Skip to Main Content
Skip Nav Destination

Phase transition of wadsleyite-ringwoodite in the Mg2SiO4-Fe2SiO4 system

American Mineralogist (2019) 104 (4): 588–594.
This article has been cited by the following articles in journals that are participating in CrossRef Cited-by Linking.
No globally detectable seismic interfaces within Earth's mantle transition zone: Evidence for basalt enrichment
Earth and Planetary Science Letters (2024) 641: 118838.
The Upper‐Mantle Structure Beneath Alaska Imaged by Teleseismic S‐Wave Reverberations
Journal of Geophysical Research: Solid Earth (2023) 128 (6)
First-principles investigation of equilibrium magnesium isotope fractionation among mantle minerals: Review and new data
Earth-Science Reviews (2023) 237: 104315.
Hadean mantle oxidation inferred from melting of peridotite under lower-mantle conditions
Nature Geoscience (2023) 16 (5): 461.
High pressure-temperature single-crystal elasticity of ringwoodite: Implications for detecting the 520 discontinuity and metastable ringwoodite at depths greater than 660 km
Earth and Planetary Science Letters (2022) 579: 117359.
Apollo 15 regolith breccia provides first natural evidence for olivine incongruent melting
American Mineralogist (2022) 107 (9): 1661.
A Single 520 km Discontinuity Beneath the Contiguous United States With Pyrolitic Seismic Properties
Geophysical Research Letters (2022) 49 (24)
A first-principles study of water in wadsleyite and ringwoodite: Implication for the 520 km discontinuity
American Mineralogist (2022) 107 (7): 1361.
Mantle Transition Zone Receiver Functions for Bermuda: Automation, Quality Control, and Interpretation
Journal of Geophysical Research: Solid Earth (2021) 126 (3)
Global variations of Earth's 520- and 560-km discontinuities
Earth and Planetary Science Letters (2020) 552: 116600.
Close Modal

or Create an Account

Close Modal
Close Modal