Thesis--Georg-August Universität, Göttingen.

Inaug.-Diss.--Basel. / Vita. Description based on print version record. Bibliography: p. 153-154.

Inaug.-Diss.--Berlin. / Lebenslauf. "Mozarts opern in der Gesamtausgabe": p. 78. "Literatur": p. 79.

Thesis (D.M.A.)--Ohio State University, 1980. / Includes bibliographical references (leaves 121-123). Available online via OhioLINK's ETD Center.

Texte remanié de: Thesis--Leeds, 1990. / Bibliogr. p. 401-407. Index.

No description available.

Submitted by Daniella Sodre (daniella.sodre@ufpe.br) on 2015-03-09T13:43:22Z No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) Dissertacao JFBN.pdf: 5041452 bytes, checksum: abf0f91890177ce9882a83feb5ed8827 (MD5) / Made available in DSpace on 2015-03-09T13:43:22Z (GMT). No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) Dissertacao JFBN.pdf: 5041452 bytes, checksum: abf0f91890177ce9882a83feb5ed8827 (MD5) Previous issue date: 2012-12-17 / A indústria dos jogos digitais (games) vem superando o faturamento da indústria do cinema desde 2007. Atualmente, jogar faz parte da rotina de muitos brasileiros, especialmente dos jovens. Tal fato também é reflexo do aumento da qualidade dos recursos de tecnologia de informação e comunicação nos últimos anos. As transformações ocorridas nos meios de comunicação têm acarretado uma série de mudanças no âmbito da educação, haja vista a utilização de mídias digitais, as quais se tornaram uma realidade bem comum para a maioria das escolas brasileiras. . Além disso, dispositivos móveis estão cada vez mais acessíveis à população. Este trabalho investiga a utilização de jogos educativos digitais na educação. Este trabalho foi iniciado com uma pesquisa sobre a utilização de jogos na educação. Após estudos, foi desenvolvida metodologia para desenvolvimento de jogos educativos, a qual também define uma integração com ambientes virtuais de aprendizagem. Como prova de conceito, foi criado um jogo educacional desenvolvido para dispositivos móveis na plataforma Android, integrado com ambientes virtuais de aprendizagem, o qual foi desenvolvido reproduzindo fielmente a metodologia proposta. A integração foi feita por meio de um componente de comunicação, facilitando a troca de informações entre jogos e ambientes de aprendizagem, de modo a proporcionar maior independência do aluno. Ao final do desenvolvimento do protótipo executável foi realizada uma avaliação em duas partes: testes com especialistas na área pedagógica e uma avaliação em um contexto real de ensino.

Made available in DSpace on 2014-06-12T15:56:10Z (GMT). No. of bitstreams: 2 arquivo2752_1.pdf: 4894183 bytes, checksum: 84bd88480a7114d246679f1d39a7acf2 (MD5) license.txt: 1748 bytes, checksum: 8a4605be74aa9ea9d79846c1fba20a33 (MD5) Previous issue date: 2010 / Com a crescente sofisticação dos ambientes virtuais de aprendizagem, a aprendizagem online tem à sua disposição recursos que proporcionam um ensino com mais eficácia. É importante ressaltar, que as atividades de colaboração podem ser ampliadas nos ambientes virtuais de aprendizagem, desde que, os elementos de percepção social estejam dispostos e permitam os participantes compartilharem saberes e experiências. A utilização e familiarização de ferramentas tecnológicas, que permitam explorar oportunidades para a colaboração e engajamento dos participantes de diversas formas, conduzem ao aprendizado coletivo. Além, de motivarem a prática das suas habilidades e competências, e de permitirem à re-elaboração e construção conjunta de novos conhecimentos. O presente trabalho tem como objetivo estabelecer requisitos relacionados aos fenômenos de percepção social e de colaboração no LMS Amadeus. Esta pesquisa teve caráter exploratório com abordagem qualitativa. O procedimento metodológico aplicado neste trabalho consistiu na interação com o ambiente, aplicação de questionários, realização de grupo focal, gravação em vídeo e observação. Os participantes são alunos do último ano do curso técnico do IFPE Campus Belo Jardim. Foram identificadas necessidades e os resultados obtidos sinalizam que as funcionalidades dos elementos de percepção social do LMS Amadeus, precisam ser complementadas, e que outros elementos necessitam ser integrados

The problem of how to perform the early Classical keyboard slur has prompted perplexity and dissension in generations of thoughtful performers and teachers. While the mandatory legato indicated by the slur is unquestioned, diversity of opinion centers around the performance of the last note of the slur, specifically regarding its length. Modern pedagogy has generally followed a time-honoured principle of an early release for the last note of a slur, yet many artists seem to disregard this guidance at will. This study attempts to clarify the issue by examining several treatises of the early Classical period. A brief history of the slur is included because its origins undoubtedly influenced how it was later performed. Most of the research, however, focuses on relevant material found in three treatises written by contemporaries of Wolfgang Mozart, namely, CPE. Bach, Daniel Turk, and Mozart's father, Leopold. The three components of the slur—the first note, the notes under the slur, and the last note are treated in turn by presenting information found in the treatises and providing interpretative commentary. This information is then applied to slurs found in the keyboard sonatas of Wolfgang Mozart. Unfortunately, treatises provide no definitive answer to the question of the performance of the last note of a slur. This lacuna is most likely due to the daunting task of describing the many musical circumstances involved in performing the last note under a slur. Solutions to the problem, therefore, cannot simply be founded solely on treatise instructions regarding the slur. Fortunately, the wealth of descriptive writing on the general art of effective music-making also provides some important clues to understanding the principles of performing the last note under a slur. Much of this study focuses on understanding the three important factors influencing the slur's ending: formal structure, Classical violin bowing technique and, most important, the musical context in which a slur is found. When these three aspects of performance are understood, much of the uncertainty surrounding Wolfgang Mozart's slurs will disappear. / Arts, Faculty of / Music, School of / Graduate

The Arumbera Sandstone forms distinctive strike ridges with dark reddish slopes and orange-white cliffs throughout most of the northeastern Amadeus Basin. It is divisible into four readily mappable informal units. The ridge-forming units, 2 and 4, are divided into three and two subunits, respectively. Unit 1, Subunit 2b, Unit 3 and Subunit 4b are generally comprised of recessive, pale-red to grayish-red, medium- to thin-bedded, fineto medium-grained arkose with major proportions of siltstone and mudshale. These sedimentary bodies are interpreted as a complex system of coastal to nearshore-marine environments including tidal flats, tidal channels, estuaries and beaches. Evidence includes: (1) predominance of alpha-, beta, and cross-stratification with common herringbone laminae, truncated wave-ripple laminae, and flaser bedding; (2) bimodal paleocurrents; (3) records of intermittent, subaerial exposure (desiccation mudcracks, raindrop prints, and casts of gypsum and halite crystals); and (4) rare to abundant trace fossils of probable marine origin. Subunits 2a and 4a are comprised of cliff-forming, white to pinkish-gray, thick-bedded, fine- to medium-grained lithic arkose and arkose. Subunit 2c is also resistant, and is comprised of "maroon" to moderate-red, thick-bedded conglomerate and conglomeratic sandstone with pebbles and small cobbles of chert, quartzite, and vein quartz. These three subunits are interpreted as fluvial sheet sandstones on the basis of: (1) predominance of pi-, omikron-, and lambda cross-stratification; (2) thick bedding and paucity of mudrocks; (3) unimodal, northeastward-oriented paleocurrents with a crude radiating pattern; (4) abundant shale pebbles and wedging channelsand bodies; (5) absence or rarity of trace fossils in the subunits; and (6) sheet-like geometry. The Arumbera Sandstone was probably deposited in a coastal environment perhaps analogous to the delta of modern Godavari River of India. Evidence includes: (1) a pronounced depocenter for the unit in the central part of the study area (1123 m relative to 216 m in the southwest); (2) unidirectional paleocurrents from fluvial sheet sands that radiate to the N, NE, E, and SE; (3) fluvial and coastal deposits in vertical, cyclic succession; and (4) east- and northeast-trending zones of thicker deposits within fluvial sheet sands, which may be distributary lobes. The Arumbera is considered part of the molasse sequence associated with the Late Proterozoic and Early Cambrian Petermann Ranges orogeny. The uplifted Petermann Ranges shed sediment from sedimentary, metamorphic, and plutonic rocks. Terrigenous material was probably transported to the coastal environment of the northeastern Amadeus Basin by braided streams in an environment devoid of vascular terrestrial vegetation. Grain mineralogy and weathering characteristics suggest a hot, semiarid to humid climate throughout this region. Detailed petrographic study of ten thin sections demonstrates the following average sandstone composition: quartz (54%), orthoclase (25%), chert (6%), plagioclase (5%), lithics (4%), microcline (2%), and minor zircon, tourmaline, rutile, magnetite, muscovite, and biotite. Common cementing agents are syntaxial quartz and feldspar overgrowths, chert, hematite, kaolinite, and carbonate. The inferred diagentic sequence is : Eogenetic: (1) mechanical compaction and (2) formation of "dust rims"; Mesogenetic: (3) syntaxial feldspar overgrowths, (4) syntaxial quartz overgrowths, (5) calcite cement, (6) organic maturation(?) and creation of secondary porosity, and (7) pyrite crystals; T elogenetic: (8) kaolinite, and (9) chert. The Arumbera is regarded as of possible Late Proterozoic and probable Early Cambrian age based on the presence of the trace fossils Rangea cf. longea and Phycodes antecedens in Unit 1, Arumberia banksi in Subunit 2b, and Bergauria, Diplichnites, Laevicyclus, Phycodes pedum, Plagiogmus, Psammichnites, Rusophycus and Skolithos in Units 3 and 4. The Arumbera is a potential petroleum reservoir. Suitable source rocks, sealing mechanisms, reservoir porosity and permeability, and stratigraphic and structural traps are present in the northeastern Amadeus Basin. The close association of organic maturation with generation of secondary porosity and tectonic fracturing, both in time and space, also favors the accumulation of petroleum in the Arumbera.