The rocks of the Maykhan Khudug formation are thought to have been deposited as proximal to distal turbidites and folded and metamorphosed during the Variscan orogeny.

• 人们认为在华力西造山运动期间MaykhanKhudug群系岩沉积最接近远源浊积岩，并形成褶皱，且受变质。