Earth and Planetary Sciences
Magma
100%
Lower Mantle
67%
Machine Learning
60%
Thermal Conductivity
40%
Core-Mantle Boundary
35%
Perovskite
35%
Seismic Anisotropy
30%
Silicate Melt
30%
Upper Mantle
28%
Dynamic Simulation
27%
Silicate
25%
Bulk Modulus
23%
Seismic Velocity
23%
Boundary Condition
23%
Earth Pressure
20%
Magnesium Oxide
20%
Peru
20%
Thermochemical
20%
Earth Mantle
20%
Acoustic Velocity
20%
Fractionation
20%
Thermal Radiation
20%
Planetary Atmosphere
20%
North America
20%
Mantle Convection
13%
Heat Flux
10%
Alkali Halides
10%
Seismic Data
10%
Oceanic Lithosphere
10%
Transport Property
10%
Shear-Wave Splitting
10%
Bolivia
10%
Plate (Tectonics)
10%
Lithosphere
10%
Volcanism
10%
Radiation Spectra
10%
Stacking
10%
United States of America
10%
Laser Heating
10%
Pacific Ocean
10%
Radiant Flux Density
10%
Geodynamics
10%
Thermal Evolution
8%
Water Distribution
8%
Ocean Island Basalt
6%
Paleointensity
6%
Mexico
5%
Reflectance
5%
Moisture Content
5%
Partition Coefficient
5%
Earth Core
5%
Eutectics
5%
Extrasolar Planet
5%
Keyphrases
North America
20%
Lowermost Mantle
20%
Seismic Anisotropy
20%
Earth Pressure
20%
Melts System
20%
Silicate Liquids
20%
Redox History
20%
Viscosity Jump
20%
Polytypic
20%
Basal Magma Ocean
20%
Melting Phase Relations
20%
Melting Temperature Depression
20%
Magma Ocean
20%
Crystallization
20%
Hydrous
20%
Geomagnetism
13%
Core-mantle Boundary Heat Flow
13%
Mg Partitioning
13%
Absorption Behavior
10%
Runaway Heating
10%
Anisotropy
8%
Ocean Island Basalt
6%
Phase Stable
6%
Core Heat Flow
6%
Slab Stagnation
6%
Plume Deflection
6%
Liquidus
6%
Homologous Temperature
6%
Heat Test
6%
Paleointensity
6%
Liquidus Temperature
6%
Earth Accretion
6%
Magma Ocean Crystallization
6%
Tungsten Anomaly
6%
Hf4+
6%
Mantle Anisotropy
5%
Hydrous Melt
5%
Melt Migration
5%
Congruent Melting
5%
Seismic Anomalies
5%
Thermal Radiation Intensity
5%
Margules
5%
Lindemann Law
5%
Engineering
Diamond
40%
Melting Temperature
25%
Thermal Conductivity
24%
Temperature Gradient
20%
Defects
20%
Computer Simulation
20%
Deep Learning Method
20%
Constrains
11%
Heat Flux
10%
Drastic Change
10%
Thermal Radiation
10%
Deep Learning
6%
Stable Phase
6%
Triple Point
6%
Learning Scheme
6%
Magnetic Field
6%
Temperature Range
6%
Feature Extraction
6%
Laser Heating
5%
Radiation Intensity
5%
