In Situ Observations of Phase Changes in Shock Compressed Forsterite-Reference-Cited by-同舟云学术

In Situ Observations of Phase Changes in Shock Compressed Forsterite

Published:2018-08-17 Issue:16 Volume:45 Page:8129-8135
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Newman M. G.¹^ORCID,Kraus R. G.²^ORCID,Akin M. C.²^ORCID,Bernier J. V.²,Dillman A. M.³,Homel M. A.²^ORCID,Lee S.⁴,Lind J.²,Mosenfelder J. L.³,Pagan D. C.⁵,Sinclair N. W.⁶^ORCID,Asimow P. D.¹^ORCID

Affiliation:

1. California Institute of Technology Pasadena CA USA

2. Lawrence Livermore National Laboratory Livermore CA USA

3. Department of Earth SciencesUniversity of Minnesota Minneapolis MN USA

4. High Pressure Science and Engineering CenterUniversity of Nevada, Las Vegas Las Vegas NV USA

5. Cornell High Energy Synchrotron Source Ithaca NY USA

6. Dynamic Compression Sector, Institute for Shock Physics, Argonne National LaboratoryWashington State University Pullman WA USA

Funder

Center for Hierarchical Manufacturing, National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL077996

Reference32 articles.

1. Transport properties of Mg2SiO4 liquid at high pressure: Physical state of a magma ocean

2. A measure of mantle melting

3. Experimental evidence for a phase transition in magnesium oxide at exoplanet pressures

4. Thermodynamics of the MgO–SiO2 liquid system in Earth's lowermost mantle from first principles

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