Immiscible metallic melts in the upper mantle beneath Mount Carmel, Israel: Silicides, phosphides, and carbides

Cr 2 O 3 in corundum: Ultrahigh contents under reducing conditions

Ultra-reduced phases in ophiolites cannot come from Earth’s mantle

Silicon Carbide Dust? The Answer Is Blowin’ in the Wind

Why Tolbachik Diamonds Cannot be Natural

An evolutionary system of mineralogy. Part I: Stellar mineralogy (>13 to 4.6 Ga)

“Kamchatite” diamond aggregate from northern Kamchatka, Russia: New find of diamond formed by gas phase condensation or chemical vapor deposition

Phase transition in SiC from zinc-blende to rock-salt structure and implications for carbon-rich extrasolar planets

A new hydrothermal moissanite cell apparatus for optical in-situ observations at high pressure and high temperature, with applications to bubble nucleation in silicate melts

Deep mantle origin and ultra-reducing conditions in podiform chromitite: Diamond, moissanite, and other unusual minerals in podiform chromitites from the Pozanti-Karsanti ophiolite, southern Turkey

Origin and significance of diamonds and other exotic minerals in the Dingqing ophiolite peridotites, eastern Bangong-Nujiang suture zone, Tibet

Spectroscopic analysis of microdiamonds in ophiolitic chromitite and peridotite

Discovery of in situ super-reducing, ultrahigh-pressure phases in the Luobusa ophiolitic chromitites, Tibet: New insights into the deep upper mantle and mantle transition zone

Ca-Al-silicate inclusions in natural moissanite (SiC)

Diamonds in Ophiolites

Local redox buffering by carbon at low pressures and the formation of moissanite – natural SiC

PERSPECTIVE

Carbon Mineralogy and Crystal Chemistry

A moissanite cell apparatus for optical in situ observation of crystallizing melts at high temperature

First in situ observation of crystallization processes in a basaltic-andesitic melt with the moissanite cell