Copy the page URI to the clipboard
Mittlefehldt, D. W.; Barrett, T. J.; Le, L; Peng, Z. X.; Berger, E. L. and Ross, D. K
(2018).
URL: https://www.hou.usra.edu/meetings/lpsc2018/pdf/270...
Abstract
Most asteroidal igneous rocks are eucrite-like basalts and gabbros, composed mostly of ferroan low- and high-Ca pyroxenes and calcic plagioclase, plus smaller amounts of silica (most commonly tridymite), ilmenite, chromite, troilite, Ca-phosphate, metal and sometimes ferroan olivine. Eucrite-like mafic rocks are fragments of the crusts of differentiated asteroids, and most are likely from 4 Vesta.