Anders Meibom
Four heavily altered dark inclusions (4301-2, IV-1, 3b-1, IVa) in the Allende meteorite are composed exclusively of secondary minerals, including fayalitic olivine (Fa(40-45)), salitic pyroxenes (Fs(10-30)Wo(50)), nepheline, sodalite, and Fe-Ni sulfides. C ...
2000