Carbonatites are igneous rocks formed in the crust by fractional crystallization of carbonate-
rich parental melts that are mostly mantle derived. They dominantly consist of carbonate …

Carbonatites are formed from volatile-rich melts, commonly associated with a characteristic
hydrothermal footprint. However, studies of their fluid inclusions are relatively scarce and …

Kerimasi calciocarbonatite consists principally of calcite together with lesser apatite,
magnetite, and monticellite. Calcite hosts fluid and S-bearing Na–K–Ca-carbonate …

Melt inclusions (MI) are small droplets of melt now containing some combination of crystals,
glass and vapor that are trapped in crystals formed in magmas. Over the past few decades …

The evolution of a carbonated nephelinitic magma can be followed by the study of a
statistically significant number of melt inclusions, entrapped in co-precipitated perovskite …

We have reconstructed the compositional evolution of the silicate and carbonate melt, and
various crystalline phases in the subvolcanic reservoir of Kerimasi Volcano in the East …

Ultramafic-alkaline-carbonatite complexes (UACC), which are formed from mantle-derived
carbonated alkali-ultramafic melts in large igneous provinces (LIPs), are important resources …

New data on silicate melt inclusions in accessory Cr-spinel have given an insight into the
physicochemical conditions of petrogenesis of dunites of the Guli massif (northern Siberian …

The investigation of rocks, minerals, and melt inclusions showed that porphyritic alkaline
picrites and meimechites crystallized from different parental magmas. At a similar ultrabasic …

Carbon flux metasomatism in the subduction environment is an important process, but it
remains poorly understood. The paucity of exposed lower crust and upper mantle rocks in …