2013•AGU Fall Meeting AbstractsRequires access

Effect of Fe2+ on the high pressure phase transformation of (Mg, Fe)SiO3 in the mantle transition zone: implications for the 520 km seismic discontinuity

H. H. Feng, Yao Wu, Y. Zhang, Zhenmin Jin

Open publisher page 0 citations

Abstract

This record does not include an abstract. Use the full-text link above if available.

About this research paper

What this paper is about

An abstract is not available in the OpenAlex record for this paper.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Key concepts: Geology, Transition zone, Discontinuity (linguistics), Mantle (geology), Core–mantle boundary, Geophysics, Seismology, Mathematical analysis

Back to paper search Browse research topics Original source

Effect of Fe2+ on the high pressure phase transformation of (Mg, Fe)SiO3 in the mantle transition zone: implications for the 520 km seismic discontinuity — Research Paper | ScholarLens