Drilling in fractured formations poses a substantial challenge due to mud loss, which not only impedes operations but also leads to substantial costs and delays. Effectively controlling mud loss is crucial for efficient drilling. However, determining the appropriate mud additive to minimize mud loss in fractured formations requires further investigation. This is because proper mud additives can assist in sealing fractures, preventing wellbore instability issues and minimizing formation fluid influx. This study aims to investigate mud loss in fractured porous media by evaluating three additives' performance using an experimental setup that provides different fracture apertures. This setup provides an accurate simulation of down-hole static filtration at high pressure/temperature by flowing pressurized mud through fractured porous media and measuring effluent under different scenarios. The particular focus is on preformed particle gel (PPG), walnut shell, and shell additives. The study examines the effects of these additives, their particle sizes, and their mixture effect on mud loss. An optimal concentration of 8000 ppm of PPG, as well as larger particle sizes (mesh No.200) of walnut shell and shell, are found to be more effective in controlling mud loss, reducing mud loss by 34.4%, 110%, and 20.85%, respectively, compared to the base mud. The results reveal that when mud contains only one additive, the walnut shell is the most effective, reducing the volume of mud loss from 394.2 cc to 150.2 cc, while a mixture of PPG-shell-base mud at elevated temperatures represents the highest performance of additive combinations. The PPG-shell-base mud significantly reduces mud loss from 394.2 cc to 115 cc and 27.8 cc at 50 °C and 80 °C. In conclusion, this research not only contributes valuable insights to the field but also offers practical recommendations for the use of additives to effectively control mud loss during drilling operations in fractured formations, ultimately improving drilling efficiency and cost-effectiveness.