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This study is focused on the mineralogical and chemical compositions,deposition environment andmechanism of formation of sediments of Kyzyltokoy basin.By an interpretation of formation,anenvironment of sedimentation of a basin was separated into three general conditions:a condition whereglauconitization process interrupted,where process reached a completion and where occurred decay ofglauconites,i.e.,the beginning and interruption in the middle of glauconitization,completion of the processand decaying of the mineral.