High‐pressure minerals in shocked meteorites-Reference-Cited by-同舟云学术

High‐pressure minerals in shocked meteorites

Published:2017-07-02 Issue:9 Volume:52 Page:2017-2039
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Tomioka Naotaka¹^ORCID,Miyahara Masaaki²^ORCID

Affiliation:

1. Kochi Institute for Core Sample Research Japan Agency for Marine‐Earth Science and Technology Nankoku Kochi 783‐8502 Japan

2. Department of Earth and Planetary Systems Science Graduate School of Science Hiroshima University Higashi‐Hiroshima Hiroshima 739‐8526 Japan

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.12902

Reference183 articles.

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3. High-pressure phase relations in the system CaAl4Si2O11–NaAl3Si3O11 with implication for Na-rich CAS phase in shocked Martian meteorites

4. Structure and twinning of single‐crystal MgSiO3 garnet synthesized at 17 GPa and 1800°C;Angel R. J.;American Mineralogist,1989

5. BadjukovD. D. BrandstaetterF. KuratG. LibowitzkyE. andRaitalaJ.2005.Ringwoodite‐olivine assemblages in Dhofar 922 L6 melt veins (abstract #1684). 36th Lunar and Planetary Science Conference. CD‐ROM.

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