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Universites et colleges --- Ecoles --- Emplacement --- Emplacement --- Universites et colleges --- Ecoles --- Emplacement --- 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.

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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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.