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Figure 5 | Earth, Planets and Space

Figure 5

From: Aqueous alteration without initial water: possibility of organic-induced hydration of anhydrous silicates in meteorite parent bodies

Figure 5

Schematic image of proto-phyllosilicate formation on the olivine surface. a Dissolution of olivine into the organic fluid. Magnesite formation also proceeded. b Precipitation features cover the olivine surface. Etch pits evolved with the dissolution progress. These features were confirmed using SEM. c Flake-like particles evolved to a tubular structure, from amorphous to crystalline, in the precipitation features. These features were confirmed using TEM. d Formation of crystalline proto-phyllosilicates on the olivine surface

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