An experimental investigation of the stability of majoritic garnet in the Earth’s mantle and an improved majorite geobarometer

Phase relations and formation of chromium-rich phases in the system Mg4Si4O12–Mg3Cr2Si3O12 at 10–24 GPa and 1,600 °C

(2015) E. A. Sirotkina et al.   CONTRIBUTIONS TO MINERALOGY AND PETROLOGY

Diamonds in Ophiolites

(2014) J.-S. Yang et al.   Elements

Thermodynamic and magnetic properties of knorringite garnet (Mg3Cr2Si3O12) based on low-temperature calorimetry and magnetic susceptibility measurements

(2014) C. H. Wijbrans et al.   PHYSICS AND CHEMISTRY OF MINERALS

Thermal equation of state of majoritic knorringite and its significance for continental upper mantle

(2014) Anna M. Dymshits et al.   JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH

Garnet in the Earth's Mantle

(2013) B. J. Wood et al.   Elements

Metapyroxenite in the mantle transition zone revealed from majorite inclusions in diamonds

(2013) Ekaterina S. Kiseeva et al.   GEOLOGY

Melting and Phase Relations of Carbonated Eclogite at 9-21 GPa and the Petrogenesis of Alkali-Rich Melts in the Deep Mantle

(2013) E. S. Kiseeva et al.   JOURNAL OF PETROLOGY

Stagnation of subducting slabs in the transition zone due to slow diffusion in majoritic garnet

(2013) W. L. van Mierlo et al.   Nature Geoscience

Na-bearing majoritic garnet in the Na2MgSi5O12–Mg3Al2Si3O12 join at 11–20GPa: Phase relations, structural peculiarities and solid solutions

(2012) Anna M. Dymshits et al.   GEOCHIMICA ET COSMOCHIMICA ACTA

Phase relations in Mg3Cr2Si3O12 and formation of majoritic knorringite garnet at high pressure and high temperature

(2012) Yongtao ZOU et al.   Journal of Mineralogical and Petrological Sciences

Crystal chemistry of sodium in the Earth's interior: The structure of Na2MgSi5O12 synthesized at 17.5 GPa and 1700  C

(2011) L. Bindi et al.   AMERICAN MINERALOGIST

Petrologic origin of exsolution textures in mantle minerals: evidence in pyroxenitic xenoliths from Yakutia kimberlites

(2011) Taisia Aleksandrovna Alifirova et al.   INTERNATIONAL GEOLOGY REVIEW

Experimental Evidence for a Reduced Metal-saturated Upper Mantle

(2011) Arno Rohrbach et al.   JOURNAL OF PETROLOGY

Redox freezing and melting in the Earth’s deep mantle resulting from carbon–iron redox coupling

(2011) Arno Rohrbach et al.   NATURE

Deep Mantle Cycling of Oceanic Crust: Evidence from Diamonds and Their Mineral Inclusions

(2011) M. J. Walter et al.   SCIENCE

Majoritic garnet: A new approach to pressure estimation of shock events in meteorites and the encapsulation of sub-lithospheric inclusions in diamond

(2010) Kenneth D. Collerson et al.   GEOCHIMICA ET COSMOCHIMICA ACTA

Diamond formation in the deep mantle: the record of mineral inclusions and their distribution in relation to mantle dehydration zones

(2010) B. Harte   MINERALOGICAL MAGAZINE

The Upper Mantle and Transition Zone

(2008) D. J. Frost   Elements

Phase relations on the diopside–jadeite–hedenbergite join up to 24GPa and stability of Na-bearing majoritic garnet

(2008) Andrey V. Bobrov et al.   GEOCHIMICA ET COSMOCHIMICA ACTA

The origin of cratonic diamonds — Constraints from mineral inclusions

(2008) T. Stachel et al.   ORE GEOLOGY REVIEWS

Density profiles of oceanic slabs and surrounding mantle: Integrated thermodynamic and thermal modeling, and implications for the fate of slabs at the 660km discontinuity

(2008) Jibamitra Ganguly et al.   PHYSICS OF THE EARTH AND PLANETARY INTERIORS

Majoritic garnets monitor deep subduction fluid flow and mantle dynamics

(2007) M. Scambelluri et al.   GEOLOGY