Minerals included in diamonds provide direct information about the petrologic and chemical
environment of diamond crystallization. They record information relating to local and …

Sublithospheric diamonds and the inclusions they may carry crystallize in the
asthenosphere, transition zone, or uppermost lower mantle (from 300 to∼ 800 km), and are …

Forty-one diamonds sourced from the Juina-5 kimberlite pipe in Southern Brazil, which
contain optically identifiable inclusions, have been studied using an integrated approach …

Laser-heated diamond anvil cell (LH-DAC) experimentation has emerged as a leading
technique for materials processing at extreme pressures and temperatures. LH-DAC …

Abstract “Super-deep” diamonds are thought to crystallize between 300 and 800 km depth
because some of the inclusions trapped within them are considered to be the products of …

The science of studying diamond inclusions for understanding Earth history has developed
significantly over the past decades, with new instrumentation and techniques applied to …

The production of metal via the iron disproportionation reaction in the deep Earth has been a
long debated topic with important implications for the geochemistry of the lower mantle. To …

The trace element compositions of inclusions in sub-lithospheric diamonds from the Juina-5
kimberlite, Brazil, are presented. Literature data for mineral/melt partition coefficients were …

We carried out a series of silicate fractional crystallization experiments at lower mantle
pressures using the laser‐heated diamond anvil cell. Phase relations and the compositional …

Classic lamellar clinopyroxene-ilmenite intergrowths (type 1) are extended to include
discovery of olivine-ilmenite-perovskite-wüstite (type 2) and olivine-spinel-perovskite (type …