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. Author manuscript; available in PMC: 2015 Jul 28.
Published in final edited form as: RSC Adv. 2015 Mar 27;5:36614–36633. doi: 10.1039/C4RA17180B

Fig.1.

Fig.1

Two HAp crystals of mineralogical origin: one with the exposed (001) face (left) and the other one with the (001) face being overgrown by the (011) and (101) planes as the result of its preferred growth on the account of the stagnation of the adjacent planes (right). Reprinted with permission from Ref.78.