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Full-waveform tomography reveals iron spin crossover in Earth's lower mantle
Laura Cobden
*
, Jingyi Zhuang
, Wenjie Lei
, Renata Wentzcovitch
*
,
Jeannot Trampert
, Jeroen Tromp
*
Corresponding author for this work
Research Programme in Earth Sciences Utrecht (DES / IVAU)
DES - Seismology group
Utrecht Centre for Earth & Planetary Processes (UCEPP, in development)
Princeton University
Columbia University
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Keyphrases
Spin Crossover
100%
Wave Speed
100%
Earth's Lower Mantle
100%
Full Waveform Tomography
100%
Shear Wave Velocity
50%
Speed Distribution
50%
Bulk Wave
50%
Temperature Effect
25%
Silica
25%
Tomographic Model
25%
Spin State
25%
Lower Mantle
25%
Seismic Wave Velocity
25%
Three Dimensional Model
25%
Seismic Structure
25%
Core-mantle Boundary
25%
Mineralogical Phases
25%
Spin Electronics
25%
Ferropericlase
25%
Joint Interpretation
25%
Silica Content
25%
Spherical Averages
25%
Basal Magma Ocean
25%
Silica Enrichment
25%
Earth and Planetary Sciences
Tomography
100%
Lower Mantle
100%
Iron
100%
Magma
33%
Core-Mantle Boundary
33%
Seismic Wave
33%