In situ measurements of the majorite-akimotoite-perovskite phase transition boundaries in MgSiO 3
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December 2001 |
Vibrational spectrum of MgSiO 3 perovskite: Zero-pressure Raman and mid-infrared spectra to 27 GPa
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January 1987 |
Compositional dependence of structural transition pressures in amorphous phases with mantle-related compositions
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June 2009 |
Laser heated diamond cell system at the Advanced Photon Source for in situ x-ray measurements at high pressure and temperature
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January 2001 |
The Postspinel Phase Boundary in Mg2SiO4 Determined by in Situ X-ray Diffraction
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March 1998 |
Determination of pressure effect on thermocouple electromotive force using multi-anvil apparatus
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March 2016 |
Intercomparison of the gold, platinum, and MgO pressure scales up to 140 GPa and 2500 K: EQUATIONS OF STATE OF AU, PT, AND MGO
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May 2017 |
Temperature gradients and evaluation of thermoelastic properties in the synchrotron-based laser-heated diamond cell
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June 2004 |
A numerical model for steady-state temperature distributions in solid-medium high-pressure cell assemblies
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February 2006 |
Seismic Evidence for Olivine Phase Changes at the 410- and 660-Kilometer Discontinuities
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May 2002 |
The postspinel boundary in pyrolitic compositions determined in the laser-heated diamond anvil cell
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June 2014 |
Toward an internally consistent pressure scale
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May 2007 |
Adiabatic temperature profile in the mantle
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November 2010 |
Complete agreement of the post-spinel transition with the 660-km seismic discontinuity
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April 2018 |
Shock compression of tungsten and molybdenum
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February 1992 |
Post-spinel transition in Mg2SiO4 determined by high P–T in situ X-ray diffractometry
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April 2003 |
Reconciling PP and P′P′ precursor observations of a complex 660 km seismic discontinuity
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May 2013 |
Equations of state of MgO, Au, Pt, NaCl-B1, and NaCl-B2: Internally consistent high-temperature pressure scales
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December 2007 |
The influence of wavelength-dependent absorption and temperature gradients on temperature determination in laser-heated diamond-anvil cells
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January 2017 |
A complex 660 km discontinuity beneath northeast China
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July 2003 |
Brillouin spectrometer interfaced with synchrotron radiation for simultaneous x-ray density and acoustic velocity measurements
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October 2006 |
The post-spinel transformation in Mg2SiO4 and its relation to the 660-km seismic discontinuity
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May 2001 |
Effect of Pressure on the emf of Chromel‐Alumel and Platinum‐Platinum 10% Rhodium Thermocouples
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October 1970 |
X-ray diffraction study of the static strength of tungsten to
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April 2006 |
Thermodynamic parameters in the Earth as determined from seismic profiles
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September 1981 |
Vitreous forsterite (Mg 2 SiO 4 ): Synthesis, structure, and thermochemistry
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July 2001 |
DIOPTAS : a program for reduction of two-dimensional X-ray diffraction data and data exploration
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May 2015 |
Effect of pressure on temperature measurements using WRe thermocouple and its geophysical impact
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January 2020 |
Constraints on seismic velocities in the Earth from traveltimes
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July 1995 |
Absolute temperature measurement in a laser-heated diamond anvil cell
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January 2004 |
Microscopic anharmonicity and equation of state of MgSiO 3 -perovskite
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October 1996 |
Preliminary reference Earth model
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June 1981 |
Measurement of the shear strength of pure tungsten during one-dimensional shock loading
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February 2007 |
Post-spinel transitions in pyrolite and Mg2SiO4 and akimotoite–perovskite transition in MgSiO3: Precise comparison by high-pressure high-temperature experiments with multi-sample cell technique
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September 2011 |
Comparative Raman spectroscopic study on ilmenite-type MgSiO3 (akimotoite), MgGeO3, and MgTiO3 (geikielite) at high temperatures and high pressures
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January 2008 |
The Gruneisen ratio for the last 30 years
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November 2000 |
Experimentally determined postspinel transformation boundary in Mg 2 SiO 4 using MgO as an internal pressure standard and its geophysical implications : POSTSPINEL TRANSFORMATION IN MG
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February 2004 |
Cell assemblies for reproducible multi-anvil experiments (the COMPRES assemblies)
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January 2012 |
Complete agreement of the post-spinel transition with the 660-km seismic discontinuity
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January 2018 |