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. Author manuscript; available in PMC: 2021 Jan 15.
Published in final edited form as: Geochim Cosmochim Acta. 2020 Jan 15;269:639–660. doi: 10.1016/j.gca.2019.10.042

Figure 2.

Figure 2.

(a, b) BF STEM images of the CAI mantle edge composed of oriented gehlenite with minor fine-grained inclusions of hibonite and grossite. An inset in (a) is electron diffraction patterns of melilite view down the [130] zone axis, whereas an inset in (b) is electron diffraction patterns of grossite view down the [3¯1¯2] zone axis. (c) Compositional profile across a single melilite crystal in the CAI mantle, obtained using EPMA. The traverse was obtained along the elongation direction of the melilite crystal with a spacing of 2 μm between points. See Figure 1 for the location of the traverse line. Abbreviation: grs = grossite.