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Ringwoodite
Quantification of Water in Hydrous Ringwoodite
Seismic Evidence for Water Deep in Earth's Upper Mantle
Influence of the Ringwoodite-Perovskite Transition on Mantle Convection in Spherical Geometry As a Function of Clapeyron Slope A
The Upper Mantle and Transition Zone
RINGWOODITE-OLIVINE ASSEMBLAGES in DHOFAR 922 L6 MELT VEINS. D. D. Badjukov1, F. Brandstaetter2, G. Kurat3, E. Libowitzky3 and J
Spin Transition of Fe2+ in Ringwoodite (Mg,Fe)2Sio4 at High Pressures
Whole-Mantle Convection and the Transition-Zone Water Filter
Comparative Compressibility of Hydrous Wadsleyite and Ringwoodite
5 Ringwoodite: Its Importance in Earth Sciences
Phase Relations in MAFSH System up to 21 Gpa: Implications for Water Cycles in Martian Interior
Mccoy, T. J. Mineralogical Evolution of Meteorites. Elements
Suppressing the Martian Dynamo with Ongoing Hydrogenation of the Core by Hydrated Mantle Minerals
The Coexistence of Wadsleyite and Ringwoodite in L/LL Chondrite SAH 293: Constraints on Shock Pressure Conditions and Olivine Transformation
1 Revision 3: Phase Transformation of Hydrous Ringwoodite to the Lower
The Post-Spinel Transformation in Mg2sio4 and Its Relation to the 660-Km Seismic Discontinuity
Incorporation of Tetrahedral Ferric Iron in Hydrous Ringwoodite
Lecture 10: Mantle Minerals
Rare Diamond Confirms That Earth's Mantle Holds an Ocean's Worth Of
Top View
Phase Transformation of Hydrous Ringwoodite to the Lower-Mantle Phases and the Formation of Dense Hydrous Silica
Equation of State of Hydrous Fo90 Ringwoodite to 45 Gpa by Synchrotron Powder Diffraction
Fayalite- Spinel + Stishovite in Shocked Umbarger L6 Chondrite
Shear-Induced Ringwoodite Formation in the Martian Shergottite Dar Al Gani 670
Water Incorporation in Wadsleyite and Ringwoodite: Effect on Phase Stability and Structure
Experimental Deformation of Forsterite, Wadsleyite and Ringwoodite: Implications for Seismic Anisotropy of the Earth’S Mantle Hélène Couvy
Spe388 207-216 Presnall
Water Partitioning in the Earth's Mantle
Complete Agreement of the Post-Spinel Transition Pressure with the 660-Km Seismic Discontinuity Depth
Department of Embryology
Program of Technical Sessions
Water-Induced Convection in the Earth's Mantle Transition Zone
Back-Transformation of Ringwoodite in L5-6 Chondrite Mbale: Implications for the Preservation of Shock Effects in Highly Shocked Meteorites J
Evidence for Fractional Crystallization of Wadsleyite and Ringwoodite from Olivine Melts in Chondrules Entrained in Shock-Melt Veins
High Pressure Crystal Chemistry of Hydrous Ringwoodite and Water in the Earth’S Interior
Effects on the Wadsleyite–Ringwoodite Phase Transition
Complete Agreement of the Post-Spinel Transition with the 660
Sound Velocities of Hydrous Ringwoodite to 16Gpa and 673K
Atomistic Simulation of Mg2sio4 and Mg2geo4 Spinels: a New Model
Plastic Deformation Experiments to High Strain on Mantle Transition Zone Minerals Wadsleyite and Ringwoodite in the Rotational Drickamer Apparatus
Forsterite, Hydrous and Anhydrous Wadsleyite and Ringwoodite
Shock-Induced Ringwoodite Rims Around Olivine Fragments in Melt Vein of Antarctic Chondrite GRV022321 : Transformation Mechanism Zhidong
Ringwoodite Lamellae in Olivine: Clues to Olivine–Ringwoodite Phase Transition Mechanisms in Shocked Meteorites and Subducting Slabs
Synthesis of Large and Homogeneous Single Crystals of Water-Bearing Minerals by Slow Cooling at Deep-Mantle Pressures
Thermophysical Properties and Phase Diagrams in the System Mgo–Sio2–Feo at Upper Mantle and Transition Zone Conditions Derived from a Multiple-Einstein Method
Physics of the Earth and Planetary Interiors 184 (2011) 91–104
Synthesis of Inverse Ringwoodite Sheds Light on the Subduction History of Tibetan Ophiolites Received: 25 January 2018 Luca Bindi 1,2, William L
Mineral Evolution