Fig. 6
From: Using Mg isotopes to constrain the formation temperature of dolomite

Origin model of different dolostones. (A) Micro-fine crystal dolostone (D1); (B) Fine-medium crystal dolostone (D2); (C) Medium-coarse crystal dolostone (D3).
From: Using Mg isotopes to constrain the formation temperature of dolomite
Origin model of different dolostones. (A) Micro-fine crystal dolostone (D1); (B) Fine-medium crystal dolostone (D2); (C) Medium-coarse crystal dolostone (D3).