High-pressure minerals in eucrite suggest a small source crater on Vesta

Author:

Pang Run-Lian,Zhang Ai-Cheng,Wang Shu-Zhou,Wang Ru-Cheng,Yurimoto Hisayoshi

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Reference51 articles.

1. Melosh, H. J. Impact Cratering: A Geological Process. (Oxford Univ. Press, 2009).

2. Melosh, H. J. The contact and compression stage of impact cratering. In Impact Cratering: processes and products. (eds Osinski, G. R. & Pierazzo, E. ) 32–42 (Wiley-Blackwell, West Sussex, 2013).

3. Chen, M., Sharp, T. G., El Goresy, A., Wopenka, B. & Xie, X. The majorite-pyrope + magnesiowüstite assemblage: constraints on the history of shock veins in chondrites. Science 271, 1570–1573 (1996).

4. Sharp, T. G. & DeCarli, P. S. Shock effects in meteorites. In Meteorites and the Early Solar System II. (eds Lauretta, D. S. & McSween, H. Y. ) 653–677 (University of Arizona Press, 2006).

5. Gillet, P., El Goresy, A., Beck, P. & Chen, M. High pressure mineral assemblages in shocked meteorites and shocked terrestrial rocks: mechanisms of phase transformations and constraints to pressure and temperature histories. In Advances in High-Pressure Mineralogy. (ed Ohtani, E.) Geol Soc Am Special paper 421, 57–82 (2007).

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