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c-axes in growth direction (“fascicular-optic”), (ii) such with converging c axes in growth direction (“radiaxialfibrous”) and (iii) such with uniform c-axes (“radialfibrous”). Following this classification, Neuser & Richter (2007) have presented oblong calcite crystals with converging and diverging c-axes in growth directions within stalagmites from caves located in dolostone host rock lithologies. Data obtained at these sites clearly documented that the Mg content of the drip waters is significant (Richter et al., 2011).

Radiaxial-fibrous and fascicular-optic Mg-calcitic cave cements: a characterization using electron backscattered diffraction (EBSD)