The relative behaviour of bulk and shear modulus as an indicator of the iron spin transition in the lower mantle
Author:
Funder
Australian National University
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference46 articles.
1. Spin crossover in ferropericlase at high pressure: a seismologically transparent transition?;Antonangeli;Science,2011
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3. High-pressure experiments and the phase diagram of lower mantle and core materials;Boehler;Rev. Geophys.,2000
4. Thermodynamic parameters in the Earth as determined from seismic profiles;Brown;Geophys. J. Int.,1981
5. Cold shear modulus and Grüneisen parameter at all densities;Burakovsky;Solid State Commun.,2004
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1. Effect of vacuum atomic oxygen irradiation on tribological properties of MoS2/WC multilayer films;Ceramics International;2024-07
2. Full-waveform tomography reveals iron spin crossover in Earth’s lower mantle;Nature Communications;2024-03-04
3. Compressibility of ferropericlase at high-temperature: Evidence for the iron spin crossover in seismic tomography;Earth and Planetary Science Letters;2023-09
4. Broad Elastic Softening of (Mg,Fe)O Ferropericlase Across the Iron Spin Crossover and a Mixed‐Spin Lower Mantle;Journal of Geophysical Research: Solid Earth;2022-08
5. The Earth's Interior: From the Perspective of Mineral Science;Journal of Geography (Chigaku Zasshi);2022-04-25
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