High pressure minerals in the Château-Renard (L6) ordinary chondrite: implications for collisions on its parent body
Author:
Funder
UK Science and Technology Facilities Council
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/s41598-018-28191-6.pdf
Reference63 articles.
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2. Bischoff, A. & Stoeffler, D. Shock metamorphism as a fundamental process in the evolution of planetary bodies: information from meteorites. Eur. J. Mineral. 4, 707–755 (1992).
3. Beck, P., Gillet, P., El Goresy, A. & Mostefaoui, S. Timescales of shock processes in chondritic and martian meteorites. Nature 435(7045), 1071–1074 (2005).
4. Gillet, P. & El Goresy, A. Shock events in the Solar System: The message from minerals in terrestrial planets and asteroids. Ann. Rev. Earth Planet. Sci. 41, 257–285 (2013).
5. Chen, M., Sharp, T. G., El Goresy, A., Wopenka, B. & Xei, X. The majorite-pyrope plus magnesiowustite assemblage: constraints on the history of shock veins in chondrites. Science 271(5255), 1570 (1996).
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