Kimberlites represent magmas derived from great mantle depths and are the principal
source of diamonds. Kimberlites and their xenolith cargo have been extremely useful for …

Using water and major and trace element data obtained from melt inclusions primarily in
pegmatite quartz we have shown in this, and previous papers, that melt–melt–fluid …

This contribution provides an overview of available experimental, thermodynamic, and
molecular data on Au aqueous speciation, solubility, and partitioning in major types of …

Melt inclusions (MI) are considered the best tool available for determining the pre-eruptive
volatile contents of magmas. H2O and CO2 concentrations of the glass phase in MI are …

Liquid–liquid partitioning of 42 elements between synthetic silicate melts and immiscible
fluoride, chloride, carbonate, phosphate and sulfate liquids was studied at temperatures of …

Mineral-hosted melt inclusions have become an important source of information on
magmatic processes. As the number of melt inclusion studies increases, so does the need to …

Geofluids: Developments in Microthermometry, Spectroscopy, Thermodynamics, and Stable
Isotopes is the definitive source on paleofluids and the migration of hydrocarbons in …

As volatile and variably mobile components, halogens play key roles in magmatic,
metasomatic, mineralizing, and volcanic processes by influencing the physical and chemical …

Pegmatites and adjacent subsolvus granites (two alkali feldspars) of the Mid-Proterozoic
Strange Lake pluton (Québec-Labrador, Canada) host potentially economic concentrations …

Olivine-hosted melt inclusions (MIs) provide samples of magmatic liquids and their dissolved
volatiles from deep within the plumbing system. Inevitable post-entrapment modifications …