This paper, based on the grain size data of drilling cores in Kunming basin, analyzes the grain size trend curve, grain size parameters, possibility accumulative curve, discusses the evolution of the Quaternary sedimentary environment in Kunming basin. The work reveals that the early Pleistocene is fluvial facies—lake facies, the middle Pleistocene is lake facies—shallow lake facies—lake facies—fluvial facies, and since the late Pleistocene is fluvial facies—lake facies—shallow lake facies—lake facies—fluvial facies.