the proximal zone extending to ENE (Cachoeira do Sul region) and the distal zone reaching the SSW (south of São Gabriel-southwest of Lavras do Sul). The rhythmites type B are concentrated in the proximal zone, the rhythmites type A and C, in the marginal plains, lateral to the main body water, and the heterolithic deposits characterize the estuary mouth, opening to the sea, under brackish water conditions. The ichnological and faciological characteristics of the paleoichnocoenoses A and B reveal the existence of an atypical Scoyenia Ichnofaceis and an impoverished Cruziana Ichnofacies, respectively, in the studied deposits. According to the global record, the presence of G. cooperi, M. varia, T. pollardi and T. itararensis n. isp. in the rhythmites allows to infer an Upper Carboniferous (Pennsylvanian) age to these rocks.
Fumes, Regiane Andrade [UNESP]. "Modelagem metamórfica e geotermobarometria de elementos traço em metapelitos e quartzitos: exemplo de Nappe de Luminárias-MG." Universidade Estadual Paulista (UNESP), 2017. http://hdl.handle.net/11449/148605.
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
A Nappe Luminárias corresponde a uma estrutura alongada de orientação NNE-SSW com cerca de 40 km de extensão, situada na porção sul do Orógeno Brasília (idade neoproterozoica), bordejando o Cráton do São Francisco. Tal estrutura é composta majoritariamente por metapelitos e quartzitos do Grupo Carrancas. O presente trabalho foca na caracterização metamórfica de metapelitos e quartzitos do Grupo Carrancas na Nappe Luminárias. Para tal, utiliza-se modelagem metamórfica através de pseudosseções (THERMOCALC), química mineral e os geotermômetros Zr em rutilo e Ti em quartzo. Com base na mineralogia e nas relações texturais e estruturais observadas em lâmina, foram identificadas paragêneses distintas nas porções norte, centro-norte e sul da Nappe Luminárias. Na porção norte, a paragênese é Cld+Chl+Ky+Rt+Qtz+Ms. Na porção centro-norte, ocorre a paragênese St+Grt+Rt+Qtz+Ms, com biotita, clorita e ilmenita retrometamórfica. A assembleia de pico metamórfico registrada nas rochas da porção sul é Grt+Ky+St+Rt+Qtz+Ms com biotita, clorita e ilmenita retrometamórfica. Os resultados indicam a presença de um gradiente metamórfico com condições variando de fácies xisto-verde na porção norte (560˚C e 10kbar) e centro-norte (610˚C e 12,5kbar) a fácies anfibolito / eclogito na porção sul (630˚C e 15kbar). As rochas metapelíticas da Nappe de Luminárias evoluíram através de trajetórias P-T-t horárias, que indicam aquecimento seguido de uma forte descompressão. Análises de elementos traço em grãos de rutilo derivados de quartzito indicam que os mesmos podem ser utilizados para cálculo de temperatura utilizando-se o geotermômetro Zr no rutilo. Todavia, os dados indicam que a homogeneização, ou reequilíbrio, da concentração de Zr em rutilos detríticos em quartzitos ocorre em temperaturas mais elevadas que nos metapelitos, em torno de 580˚C. Não foi observada sillimanita nas rochas estudadas. Estes dados colocam em dúvida a extensão da Zona de Interferência entre as Faixas Brasília e Ribeira até a região de Luminárias. Além disso, os dados de modelagem do presente trabalho mostram que seria necessária descompressão isotérmica de aproximadamente 8 kbar para a cristalização de sillimanita, o que é incompatível com a superposição da Faixa Ribeira sobre a Faixa Brasília, que levaria a um soterramento ainda maior das unidades.
The Luminárias Nappe is a 40 km long, NNE-SSW elongated structure, located in the southern portion of the Neoproterozoic Brasília Orogen, which borders the São Francisco Craton (Minas Gerais, Brazil). It is composed of high aluminium metapelites and quartzites from the Carrancas Group. The present work focuses on the metamorphic characterization of the metapelites and the quartzites of the Luminárias Nappe by means of pseudosection modelling, mineral chemistry and the Zr-in-rutile thermometer. In the northern portion, the paragenesis is Cld + Chl + Ky + Rt + Qtz + Ms. In the center-north portion, the paragenesis is St + Grt + Rt + Qtz + Ms, with retro-metamorphic biotite, chlorite and ilmenite. The metamorphic peak assembly recorded in rocks from the southern portion is Grt + Ky + St + Rt + Qtz + Ms with retro-metamorphic biotite, chlorite and ilmenite. Results indicate the presence of a metamorphic gradient with conditions increasing from green-schist facies in the northern portion (560˚C and 10kbar) and center-north (610˚C and 12,5kbar) to amphibolite / eclogite facies in the southern portion (630˚C and 15kbar). Metapelitic rocks of the Luminárias Nappe followed a clockwise P-T-t path, characterised by an initial heating stage that is followed by strong decompression. Analyses of trace elements in rutile grains derived from quartzite indicate that they can be used for temperature calculation using the geothermometer Zr in rutile. However, the data shows that the homogenisation, or reequilibration, of the Zr content detrital rutile in quartzites occurs at higher temperatures than in the metapelites, at about 580˚C. No sillimanite has not been described in the studied rocks. Therefore, it suggests that the Interference Zone between the Brasília and Ribeira belts does not extent to the Luminárias Nappe region. In addition, our modelling shows that it would be require an isothermal decompression of approximately 8 kbar for the crystallization of sillimanite, which is incompatible with the overlapping of the Ribeira Belt over the Brasilia Belt, which would lead to an even greater burial of the units.
FAPESP: 2015/05230-0
FAPESP: 2015/07750-0
Tokushige, Yuki. "Random Walks on random trees and hyperbolic groups: trace processes on boundaries at infinity and the speed of biased random walks." Kyoto University, 2019. http://hdl.handle.net/2433/242580.
Full textPratscher, Jennifer [Verfasser], and Ralf [Akademischer Betreuer] Conrad. "Investigation of microbial groups involved in the uptake of atmospheric trace gases in upland soils / Jennifer Pratscher. Betreuer: Ralf Conrad." Marburg : Philipps-Universität Marburg, 2011. http://d-nb.info/1013255461/34.
Full textSchwarzenberger, Fabian. "The Integrated Density of States for Operators on Groups." Doctoral thesis, Universitätsbibliothek Chemnitz, 2013. http://nbn-resolving.de/urn:nbn:de:bsz:ch1-qucosa-123241.
Full textFischer, Wolfgang. "Approche expérimentale du fractionnement magmatique et exemples de redistributions hydrothermales des éléments du groupe du platine (EGP)." Phd thesis, Grenoble 1, 1988. http://tel.archives-ouvertes.fr/tel-00691647.
Full textMurisa, Tendai. "An analysis of emerging forms of social organisation and agency in the aftermath of 'fast track' land reform in Zimbabwe." Thesis, Rhodes University, 2010. http://hdl.handle.net/10962/d1003081.
Full textGhasabyan, Levon. "Use of Serpent Monte-Carlo code for development of 3D full-core models of Gen-IV fast-spectrum reactors and preparation of group constants for transiet analyses with PARCS/TRACE coupled system." Thesis, KTH, Fysik, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-118072.
Full textSmilek, Krista R. "Using Ichnology and Sedimentology to Determine Paleoenvironmental and Paleoecological Conditions of a Shallow-Water, Marine Depositional Environment: Case Studies from the Pennsylvanian Ames Limestone and Modern Holothurians." Ohio : Ohio University, 2009. http://www.ohiolink.edu/etd/view.cgi?ohiou1250003072.
Full textDo, Viet Cuong. "Le lemme fondamental métaplectique de Jacquet et Mao." Phd thesis, Université de Lorraine, 2012. http://tel.archives-ouvertes.fr/tel-00821520.
Full textGangloff, Sophie. "Evaluation of the mechanisms of trace elements transport (Pb, Rare Earth Elements,... ) and the elemental and isotopic fractionation (Ca and Sr) at the interface water-soil-plant." Thesis, Strasbourg, 2016. http://www.theses.fr/2016STRAH002/document.
Full textThis work is focused on the study of a profile of soil and soil solutions collected on an experimental plot covered with spruce. All these samples come from the watershed of the Strengbach (environment - OHGE Hydrogeochimique Observatory), were sampled at different depths (5, 10, 30 and 60 cm) and during the period between 2009 and 2013. Characterizations of soil extracts by infrared spectroscopy allowed to highlight changes in the organic functional groups with depth and that these changes have a significant impact on the behaviour of the cations (major and trace) in the soil. Ultrafiltration experiments helped to identify flows of colloidal and dissolved organic carbon as well as those of the major and trace-element present in soil solutions. The joint use of isotope tracers (87Sr / 86Sr and δ44 / 40 Ca) and chemical (Rare Earth Elements) have highlighted processes taking place at the water-soil-plant interface, as the uptake by root or soil alteration
Trommetter, Guillaume. "Développements analytiques et d’échantillonneurs passifs appliqués aux terres rares et platinoïdes : application aux systèmes aquatiques anthropisés." Thesis, Lille 1, 2020. http://www.theses.fr/2020LIL1R051.
Full textAquatic ecosystems are fragile systems, vital for the biosphere and yet subject to numerous, sometimes significant, anthropogenic pressures. Currently, reliable methods allow the quantification and study of the fate of metallic trace elements (Pb, Zn, Cd, etc.) and many organic micropollutants in water and sediments. For other elements such as rare earths or platinum group elements, which are increasingly used by industry, their quantification remains more complex and even uncertain due to their very low concentrations. Their quantification is practically impossible without the use of preconcentration techniques or the development of specific analytical methods to reduce the spectral interferences linked to interferents present in high concentrations in the environment. This research work has allowed (i) to quantify precisely these elements by inductively coupled plasma mass spectrometry combined with the use of a collision/reaction cell by judiciously choosing the gas and its flow applied in the cell ; (ii) to preconcentrate in situ and then determine concentrations ranging from pg L-1 to ng L-1 for platinum group elements, in areas impacted by human activities (road leaching, Pt-based drug releases), by developing passive sampling techniques called "Diffusive Gradients in thin films (DGTs)" based on the use of two different resins, and (iii) to better understand how some of these elements can be used as tracers of urban discharges, particularly in connection with wastewater treatment plants containing domestic and hospital discharges, in addition to the tracers usually used. To this end, the Marque River served as a pilot site for this prospective study during a period of low water levels. These studies made it possible to determine the current concentrations of rare earths and platinum in environments heavily impacted by human activities, making it possible to monitor their evolution and evaluate their potential impact in the future
Vigneron, Francois. "Localisation et décroissance des champs de la mécanique des fluides et des plasmas. Espaces fonctionnels associés à une famille de champs de vecteurs." Phd thesis, Ecole Polytechnique X, 2006. http://tel.archives-ouvertes.fr/tel-00136144.
Full textLa seconde partie est consacrée à l'étude des espaces de Sobolev associés à une famille de champs de vecteurs, de type sous-elliptique. Les principaux résultats sont la description des régularités fractionnaires avec la distance de Carnot, la démonstration d'inégalités de Hardy et, dans le cas du groupe de Heisenberg, la théorie des traces sur une hypersurface caractéristique générique.