Exploring and Modeling the Magma-Hydrothermal Regime
Eichelberger, John C.
Exploring and Modeling the Magma-Hydrothermal Regime - Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute 2020 - 1 electronic resource (262 p.)
Open Access
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.
Creative Commons
English
books978-3-03936-637-8 9783039366361 9783039366378
10.3390/books978-3-03936-637-8 doi
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
Exploring and Modeling the Magma-Hydrothermal Regime - Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute 2020 - 1 electronic resource (262 p.)
Open Access
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.
Creative Commons
English
books978-3-03936-637-8 9783039366361 9783039366378
10.3390/books978-3-03936-637-8 doi
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