Fine‐structures of planar deformation features in shocked olivine: A comparison between Martian meteorites and experimentally shocked basalts as an indicator for shock pressure-Reference-Cited by-同舟云学术

Fine‐structures of planar deformation features in shocked olivine: A comparison between Martian meteorites and experimentally shocked basalts as an indicator for shock pressure

Published:2019-07-21 Issue:9 Volume:54 Page:1990-2005
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Takenouchi Atsushi¹²^ORCID,Mikouchi Takashi³,Kobayashi Takamichi⁴,Sekine Toshimori⁵⁶,Yamaguchi Akira¹⁷^ORCID,Ono Haruka⁸^ORCID

Affiliation:

1. National Institute of Polar Research (NIPR) 10‐3 Midori‐cho Tachikawa Tokyo 190‐8518 Japan

2. Department of Basic Science The University of Tokyo 3‐8‐1 Komaba Meguro‐ku Tokyo 153‐8902 Japan

3. The University Museum The University of Tokyo 7‐3‐1 Hongo Bunkyo‐ku Tokyo 113‐0033 Japan

4. National Institute for Materials Science (NIMS) 1‐1 Namiki Tsukuba Ibaraki 305‐0044 Japan

5. Center for High Pressure Science and Technology Advanced Research (HPSTAR) 1690 Cailun Rd Pudong Shanghai 201203 P.R. China

6. Graduate School of Engineering Osaka University 2‐1 Yamadaoka Suita Osaka 565‐0871 Japan

7. Department of Polar Science School of Multidisciplinary Science SOKENDAI (The Graduate University for Advanced Studies) Tachikawa Tokyo 190‐8518 Japan

8. Department of Earth and Planetary Science The University of Tokyo 7‐3‐1 Hongo Bunkyo‐ku Tokyo 113‐0033 Japan

Funder

Japan Society for the Promotion of Science

National Institute of Polar Research

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.13367

Reference46 articles.

1. Electron petrography of shock-deformed olivine in stony meteorites

2. BauerJ. F.1979.Experimental shock metamorphism of mono‐ and polycrystalline olivine: A comparative study (abstract). Proceedings of 10th Lunar and Planetary Science Conference. pp.2573–2596.

3. Timescales of shock processes in chondritic and martian meteorites

4. EXPERIMENTAL ANALYSIS OF FRACTURE PATTERNS

5. Dynamic compression of an Fe–Cr–Ni alloy to 80 GPa

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