Reverse time migration (RTM) as a two-way wave equation method models all types of wave without any dip limitation. This is very important regarding the drawbacks of ray-based and one-way wave equation imaging methods in properly imaging the complex geological media. Despite the above superiorities, low frequency artifacts especially in large reflection angles (60 to 90 degree) are the main drawback of RTM which cover and reduce the migrated image quality. Therefore, the aim of this paper is to improve the imaging condition as the heart of RTM to suppress the low frequency artifacts and use the useful information of the large reflection angle domain (60 to 90 degree) and produce a high quality image. This was achieved by presenting a new imaging condition including a weighted function based on the reflection angles. Finally, the RTM results using the new proposed imaging condition was presented and compared with the results of some conventional and modern similar methods.