Sequence stratigraphy and metre-scale cyclicity of Neoarchean dolomite
The strata around the ore is generally very strongly silicified (visible in thin section) and the host rock dolomite heavily altered from fine-crystalline planar to medium and coarse crystalline planar and nonplanar dolomite (Baugaard, 2002; dolomite classification of Sibley and Gregg, 1987). The ore associated with the breccia is …