In the Semail Nappe of Oman in the United Arb Emirates, silicified serpentinite was found. The occurrence of such geological features is rather unusual. It is a pseudomorphic alteration where the protolith of serpentinite was already silicified. Due to tectonic events, basal serpentinite was fractured and groundwater permeated along the faults, forming a large-scale circulation of groundwater within the strata. Through hydrothermal dissolution, silica precipitated and crystallized around the voids of serpentinite. Therefore, silicification can only be seen along groundwater paths. The silicification of serpentinite was formed under the condition where groundwater flow and carbon dioxide concentration are low.