Shestopalov D. I., Golubeva L. F., McFadden Lucy-Ann A., Fornasier Sonia, Taran M. N.
Titanium-bearing pyroxenes of some E asteroids: Coexisting of igneous and hydrated rocks
Planetary and Space Science, 2010, vol. 58, pp. 1400-1403
Référence DOI : 10.1016/j.pss.2010.06.012
Référence ADS : 2010P&SS...58.1400S
Résumé :
In this paper, we present arguments for the presence of optically active Ti <SUP>3+</SUP> in the structure of low iron pyroxenes to explain the strong 0.49-mum absorption band in spectra of E[II] asteroids. Such an interpretation supports the idea that E asteroid material is formed at high temperature in a strongly reducing medium. We also discuss the possibility of high temperature and hydrated rocks coexisting on some E asteroids. Our discussion is based on the idea of collisional evolution of aubrite parent bodies that was presented by Keil (1989).