作者: G. Nehrke , P. Van Cappellen
DOI: 10.1016/J.JCRYSGRO.2005.11.080
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摘要: The morphology of vaterite aggregates framboidal structure built up smaller particles is described. It shown that the transformation into calcite occurs partly within aggregate, leading to much higher rates compared solid non-framboidal spherulites. from inside leads formation single crystal rhombs as observed for