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 …
The reliability of eight Fe–Mg exchange geothermobarometers for garnet-bearing peridotites, pyroxenites and eclogites has been examined using a database comprised of …
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 …
It is generally accepted that carbonatite metasomatism in the subcontinental lithospheric mantle (SCLM) inevitably causes wehrlitization of the primary lherzolite substrate. However …
Phase relations in the carbonate constituent of mafic and ultramafic suites are decisive in the deep carbon cycle and partial melting in the Earth's mantle. Here we present an …
The interaction of natural eclogite (Ecl) with synthetic hydrous carbonate melts with Na: K= 0: 1 (KH2) and 1: 1 (NKH2) was studied in multianvil experiments at 3–6 GPa and 850–1250° …
It is generally accepted that carbonates can be subducted to the mantle depths, where they are reduced with iron metal to produce a diamond. In this work, we found that this is not …
A Shatskiy, YG Vinogradova, AV Arefiev… - … to Mineralogy and …, 2023 - Springer
In this work, we studied the phase relationships in the NaAlSi2O6–CaMgSi2O6–CO2 system in the range of 3–6.5 GPa and 900–1500℃ using a multianvil press. The duration of most …