In the interest of constraining the volatile budgets of the Earth's interior, melt inclusions are a valuable tool because they provide a geologically persistent record of melt volatile contents before they degas to the atmosphere during volcanic eruptions. However, melt inclusions require special care because of the possibility for volatile elements to diffuse from the glass into a separate fluid phase (bubble; e.g. CO2) or out of the olivine host (e.g. H2O)..
The CO2 contents of olivine-hosted melt inclusions have previously been used to constrain the depth ...
International audienceReliable evaluation of CO2 contents in parental arc magmas, which can be prese...
The H2O and CO2 contents of melt inclusions can potentially be used to infer pressures of crystalliz...
Primitive olivine-hosted melt inclusions provide information concerning the pre-eruptive volatile c...
Primitive olivine-hosted melt inclusions provide information concerning the pre-eruptive volatile c...
Primitive olivine-hosted melt inclusions (MI) are a useful means to estimate the pre-eruptive volati...
Co-auteur étrangerInternational audienceolivine-hosted melt inclusions (Mis) provide samples of magm...
Co-auteur étrangerInternational audienceolivine-hosted melt inclusions (Mis) provide samples of magm...
Co-auteur étrangerInternational audienceolivine-hosted melt inclusions (Mis) provide samples of magm...
Co-auteur étrangerInternational audienceolivine-hosted melt inclusions (Mis) provide samples of magm...
Carbon dioxide (CO2) is one of the main volatile components of natural magmas, but estimation of its...
The mass of volatiles degassed from volcanic eruptions is often estimated by comparing the volatile ...
Fluids exsolved from mafic melts are thought to be dominantly CO2-H2O ± S fluids. Curiously, althoug...
Fluids exsolved from mafic melts are thought to be dominantly CO2-H2O ± S fluids. Curiously, althoug...
Fluids exsolved from mafic melts are thought to be dominantly CO2-H2O ± S fluids. Curiously, althoug...
The CO2 contents of olivine-hosted melt inclusions have previously been used to constrain the depth ...
International audienceReliable evaluation of CO2 contents in parental arc magmas, which can be prese...
The H2O and CO2 contents of melt inclusions can potentially be used to infer pressures of crystalliz...
Primitive olivine-hosted melt inclusions provide information concerning the pre-eruptive volatile c...
Primitive olivine-hosted melt inclusions provide information concerning the pre-eruptive volatile c...
Primitive olivine-hosted melt inclusions (MI) are a useful means to estimate the pre-eruptive volati...
Co-auteur étrangerInternational audienceolivine-hosted melt inclusions (Mis) provide samples of magm...
Co-auteur étrangerInternational audienceolivine-hosted melt inclusions (Mis) provide samples of magm...
Co-auteur étrangerInternational audienceolivine-hosted melt inclusions (Mis) provide samples of magm...
Co-auteur étrangerInternational audienceolivine-hosted melt inclusions (Mis) provide samples of magm...
Carbon dioxide (CO2) is one of the main volatile components of natural magmas, but estimation of its...
The mass of volatiles degassed from volcanic eruptions is often estimated by comparing the volatile ...
Fluids exsolved from mafic melts are thought to be dominantly CO2-H2O ± S fluids. Curiously, althoug...
Fluids exsolved from mafic melts are thought to be dominantly CO2-H2O ± S fluids. Curiously, althoug...
Fluids exsolved from mafic melts are thought to be dominantly CO2-H2O ± S fluids. Curiously, althoug...
The CO2 contents of olivine-hosted melt inclusions have previously been used to constrain the depth ...
International audienceReliable evaluation of CO2 contents in parental arc magmas, which can be prese...
The H2O and CO2 contents of melt inclusions can potentially be used to infer pressures of crystalliz...