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Mineralogical and geochemical patterns of mantle xenoliths from the Jixia region (Fujian Province, southeastern China)
Zhang G., Bobrov A., Long J., Han W.
Indicator reactions of K and Na activities in the upper mantle: Natural mineral assemblages, experimental data, and thermodynamic modeling
Safonov O., Butvina V.
Glimmerite-wehrlite xenolith from the ugandite of East African Rift: Mineral composition and conditions of formation
Muravyeva N., Senin V.
Carbonate–Silicate–Sulfide Polyphase Inclusion in Diamond from the Komsomolskaya Kimberlite Pipe, Yakutia
Logvinova A., Wirth R., Zedgenizov D., Taylor L.
Magmatic evolution of the material of the Earth’s lower mantle: Stishovite paradox and origin of superdeep diamonds (Experiments at 24–26 GPa)
Litvin Y., Spivak A., Dubrovinsky L.
Test of the Ballhaus–Berry–Green Ol–Opx–Sp oxybarometer and calibration of a new equation for estimating the redox state of melts saturated with olivine and spinel
Nikolaev G., Ariskin A., Barmina G., Nazarov M., Almeev R.
Viscosity of Depolymerized Dunite Melts under Medium and High Pressures
Persikov E., Bukhtiyarov P., Sokol A.
Water in the Earth’s Lower Mantle
Felix V. Kaminsky
The mineralogy of Ca-rich inclusions in sublithospheric diamonds
Zedgenizov D., Ragozin A., Kalinina V., Kagi H.
MgCO3 + SiO2 Reaction at Pressures up to 32 GPa Studied Using in-Situ X-Ray Diffraction and Synchrotron Radiation
Litasov K., Shatskiy A.
Evolution of the Kerguelen plume and its impact upon the continental and oceanic magmatism of East Antarctica
Sushchevskaya N., Belyatsky B., Dubinin E., Levchenko O.
Evolution of Diamond-Forming Systems of the Mantle Transition Zone: Ringwoodite Peritectic Reaction (Mg,Fe)2SiO4 (Experiment at 20 GPa)
Spivak A., Litvin Y., Zakharchenko E., Simonova D., Dubrovinsky L.
Age of zircon from apoharzburgite serpentinite representing mantle of the Uralian paleoocean
Montero P., Bea F., Fershtater G.
Fundamentals of the mantle carbonatite concept of diamond genesis
Litvin Y., Spivak A., Kuzyura A.
Melting Relations in the Model Pyrolite at 2.5, 3.0, 7.0 GPa and 1400–1800°C: Application to the Problem of the Formation of High-Chromium Garnets
Matrosova E., Bendeliani A., Bobrov A., Kargal’tsev A., Ignat’ev Y.
Modeling the dynamics of sublimation of fractured rocks in the lithospheric mantle wedge beneath volcanoes of the Avacha group (Kamchatka)
Sharapov V., Kuznetsov G., Logachev V., Cherepanova V., Cherepanov A.
Micro- and nano-inclusions in a superdeep diamond from São Luiz, Brazil
Kagi H., Zedgenizov D., Ohfuji H., Ishibashi H.
SiO2 Inclusions in Sublithospheric Diamonds
Zedgenizov D., Ragozin A., Kagi H., Yurimoto H., Shatsky V.
Application of IR and Raman spectroscopy for the determination of the role of oxygen fugacity in the formation of N–С–О–Н molecules and complexes in the iron-bearing silicate melts at high pressures
Kadik A., Koltashev V., Kryukova E., Tsekhonya T., Plotnichenko V.
The influence of low aluminum concentrations on the composition and conditions of crystallization of majorite–knorringite garnets: Experiment at 7.0 GPa and 1500–1700°C
Sirotkina E., Bobrov A., Kargal’tsev A., Ignat’ev Y., Kadik A.
Effect of Thermal State on the Mantle Composition and Core Sizes of the Moon
Kuskov O., Kronrod E., Kronrod V.
Distribution of siderophile and chalcophile elements in serpentinites of the oceanic lithosphere as an insight into the magmatic and crustal evolution of mantle peridotites
Silantyev S., Kubrakova I., Tyutyunnik O.
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