The paper presents a comprehensive review of currently available data on melt inclusions
entrapped in minerals of kimberlites of different age and different provenance in ancient …

Elucidating the origin, composition and physical properties of primary kimberlite melts is
crucial to our understanding of their source, petrogenesis, ascent mechanisms and …

It is well known that water significantly lowers mantle solidi. But it turns out this paradigm is
not always true. Here, we studied the interaction of K-rich carbonate melts with the natural …

This report deals with the first mineralogical examination of secondary crystallized melt
inclusions (CMIs) in healed cracks within olivine in a mantle peridotite xenolith from the V …

Cratonic lithospheric mantle is believed to have been formed in the Archean, but kimberlite-
hosted coarse peridotites from Udachnaya in the central Siberian craton typically yield …

Identifying the composition of primary/primitive mantle melts is crucial for understanding the
mantle's evolution and mantle‐derived magmatism. Melt inclusions in mantle xenoliths …

The reactions between pyroxenes and carbonates have been studied in the CaMgSi 2 O 6+
MgCO 3 (Di+ 2Mgs), CaMgSi 2 O 6+ NaAlSi 2 O 6+ 2MgCO 3 (Di+ Jd+ 2Mgs), CaMgSi 2 O …

Garnet grains in mantle-derived peridotite xenoliths from kimberlites are surrounded by fine-
grained aggregate of epigenetic minerals known as kelyphite. Existing models propose …

A coesite-bearing diamondiferous eclogite from the Udachnaya kimberlite (Daldyn field,
Siberian craton) has been studied to trace its complex evolution recorded in rock-forming …

The range of carbonatite melts in equilibrium with the subcontinental lithospheric mantle
(SCLM) under geothermal conditions is limited by alkali-rich near-eutectic compositions …