Thesis (Masters (Depertment of Economics, Faculty of Economic and Management Sciences.))--University of the Western Cape, 2009. / Includes bibliographical references (leaves 68-72).

Thesis (Ph. D.)--University of Hawaii at Manoa, 2003. / Includes bibliographical references (leaves 97-121).

Thesis (M.A.)--Georgia State University, 2005. / Title from title screen. Sally Wallace, committee chair; L.F. Jameson Boex , James R. Alm, committee members. Electronic text (72 p.) : digital, PDF file. Description based on contents viewed June 26, 2007. Includes bibliographical references (p. 67-70).

Depuis les années 1990, le Mozambique connaît des changements sociopolitiques importants qui se prétendent démocratiques. Ces changements ont constitué un bouleversement de l’environnement du fonctionnement de la police. Depuis lors, la police est objet des réformes dont le but de rendre son organisation et fonctionnement compatibles aux exigences du maintien de l’ordre dans ce nouveau contexte sociopolitique. Toutefois, ces réformes n’ont pas changé profondément les pratiques policières. En effet, la police continue violente malgré les réformes démocratiques qu’elle a bénéficié. Inscrit dans la sociologie d’État et de la Police, cette étude cherche à expliquer ce paradoxe. Elle soutient que la continuité des pratiques policières violentes n’est pas étranger à l’État démocratique en construction au Mozambique. Elle traduit les limites de celui-ci et la conjoncture sociopolitique que le pays traverse depuis la transition démocratique, caractérisée par l’essor de la violence sociale et politique. Le contrôle de cette violence, en plus de freiner les réformes démocratiques de la police, légitime la violence policière comme mécanisme de contrôle social et d’affirmation d’État. / From the year of 1990, Mozambique suffered profound changes which are called as being democratic. These changes constituted a change in the operating environment of the police. Since then, the police have come to be the object of reforms whose goal is to make this organization and operation compatible with the requirements of maintaining order in new socio-political context. However, these reforms did not change profoundly the police practices. Enrolled in the sociology of the State and the Police, the present study seeks to explain this paradox. He argues that the persistence of violent police practices is not contrary to democratic State under construction in Mozambique. It translates the limits of this and socio-political situation that the country has been experiencing since the democratic transition, characterized by the increase of social and political violence. The control of this violence, in addition to brake the democratic reforms of the police, justifies the repression and police violence as a mechanism of social control and of the affirmation of the State.

Thesis (M.A. in National Security Affairs)--Naval Postgraduate School, September 2006. / Thesis Advisor(s): Letitia Lawson, Jessica Piombo. "September 2006." Includes bibliographical references (p. 59-64). Also available in print.

Thesis (M.S.)--Michigan State University. Dept. of Agricultural Economics, 2008. / Title from PDF t.p. (viewed on Aug. 4, 2009) Includes bibliographical references (p. 94-100). Also issued in print.

Thesis (MPhil)--University of Stellenbosch, 2005. / On t.p.: Master of Philosophy in Livestock Industry Management (Aquaculture) Bibliography. Also available via the Internet.

Th. doct.--Géographie humaine--Lisboa--Faculdade de letras da universidade de Lisboa, 1979. / Ouvrage en portugais contenant des traductions en français et en anglais. Bibliogr. p. 525-550.

Akademisk avhandling--Göteborg, 1999.

M.Sc. / The ca. 800 km2 Tete Complex of NW Mozambique is located at the eastern end of the 830 ±30 Ma Zambezi Belt, near the transition zone into the Neoproterozoic Mozambique Belt. The Complex is located just south of the Sanangoe Shear Zone where Mesozoic and Late Palaeozoic cover rocks obscure much of the region. Country rocks immediately in contact with the Tete Complex include amphibolitic gneiss, graphite-bearing marble, calcsilicate gneiss, muscovite and biotite schist and quartzite of the Chidue Group. The Tete Complex may have been intrusive into the Chidue Group, although there is evidence inferring tectonic emplacement. Those few contact exposures that exist are equivocal. Some of the rocks within the Tete Complex have been affected by metamorphism up to amphibolite grade, although large proportions of the rocks retain pristine magmatic mineralogy and texture. The Tete Complex contains mafic, ultramafic and anorthositic rocks, dolerite dykes and minor Fe-Ti oxide-rich rocks that occur as rubble. Pyroxenite occurs as thin (<1-2 m), cumulate layers within gabbroic rocks. Most exposed anorthositic rocks occur in the Nyangoma area in the eastern part of the Tete Complex. The anorthosites and leucotroctolites are massive, coarse grained (2-3 cm), and contain plagioclase (An47-An57) megacrysts up to 10 cm in length, interstitial olivine (Fo59-Fobs) and orthopyroxene (En59- En75, mean A1203 = 1.84 wt.%) rimmed by clinopyroxene (mean = Wo 46En38Fs i6), pyrite and Fe-Ti oxides. Secondary biotite, iddingsite, epidote and green spinet are present. The stable coexistence of olivine and plagioclase limits the depth of emplacement to <7-8 kbar, or <20- 25 km; a relatively shallow level of emplacement is favored by the generally fine grain size of the gabbroic and doleritic rocks. Compositions of coexisting plagioclase and mafic silicates (orthopyroxene and olivine) are similar to those of massif-type anorthosites. Previously unmapped meta-anorthosite occurs along the western and northern margin (within the Sanangoe Shear Zone) of the Tete Complex and has been metamorphosed to amphibolite grade. The rock contains plagioclase (An38-An39), with the more Ab-rich compositions related to the formation of garnet (mean = A1m67GrotsPYI6Sp2). Metamorphic orthopyroxene (Enso-En53), clinopyroxene (mean = Wo37En38Fs25), mizzonitic scapolite (Me63), amphibole, biotite and apatite are present. High Cl contents in amphibole, scapolite and biotite (e.g., up to 4.7 wt. % in amphibole), suggest that a Cl-rich metamorphic fluid infiltrated the western margin of the Tete Complex. Olivine melagabbro from the north-central part of the Tete Complex contains plagioclase (An70-An26), olivine (Fo82-Fos4) and clinopyroxene (mean = WanEn1Fs0.2, mean A1203 = 2.56 wt. %), with primitive compositions compared to those in Nyangoma anorthositic rocks and pyroxenites. Pyroxenites are modally dominated by clinopyroxene (mean = Wo46-48En36-39Fsi3-18) with accessory interstitial plagioclases (Ano-An45) and discrete and exsolved orthopyroxenes (En 56-En75). Clinopyroxenes with high A1203 contents up to 9 wt. % are similar to high-Al pyroxene megacrysts. One sample of pyroxenite contains orthopyroxene (En56-En60) and plagioclase (An40-An45) with more evolved compositions compared to those in Nyangoma anorthositic rocks and olivine melagabbro. Normal Fe4- and Na-enrichment trends accompanying fractionation from magmas that may be common to the Nyangoma anorthositic rocks, pyroxenites and olivine melagabbro, are associated with an increase in Al relative to Cr along a line of nearly constant relative Ti content. Gabbro contains olivine and plagioclase crystals that are commonly zoned, thus ranging widely in composition (Fool -Fos°, Anss-Ans2)• Clinopyroxene (mean = Wo36En47Fsi6) constitutes ca. 34 modal % of gabbro. New whole-rock (Nyangoma anorthosite and leucotroctolite) and mineral (plagioclase, clinopyroxene and orthopyroxene) Sm-Nd isotopic data yields ages between 975 ±33 Ma and 1041 ±131 Ma. The igneous crystallization age of the anorthositic rocks is estimated at 1025 ±79 Ma (9-point whole-rock regression). Rb-Sr isotopic compositions for whole-rock samples reveal no meaningful age relationships. Initial Nd isotopic compositions (calculated at 1.0 Ga) correspond to E Nd values between +3.5 and +4.5 (mean = +4.1) with Is, = 0.70276 — 0.70288 (mean = 0.70282), both inferring magmatic derivation from a depleted mantle source, possibly with little or no contamination by Archaean crustal components. TDM model ages range between 1074 and 1280 Ma (mean = 1148 Ma). There is a striking similarity between the Tete Complex anorthosites and those of SW Madagascar in terms of Nd isotopic compositions and the nature of country rocks; in both regions the anorthosites were emplaced either magmatically or tectonically into shelf-type supracrustal metasediments (marbles, quartzites, graphitic schists, etc.). Anorthosites intruded similar country rocks in Draining Maud Land, eastern Antarctica. Although anorthosites from Mozambique and Madagascar share a common depleted mantle signature with little or no contamination by Archaean crustal components, a direct stratigraphic correlation between these two areas (and possibly eastern Antarctica), awaits further geological and geochronological data.