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. Author manuscript; available in PMC: 2019 Mar 29.
Published in final edited form as: Acta Geogr Geol Meteorol Debr Geol Gemorfol Termeszfoldr Sor. 2018 Nov 29;246:419–435. doi: 10.1016/j.gca.2018.11.002

Figure 2:

Figure 2:

Backscattered electron images of textural occurrences of secondary fayalite in Kaba. chr = chromite;fa = fayalite; hed = hedenbergite; mes = mesostasis; mgt = magnetite; ol = ferromagnesian olivine; sf= sulfide. Fayalite associated with magnetite, hedenbergite, and sulfides (a, b) replaces Fe,Ni-metal nodules in type I chondrules, (c, d) forms veins crosscuttingfine-grained rims around chondrules, (e) overgrowths chondrule olivines, and (f) occurs as euhedral grains in the matrix.