Melt Inclusions in Volcanic Systems: Methods, Applications and ProblemsB. De Vivo, R.J. Bodnar Melt inclusions provide a unique record of the physical and chemical processes operating in active magma chambers associated with volcanic systems. This book includes a summary of modern techniques used to study and interpret melt inclusions in volcanic rocks, as well as descriptive studies of specific volcanoes. These various studies document the enormous potential for melt inclusions to provide a window into the dynamics of active magma chambers.
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Contents
| xi | |
| xv | |
| 1 | |
Chapter 2 Estimating the time scales of magmatic processes | 23 |
quantifying properties and structure of melts across the glass transition | 45 |
methodology and examples | 65 |
Chapter 5 Analyzing hydrogen H2O in silicate glass by secondary ion mass spectrometry and reflectance Fourier transform infrared spectroscopy | 83 |
magma degassing explosive eruptions and volcanic volatile budgets | 105 |
implications of gas emission rate and melt inclusion data | 147 |
Chapter 9 Chemistry and origin of zoned Haüyne in Tahitian phonolite with implications for magmatic fractionation | 163 |
inferences from fluid and melt inclusions in xenoliths | 185 |
constraints from silicate melt inclusions Cl and H2O solubility experiments and modeling | 207 |
Chapter 12 A model for the evolution of Mt SommaVesuvius magmatic system based on fluid and melt inclusion investigations | 227 |
Author Index | 251 |
| 253 | |
degassing process and maficfelsic magma interaction | 129 |
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Melt Inclusions in Volcanic Systems: Methods, Applications and Problems Benedetto De Vivo,R. J. Bodnar No preview available - 2003 |
Common terms and phrases
Acta Aeolian analyses andesitic ascent basaltic basaltic magma Belkin bubbles calibration Cl contents Cl solubility clinopyroxene CO2-rich concentrations conduit crystallisation crystallization curves dacitic decrease degassing process density depth differentiation Dingwell Earth Planet emission rate eruption estimated evolution experimental exsolution exsolved vapor fluid inclusions fractionation Frezzotti geochemical Geol Geology Geophys Geotherm glass transition temperature haüyne Hervig host hydrous hypersaline liquid igneous immiscibility Inamuradake isotopes Iwodake Kamenetsky Kazahaya lava Lowenstern mafic mafic magma magma chamber magmatic system melt composition microprobe minerals Miyakejima nodules nosean olivine Petrol Petrology phenocrysts phonolite phonotephrite plagioclase plinian plinian eruptions pre-eruptive pressure quartz xenoliths quenched ratios reservoirs rhyolitic rhyolitic magma Roedder Saito samples saturation shallow Shinohara Showa-Iwojima silicate melt inclusions silicic magma SIMS skarn SO2 emission Somma-Vesuvius studies sulfur techniques trapped variation Vesuvius viscosity Vivo volatile contents volatile phases volcanic gas volcanic rocks Webster xenoliths zoned
Popular passages
Page 2 - With such striking examples before us, shall we physical geologists maintain that only rough and imperfect methods of research are applicable to our own science ? Against such an opinion I certainly must protest ; and I argue that there is no necessary connexion between the size of an object and the value of a fact, and that, though the objects I have described are minute, the conclusions to be derived from the facts are great.