A vacancy‐rich, partially inverted spinelloid silicate, (Mg,Fe,Si) 2 (Si,□)O 4 , as a major matrix phase in shock melt veins of the Tenham and Suizhou L6 chondrites-Reference-Cited by-同舟云学术

A vacancy‐rich, partially inverted spinelloid silicate, (Mg,Fe,Si) 2 (Si,□)O 4 , as a major matrix phase in shock melt veins of the Tenham and Suizhou L6 chondrites

Published:2019-07-07 Issue:9 Volume:54 Page:1907-1918
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Ma Chi¹^ORCID,Tschauner Oliver²^ORCID,Bindi Luca³⁴,Beckett John R.¹,Xie Xiande⁵⁶

Affiliation:

1. Division of Geological and Planetary Sciences California Institute of Technology Pasadena California 91125 USA

2. Department of Geoscience University of Nevada Las Vegas Nevada 89154 USA

3. Dipartimento di Scienze della Terra Università degli Studi di Firenze Via G. La Pira 4 I‐50121 Firenze Italy

4. CNR Istituto di Geoscienze e Georisorse Sezione di Firenze Via G. La Pira 4 I‐50121 Firenze Florence Italy

5. Key Laboratory of Mineralogy and Metallogeny Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou 510640 China

6. Guangdong Provincial Key Laboratory of Mineral Physics and Materials Chinese Academy of Sciences Guangzhou 510640 China

Funder

Division of Earth Sciences

National Science Foundation

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.13349

Reference49 articles.

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2. Shenzhuangite, NiFeS2, the Ni-analogue of chalcopyrite from the Suizhou L6 chondrite

3. Discovery of the Fe-analogue of akimotoite in the shocked Suizhou L6 chondrite

4. Synthesis of inverse ringwoodite sheds light on the subduction history of Tibetan ophiolites

5. Ringwoodite, Natural (Mg,Fe)2SiO4 Spinel in the Tenham Meteorite

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