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Universites et colleges --- Ecoles --- Emplacement --- Emplacement --- Universites et colleges --- Ecoles --- Emplacement --- Emplacement
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In Stambeli, Richard C. Jankowsky presents a vivid ethnographic account of the healing trance music created by the descendants of sub-Saharan slaves brought to Tunisia during the eighteenth and nineteenth centuries. Stambeli music calls upon an elaborate pantheon of sub-Saharan spirits and North African Muslim saints to heal humans through ritualized trance. Based on nearly two years of participation in the musical, ritual, and social worlds of stambeli musicians, Jankowsky’s study explores the way the music evokes the cross-cultural, migratory past of its originators and their encounters with the Arab-Islamic world in which they found themselves. Stambeli, Jankowsky avers, is thoroughly marked by a sense of otherness—the healing spirits, the founding musicians, and the instruments mostly come from outside Tunisia—which creates a unique space for profoundly meaningful interactions between sub-Saharan and North African people, beliefs, histories, and aesthetics. Part ethnography, part history of the complex relationship between Tunisia’s Arab and sub-Saharan populations, Stambeli will be welcomed by scholars and students of ethnomusicology, anthropology, African studies, and religion.
Spirit possession --- Black people --- Music --- Sṭambālī (Rite) --- Rites and ceremonies. --- History and criticism. --- Religious aspects. --- music, musical studies, trance, tunisia, tunisian, ethnography, ethnographic research, healing trances, sub-saharan, north africa, muslims, religion, religious study, faith, islam, ritualized, ritualization, social worlds, migration, migratory, otherness, spirits, instruments, cultural, culture, aesthetics, history, historical, arab, rites, ceremony, possession, slave trade, slavery, movement, pilgrimage, vocality, displacement, emplacement.
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This Special Issue comprises 12 papers from authors in 10 countries with new insights on the close coupling between magma as an energy and fluid source with hydrothermal systems for the primary control of magmatic behavior. Data and interpretation are provided on the rise of magma through a hydrothermal system, the relative timing of magmatic and hydrothermal events, the temporal evolution of supercritical aqueous fluids associated with ore formation, the magmatic and meteoric contributions of water to the systems, the big picture for the highly active Krafla Caldera, Iceland, as well as the implications of results from drilling at Krafla concerning the magma–hydrothermal boundary. Some of the more provocative concepts are that magma can intrude a hydrothermal system silently, that coplanar and coeval seismic events signal “magma fracking” beneath active volcanoes, that intrusive accumulations may far outlast volcanism, that arid climate favors formation of large magma chambers, and that even relatively dry rhyolite magma can rapidly convect and so lack a crystallizing mush roof. A shared theme is that hydrothermal and magmatic reservoirs need to be treated as a single system.
Research & information: general --- la soufrière --- guadeloupe --- volcanic gas --- volcanic unrest --- hydrothermal gas --- multigas --- extensometry --- Krafla volcano --- geothermal systems --- conceptual models --- volcanology --- magma --- hydrothermal --- fracking --- volcanoes --- Kamchatka --- igneous petrology --- tectonics --- heat flow --- glaciation --- climate --- incremental pluton emplacement --- contact metamorphism --- petrochronology --- titanite --- zircon --- U-Pb dating --- thermometry --- hydrothermal fluids --- incremental intrusion --- hydrothermal fluid --- microstructure --- dissolution --- precipitation --- textural coarsening --- alteration --- porosity --- eruption --- fracture --- permeability --- dome emplacement --- hydrothermal system --- RSAM --- tremor --- gliding spectral lines --- White Island --- phreatic eruptions --- geyser --- Uzon --- CO2 --- TOUGH2 --- modeling --- Kirishima volcano group --- Ebinokogen Ioyama volcano --- geothermal activity --- multiple hydrothermal system --- magmatic hydrothermal eruption --- kick upwelling --- Erdenet Cu–Mo deposit --- cathodoluminescence --- supercritical fluid --- transient fluid pressure --- magmatic-hydrothermal system --- fluid inclusion --- magma energy --- magma convection --- heat flux --- geothermal energy --- magma–hydrothermal --- heat transport --- gas and fluid geochemistry --- phreatic eruption --- volcano monitoring --- geophysical imaging --- drilling
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This Special Issue comprises 12 papers from authors in 10 countries with new insights on the close coupling between magma as an energy and fluid source with hydrothermal systems for the primary control of magmatic behavior. Data and interpretation are provided on the rise of magma through a hydrothermal system, the relative timing of magmatic and hydrothermal events, the temporal evolution of supercritical aqueous fluids associated with ore formation, the magmatic and meteoric contributions of water to the systems, the big picture for the highly active Krafla Caldera, Iceland, as well as the implications of results from drilling at Krafla concerning the magma–hydrothermal boundary. Some of the more provocative concepts are that magma can intrude a hydrothermal system silently, that coplanar and coeval seismic events signal “magma fracking” beneath active volcanoes, that intrusive accumulations may far outlast volcanism, that arid climate favors formation of large magma chambers, and that even relatively dry rhyolite magma can rapidly convect and so lack a crystallizing mush roof. A shared theme is that hydrothermal and magmatic reservoirs need to be treated as a single system.
la soufrière --- guadeloupe --- volcanic gas --- volcanic unrest --- hydrothermal gas --- multigas --- extensometry --- Krafla volcano --- geothermal systems --- conceptual models --- volcanology --- magma --- hydrothermal --- fracking --- volcanoes --- Kamchatka --- igneous petrology --- tectonics --- heat flow --- glaciation --- climate --- incremental pluton emplacement --- contact metamorphism --- petrochronology --- titanite --- zircon --- U-Pb dating --- thermometry --- hydrothermal fluids --- incremental intrusion --- hydrothermal fluid --- microstructure --- dissolution --- precipitation --- textural coarsening --- alteration --- porosity --- eruption --- fracture --- permeability --- dome emplacement --- hydrothermal system --- RSAM --- tremor --- gliding spectral lines --- White Island --- phreatic eruptions --- geyser --- Uzon --- CO2 --- TOUGH2 --- modeling --- Kirishima volcano group --- Ebinokogen Ioyama volcano --- geothermal activity --- multiple hydrothermal system --- magmatic hydrothermal eruption --- kick upwelling --- Erdenet Cu–Mo deposit --- cathodoluminescence --- supercritical fluid --- transient fluid pressure --- magmatic-hydrothermal system --- fluid inclusion --- magma energy --- magma convection --- heat flux --- geothermal energy --- magma–hydrothermal --- heat transport --- gas and fluid geochemistry --- phreatic eruption --- volcano monitoring --- geophysical imaging --- drilling
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This Special Issue comprises 12 papers from authors in 10 countries with new insights on the close coupling between magma as an energy and fluid source with hydrothermal systems for the primary control of magmatic behavior. Data and interpretation are provided on the rise of magma through a hydrothermal system, the relative timing of magmatic and hydrothermal events, the temporal evolution of supercritical aqueous fluids associated with ore formation, the magmatic and meteoric contributions of water to the systems, the big picture for the highly active Krafla Caldera, Iceland, as well as the implications of results from drilling at Krafla concerning the magma–hydrothermal boundary. Some of the more provocative concepts are that magma can intrude a hydrothermal system silently, that coplanar and coeval seismic events signal “magma fracking” beneath active volcanoes, that intrusive accumulations may far outlast volcanism, that arid climate favors formation of large magma chambers, and that even relatively dry rhyolite magma can rapidly convect and so lack a crystallizing mush roof. A shared theme is that hydrothermal and magmatic reservoirs need to be treated as a single system.
Research & information: general --- la soufrière --- guadeloupe --- volcanic gas --- volcanic unrest --- hydrothermal gas --- multigas --- extensometry --- Krafla volcano --- geothermal systems --- conceptual models --- volcanology --- magma --- hydrothermal --- fracking --- volcanoes --- Kamchatka --- igneous petrology --- tectonics --- heat flow --- glaciation --- climate --- incremental pluton emplacement --- contact metamorphism --- petrochronology --- titanite --- zircon --- U-Pb dating --- thermometry --- hydrothermal fluids --- incremental intrusion --- hydrothermal fluid --- microstructure --- dissolution --- precipitation --- textural coarsening --- alteration --- porosity --- eruption --- fracture --- permeability --- dome emplacement --- hydrothermal system --- RSAM --- tremor --- gliding spectral lines --- White Island --- phreatic eruptions --- geyser --- Uzon --- CO2 --- TOUGH2 --- modeling --- Kirishima volcano group --- Ebinokogen Ioyama volcano --- geothermal activity --- multiple hydrothermal system --- magmatic hydrothermal eruption --- kick upwelling --- Erdenet Cu–Mo deposit --- cathodoluminescence --- supercritical fluid --- transient fluid pressure --- magmatic-hydrothermal system --- fluid inclusion --- magma energy --- magma convection --- heat flux --- geothermal energy --- magma–hydrothermal --- heat transport --- gas and fluid geochemistry --- phreatic eruption --- volcano monitoring --- geophysical imaging --- drilling --- la soufrière --- guadeloupe --- volcanic gas --- volcanic unrest --- hydrothermal gas --- multigas --- extensometry --- Krafla volcano --- geothermal systems --- conceptual models --- volcanology --- magma --- hydrothermal --- fracking --- volcanoes --- Kamchatka --- igneous petrology --- tectonics --- heat flow --- glaciation --- climate --- incremental pluton emplacement --- contact metamorphism --- petrochronology --- titanite --- zircon --- U-Pb dating --- thermometry --- hydrothermal fluids --- incremental intrusion --- hydrothermal fluid --- microstructure --- dissolution --- precipitation --- textural coarsening --- alteration --- porosity --- eruption --- fracture --- permeability --- dome emplacement --- hydrothermal system --- RSAM --- tremor --- gliding spectral lines --- White Island --- phreatic eruptions --- geyser --- Uzon --- CO2 --- TOUGH2 --- modeling --- Kirishima volcano group --- Ebinokogen Ioyama volcano --- geothermal activity --- multiple hydrothermal system --- magmatic hydrothermal eruption --- kick upwelling --- Erdenet Cu–Mo deposit --- cathodoluminescence --- supercritical fluid --- transient fluid pressure --- magmatic-hydrothermal system --- fluid inclusion --- magma energy --- magma convection --- heat flux --- geothermal energy --- magma–hydrothermal --- heat transport --- gas and fluid geochemistry --- phreatic eruption --- volcano monitoring --- geophysical imaging --- drilling
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Grandes oubliées durant près de quinze ans, les bibliothèques universitaires sont aujourd'hui à nouveau considérées comme l'un des maillons essentiels de l'acquisition des connaissances et comme l'un des lieux majeurs et fédérateurs de l'université. Intégrées dans le plan de développement de l'enseignement supérieur (shéma Université 2000) elles font l'objet de nombreux projets : rénovations, extensions, constructions nouvelles. cet ouvrage constitue le premier guide traitant de tous les aspects d'un projet de bibliothèque universitaire : définition des publics, connaissance des partenaires, développement d'une méthodologie, programmation des espaces, fonctionnalité et qualité architecturale.
Library sites --- Architecture des bibliothèques --- Emplacement --- Utilisation de l'espace --- Architecture as Topic --- -Library architecture --- Architecture des bibliothèques --- Academic libraries --- Library architecture --- 020 --- AA / International- internationaal --- 022 --- 027.71 --- 027.71 Universiteitsbibliotheken --- Universiteitsbibliotheken --- 022 Bibliotheekgebouwen. Bibliotheekinrichting --- Bibliotheekgebouwen. Bibliotheekinrichting --- Architecture --- College libraries --- Libraries, University and college --- University libraries --- Libraries --- Libraries and colleges --- Public libraries --- Bibliotheekwezen: algemeenheden --- Services to colleges and universities --- Library planning and design --- Bibliothèques universitaires --- Bibliothèques --- Buildings --- Space utilization --- Constructions --- Bibliothèque --- Bibliotheques (edifices) --- Bibliotheques universitaires --- Bibliothèques universitaires --- Conception et construction --- France
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In Mock Classicism Nilo Couret presents an alternate history of Latin American cinema that traces the popularity and cultural significance of film comedies as responses to modernization and the forerunners to a more explicitly political New Latin American Cinema of the 1960s. By examining the linguistic play of comedians such as Cantinflas, Oscarito and Grande Otelo, Niní Marshall, and Luis Sandrini, the author demonstrates aspects of Latin American comedy that operate via embodiment on one hand and spatiotemporal emplacement on the other. Taken together, these parallel examples of comedic practice demonstrate how Latin American film comedies produce a ";critically proximate"; spectator who is capable of perceiving and organizing space and time differently. Combining close readings of films, archival research, film theory, and Latin American history, Mock Classicism rethinks classicism as a discourse that mediates and renders the world and argues that Latin American cinema became classical in distinct ways from Hollywood.
Motion pictures --- Motion picture actors and actresses --- Comedy films --- Comedy videos --- Cinema --- Feature films --- Films --- Movies --- Moving-pictures --- Audio-visual materials --- Mass media --- Performing arts --- Film actors --- Film stars --- Motion picture stars --- Movie stars --- Moving-picture actors and actresses --- Stars, Movie --- Actors --- Actresses --- Production and direction --- History --- History and criticism --- 1960s. --- alternate history. --- archival research. --- cantinflas oscarito. --- comedians. --- comedic practice. --- cultural significance. --- embodiment. --- film comedies. --- film theory. --- films. --- grande otelo. --- latin america. --- latin american cinema. --- latin american history. --- linguistic play. --- luis sandrini. --- modernization. --- new latin american cinema. --- nini marshall. --- popularity. --- spatiotemporal emplacement.
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Focusing on two cases of resettlement in rural Cundinamarca, Colombia, this book examines how displaced campesinos make sense of their displacement and how displacement shapes their everyday lives. It is based on a ten-month fieldwork employing ethnographic methods working, living and sharing with the displaced and their host. The book calls for a longer time-frame analysis of the phenomenon of displacement, which considers people's lives both pre- and post- physical relocation. It examines how violence and terror altered people's sense of place and set off displacement process before they actually moved. It analyses the challenges the displaced are facing in their subsequent place-making endeavours, including the negotiation of social relations, consequences of categorization, engagement with the physical land, and memories of violence to challenge the notion that displacement starts with uprooting and terminates with resettlement or return --
Lebensbedingungen --- Soziale Situation --- Vertreibung --- Umsiedlung --- Refugees --- Displaced persons --- Persons --- Aliens --- Deportees --- Exiles --- Social conditions. --- Kolumbien --- Colombia. --- Colombie --- Estados Unidos de Colombia --- Gelunbiya --- Grã-Colômbia --- Gran Colombia --- Kolumbii︠a︡ --- Koronbia --- Kūlūmbiyā --- Neu-Granada --- República de Colombia --- United States of Colombia --- Колумбия --- كولومبيا --- コロンビア --- 哥伦比亚 --- Granadine Confederation --- New Granada --- New Granada (Republic : 1832-1858) --- Auswanderung --- Zwangsumsiedlung --- Ethnische Säuberung --- Zwangsmigration --- Flucht --- Soziale Lage --- Soziale Verhältnisse --- Soziallage --- Sozialverhältnisse --- Soziale Bedingungen --- Situation --- Soziale Stellung --- Lebenssituation --- Lebensverhältnisse --- Lebenslage --- Lebensumstände --- Kolumbii͡ --- Kūlūmbiy --- Columbien --- Colombia --- República de Colombia --- Columbia --- République de Colombie --- Republic of Colombia --- Kolumbianer --- Neugranada --- Confederación Granadina --- 1819-1832 --- 1861 --- -Lebensbedingungen --- -Refugees --- Réfugiés. --- Social history. --- Histoire sociale. --- Colombie. --- Displacement. --- belonging. --- categorisation. --- emplacement. --- fear. --- identity. --- internal displacement. --- place attachment. --- place. --- temporality. --- trust. --- violence.
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