Thesis (M.S.)--University of North Texas, May, 2007. / Title from title page display. Includes bibliographical references.

Chapter 1 is an introduction to the Malagasy language and gives a historical background of how the notion of accent was introduced in the description of Malagasy phonology. Chapter 2 deals with Malagasy words, their formation, their accent patterns and the rules which have been so far claimed to govern the accent patterns and the accent shift in Malagasy. New explanations are given concerning the stress shift in native Malagasy words as well as in loan words. Chapter 3 covers a series of experiments on the judgment of accent (in words and in sentences) conducted by the present author on different groups of listeners namely, linguistically trained and untrained speakers of different Malagasy dialects and Malagasy speakers' judgment of accent in a foreign language (Welsh-English). Acoustic measurements of accent as judged by the informants are reported in Chapter 4 and evaluated statistically. Chapter 5 discusses a previous theory of the Malagasy accent based on syntax. Evidence is given against such a theory. A new theory is given in chapter 6, according to which accent in Malagasy is determined by intonation. Semantics seem to play a major role in delimiting intonation-groups.

The results of a survey on the relative abundance of sulfur isotopes are presented, together with a review of previous work on the same subject. The possible causes of the variations found, and the biological and geological significance of these varia­tions is discussed. In addition, the equilibrium constant for the isotopic exchange between hydrogen sulfide and hydro­sulfide solution is determined experimentally and the results related to theoretical cal­culations based on partition functions. / Thesis / Master of Science (MS)

This diploma thesis is devoted to the investigation methodology of murders. The main emphasis is given to the procedure of the police authority within the investigation of murders. Since this topic is very extensive and the methodology comprises of the great amount of activities, I dedicate this diploma thesis only to the selected areas thereof. The first chapter describes the specification of the crimes against life, in particular legal regulation and related aspects. I focused on the legal regulation in Czech law with respect to a crime of murder, homicide and murder of a new born by its mother. Only marginal attention is given to a crime of negligent manslaughter and a crime of assisting with suicide. The second chapter comprises of the statistics of the committed murders. I analyse the statistics of the numbers of murders committed within the European Union, the Czech Republic and the Ústí region. Another part of the thesis is theoretically orientated. I concentrate on the criminalistics characteristic of a murder and the fundamental aspects thereof - the mode of committing a crime, the personality of a murderer, the personality of a victim and a criminal motive. The following chapter forms the crucial part the diploma thesis in which I analyse typical investigation situations, in particular in...

in English The topic of the thesis is the " The Methodology of Investigation of Murders (selected issues)". The topic is too broad for the limited capacity of the dissertation. While writing the thesis, after the necessary theoretical introduction (which contains the definition of crimes against life, medical definition of death, etc.), I focused only on the initial stage of the investigation of the crime of murder. I specifically focused on the discovery of the body, on securing the crime scene, on autopsy and on the demarcation of investigative versions. Next stage of the investigation is only briefly summarized in the ninth chapter. The thesis is divided into ten chapters. The first chapter explains basic terms, especially murder, murder of a newborn baby by its mother and other crimes against life, such as manslaughter, negligent homicide and assistance to suicide. This chapter also includes medical definition of death, and a brief description of the post-mortem changes. The second chapter consists of brief statistics on the number of murders in the Czech Republic between the periods 2000 to 2012. It contains two graphs; the first graph shows the evolution of the total number of murders each year and their solving. The second graph divides murders according to the specific motives. The third...

Les nouvelles technologies sont de plus en plus utilisées pour la commission des infractions, soit en facilitant la commission de celles-ci, soit elles en sont directement l'objet. Si des dispositions visant à réprimer certains comportements sont apparus dès 1978 avec la Loi dit CNIL, Le législateur n’a pris en compte que tardivement des mesures permettant de faciliter la répression de celles-ci ou de faciliter les actes liés à l'exercice de la police judiciaire. Il s'agit d'un domaine en perpétuel évolution qu'il est difficile d'appréhender surtout lorsqu'il faut allier les obligations juridiques et les impératifs techniques. En effet contrairement à des traces ou indices qui peuvent être appréhendés physiquement sur une scène d’infraction, les données numériques sont quant à elle immatérielles.Elles peuvent être contenues dans un support physique, ou tout simplement être en mouvement sur les réseaux. Si ces données contrairement à toute autre trace peuvent être répliquées à volonté, elles restent extrêmement volatiles si elles ne sont pas recueillies dans des conditions optimales destinées à assurer leur intégrité.Cette thèse a pour objet de faire la démonstration des difficultés d’applicabilité de la procédure pénale au regard des nouvelles technologies notamment au travers du régime des constatations policières sur les supports de stockage et les réseaux numériques.Ce travail de recherche scientifique aborde le principe et le recueil de la preuve numérique sur un support physique et sur les réseaux, mais également la distinction entre les actes techniques et l’expertise aussi bien dans le cadre de l’enquête de Police que dans la phase de l’instruction préparatoire. / New technologies are increasingly being used in the commission of offenses (Felonies and other Violations) either by facilitating the commission or they are directly the vector. If provisions to punish certain behaviors emerged in 1978 with the CNIL said Act, the legislature has considered only late measures to facilitate the prosecution of them to facilitate acts involving the exercise of Law Enforcement investigations.Since it is an area in constant evolution, it is difficult to understand especially when it is necessary to combine the legal obligations and technical requirements. Indeed, unlike traces or clues that can be seized physically on a crime scene, the digital data is in turn intangible.They may be contained in a physical support, or simply be moving over networks. If this data unlike any other track can be infinitely replicated at will, they remain extremely volatile if they are not collected under optimal conditions to ensure their integrity.This thesis aims to demonstrate the difficulties of applicability of the criminal proceedings in relation to new technologies, particularly through the system of Law Enforcement findings on storage media and digital networks.This scientific research addresses the principle and collection process of digital evidence on physical media and networks. It also addresses the distinction between technical tasks and the technical expertise as well as the preliminary phase of the Law Enforcement investigation and the phase being handled by the examining magistrate (judge).

Thesis of (M.A.)--University of Alberta, 2009. / Title from pdf file main screen (viewed on August 31, 2009). "Fall, 2009." At head of title: University of Alberta. A thesis submitted to the Faculty of Graduates Studies and Research in partial fulfillment of the requirements for the degree of Master of Arts, Department of Sociology, University of Alberta. Includes bibliographical references.

Thesis (M.Soc.Sc.)--University of Hong Kong, 2002. / Includes bibliographical references (leaves 75-82) Also available in print.

This study comprises a petrographical and mineralogical investigation of rocks from an area 850 sq. km in size, situated about 80km northeast of Middelburg. Roughly half of the area is occupied by rocks of the epicrustal phase of the Bushveld Complex, and consists largely of Rooiberg Felsite and granophyre as well as leptite, microgranite and granodiorite. Numerous veins of finegrained granite traverse the leptite which is considered to be highly metamorphosed felsite. These veins of fine-grained granite probably owe their origin to the melting of the leptite. The coalescence of these products of melting gave rise to the thick sheet of.granophyre between the leptite and the felsite. Rocks of the Layered Sequence occupy the eastern half of the area and consist of the Main and Upper Zones which were subdivided into various subzones on the basis of characteristic rock types and marker horizons. Mineralogical investigations are restricted to the minerals from rocks of the Layered Sequence, namely orthopyroxene, plagioclase, apatite and the sulphides of the Upper Zone. In Subzone A of the Main Zone, the orthopyroxene is present as cumulus crystals, but it changes in texture to ophitic in the lower half of Subzone B where small discrete grains of inverted pigeonite are also developed. Inverted pigeonite is present in the upper half of Subzone B and in rocks of the Upper Zone, whereas the orthopyroxene-pigeonite relationships in Subzone C of the Main Zone are a repetition of those observed in the underlying rocks. The phase-change from orthopyroxene to pigeonite takes place over a transition zone in which both phases crystallized from the magma. It is envisaged that the first pigeonite to have crystallized from the magma at high temperatures had a lower Fe/Mg ratio than the hypersthene precipitating at slightly lower temperatures, with the result that the early formed pigeonite was unstable and reacted with the magma to form hypersthene. This caused the formation of groups of grains of hypersthene which are optically continuous over large areas and which may contain a few blebs of augite exsolved from the original pigeonite. A few pigeonite grains were effectively trapped in other minerals, mostly augite, and consequently escaped reaction with the liquid. These inverted to hypersthene at the appropriate temperature and contain numerous exsolution-lamellae of augite. As fractional crystallization of the magma continued, it moved further into the stability field of pigeonite and out of the stability field of hypersthene with the result that the formation of hypersthene by the reaction of pigeonite with magma was replaced by inversion of pigeonite to hypersthene. This inverted pigeonite is also present as groups of grains optically continuous and contains pre-inversion exsolution-lamellae of augite orientated at random, and post-inversion exsolution-lamellae which are orientated parallel to the (100) plane of the orthopyroxene throughout a unit. The inverted pigeonite is orientated in such a way that its crystallographic c-axis lies close to or in the plane of layering. This is explained as being due to the load pressure of the superincumbent crystal mass during the inversion. Textural features of the plagioclase revealed interesting information on the postcumulus changes in the rock. Reversed zoning, interpenetration and bending of plagioclase crystals as well as the presence of myrmekite are described. These are considered to be due to increased load pressure prior to and during crystallization of the intercumulus liquid. It is considered that the various types of pegmatoids may have originated by an increase in pressure on the intercumulus liquid which was concentrated to form pipe-like bodies by lateral secretion or filter pressing. Cumulus apatite is developed in the olivine diorites of Subzone D of the Upper Zone. From unit cell dimensions it seems as if it changes in composition from a fluor-rich hydroxyapatite at the base of this subzone to a relatively pure hydroxyapatite 70m below the roof. There seems to be a substantial increase in the fluor content of the apatite in the topmost 70m of the intrusion. Rocks of the Upper Zone contain considerably more sulphides than those of the Main Zone. This is ascribed to an increase in the sulphur content of the magma owing to fractional crystallization. The magma reached the saturation point of sulphur when rocks of Subzone D of the Upper Zone started to crystallize with the result that these rocks contain numerous small droplets of sulphide which constitute on an average about 0, 5 per cent by volume of the rocks. A concentration of the sulphides in these rocks would not yield a deposit of economic interest because of the unfavourable composition of the sulphide phase, which consits of more than 90 per cent pyrrhotite. Sulphides in the rocks below this subzone are intercumulus and a concentration could be of economic importance because the sulphide phase contains appreciable amounts of chalcopyrite and pentlandite. Although no economic concentration of sulphides are known from the Upper Zone, this study has revealed the presence of a mineralized anorthosite below Lower Magnetitite Seam 2 which contains in places up to 1 per cent Cu, 0, 18 per cent Ni and 1, 6g/ton platinum metals. Continuous, slow convection and bottom crystallization probably gave rise to the homogeneous rocks of the Main Zone. Injection of a considerable amount of fresh magma took place at the level of the Pyroxenite Marker which resulted in a compositional break and gave rise to a repetition in Subzone C of the rocks of the Main Zone below this marker. The oxygen pressure during crystallization of the magma was probably low, causing a gradual enrichment in iron in the magma and gave rise to the appearance of magnetite at the base of the Upper Zone. Intermittent increase in the oxygen fugacity is considered to be important in the formation of magnetitite seams. As a result of fractional crystallization the volatile content of the remaining magma gradually increased. This is seen firstly, by the appearance of biotite secondly by the appearance of cumulus apatite and droplets of sulphide and lastly by hornblende in the rocks of the Upper Zone. Some water-rich residual liquids apparently also intruded the overlying leptite, causing additional melting of the latter and the formation of irregularly shaped veins and pockets of granodiorite. A lateral change in facies of the rocks of the Layered Sequence in a southerly direction is described. This is considered to be due to crystallization of the magma at slightly lower temperatures because of the more effective heat loss where the magma chamber was thinner. Two parameters of differentiation for layered intrusions are proposed, viz. a modified version of the differentiation index and a modified version of the crystallization index. The former seems more applicable for intrusions such as the Bushveld Complex, whereas the latter seems to be more applicable for intrusions in which there is a considerable development of ultramafic rocks. These two parameters can also be used to indicate the differentiation trend if they are plotted against height in the intrusion. / Thesis (DSc)--University of Pretoria, 2012. / Geography, Geoinformatics and Meteorology / Unrestricted

This study enhances student acceptance of career investigation and contains extensive lesson plans for each day of the school year, plus one copy of each handout to be duplicated. The classroom is run as a business where students work for the instructor and are paid by check at the end of each week. Money is deposited on account and used to purchase course grades. The more money the student earns, the higher grade he can purchase. The findings show that students learn more about careers. Students became aware that the higher paying career fields required more schooling and/or training, resulting in changed attitudes about school. They were able to see how the relationship of the learning process could determine their future.