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Fig. 4 | Earth, Planets and Space

Fig. 4

From: The layered structure model for winonaite parent asteroid implicated by textural and mineralogical diversity

Fig. 4

Modal abundance (by area %) variation of the major phases in the winonaites (Table 1). They are orthopyroxene (Opx), olivine (Ol), plagioclase (Pl), clinopyroxene (Cpx), troilite (Tro), and metal (including the Fe-rich weathering products produced from metal and troilite). The color symbols represent the studied winonaite samples. The light gray symbols represent the reported data for other winonaites (see Table 1)

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