An experimental investigation of the stability of majoritic garnet in the Earth's mantle and an improved majorite geobarometer
CH Wijbrans, A Rohrbach, S Klemme - Contributions to Mineralogy and …, 2016 - Springer
The stability of the majorite component in garnet has been experimentally investigated at
high pressure and high temperature, focusing on the effect of bulk composition and …
high pressure and high temperature, focusing on the effect of bulk composition and …
Tracing the depositional history of Kalimantan diamonds by zircon provenance and diamond morphology studies
Diamonds in alluvial deposits in Southeast Asia are not accompanied by indicator minerals
suggesting primary kimberlite or lamproite sources. The Meratus Mountains in Southeast …
suggesting primary kimberlite or lamproite sources. The Meratus Mountains in Southeast …
Thermoelastic properties of chromium oxide Cr2O3 (eskolaite) at high pressures and temperatures
A new synchrotron X-ray diffraction study of chromium oxide Cr 2 O 3 (eskolaite) with the
corundum-type structure has been carried out in a Kawai-type multi-anvil apparatus to …
corundum-type structure has been carried out in a Kawai-type multi-anvil apparatus to …
High‐Pressure and High‐Temperature Single‐Crystal Elasticity of Cr‐Pyrope: Implications for the Density and Seismic Velocity of Subcontinental Lithospheric Mantle
J Xu, D Fan, B Li, SN Tkachev… - Geochemistry …, 2022 - Wiley Online Library
Single‐crystal X‐ray diffraction and Brillouin spectroscopy experiments were performed on a
natural Cr‐pyrope (Prp71. 0Alm12. 6Sps0. 7Grs3. 5Uvr12. 2) at high pressure and high …
natural Cr‐pyrope (Prp71. 0Alm12. 6Sps0. 7Grs3. 5Uvr12. 2) at high pressure and high …
Thermal equation of state of Cr-pyrope: implications for entrapment pressure of Cr-pyrope inclusion in diamond
Cr-pyrope is one of the most abundant mineral inclusions in peridotitic diamonds and its
thermal equation of state (EoS) is a prerequisite for accurately determining its entrapment …
thermal equation of state (EoS) is a prerequisite for accurately determining its entrapment …
Effect of composition on compressibility of skiagite-Fe-majorite garnet
Skiagite-Fe-majorite garnets were synthesized using a multianvil apparatus at 7.5–9.5 GPa
and 1400–1600 K. Single-crystal X-ray diffraction at ambient conditions revealed that …
and 1400–1600 K. Single-crystal X-ray diffraction at ambient conditions revealed that …
Synthesis and crystal structure of chromium-bearing anhydrous wadsleyite
EA Sirotkina, L Bindi, AV Bobrov, SM Aksenov… - Physics and Chemistry …, 2018 - Springer
A chromium-bearing wadsleyite (Cr-Wad) was synthesized in the model system Mg 2 SiO 4–
MgCr 2 O 4 at 14 GPa and 1600° C and studied from the chemical and structural point of …
MgCr 2 O 4 at 14 GPa and 1600° C and studied from the chemical and structural point of …
[HTML][HTML] Thermodynamic behavior of Na-majorite and knorringite-majorite garnet systems
The behavior of thermal parameters pressure (P) and thermoelastic parameters ie
Isothermal bulk modulus (KT), its pressure derivative (K′ T) and Thermal expansivity (α) …
Isothermal bulk modulus (KT), its pressure derivative (K′ T) and Thermal expansivity (α) …
Фазовые отношения в модельной системе SiO2–MgO–Cr2O3 (по результатам экспериментов в петрологически значимых сечениях при 12–24 ГПа и 1600° …
ЕА Матросова, АВ Бобров, Л Бинди, Т Ирифуне - Петрология, 2018 - elibrary.ru
Обсуждаются новые результаты экспериментального изучения модельного сечения
мэйджорит MgSiO 3–магнезиохромит MgCr 2 O 4 и анализируются общие особенности …
мэйджорит MgSiO 3–магнезиохромит MgCr 2 O 4 и анализируются общие особенности …
Phase Relations in the Model System SiO2–MgO–Cr2O3: Evidence from the Results of Experiments in Petrologically Significant Sections at 12–24 GPa and 1600°C
The new results of an experimental study of the majorite MgSiO 3–magnesiochromite MgCr
2 O 4 model section are discussed, and general topology of the SiO 2–MgO–Cr 2 O 3 …
2 O 4 model section are discussed, and general topology of the SiO 2–MgO–Cr 2 O 3 …