Horizontal thick bedded limestones of Palaeozoic Permian Maokou Formation that build the World wide known scenery Ashima （means a beautiful girl) stele in the Shilin(means stone forest) World Geopark, Yunnan, China. The writers got 5 rock samples from the inconspicuous place of the stele (being allowed by the Geopark), respectively from the base part, lower part, middle part, upper part and top part. More studies focus on the micro carbonates characteristics and the sedimentary environments. Finally the writers uncover the micro carbonates and the sedimentary environment of the whole stele, from the bottom to the top of this world wide known of Ashima stele. The base is made of high energy shoal facies of grey thick bedded grainstones with bioclasts and parallel beddings. That built Ashima’s feet. The lower part is made of middle energy shallow subtidal facies of grey thick bedded packstones with bioclasts of Fusulinida. That builds Ashima’s leg. The middle part is made of middle energy shallow subtidal facies of grey thick bedded packstones with intraclasts. That builds the Ashima’s waist. The upper part is made of middle energy shallow subtidal facies of grey thick bedded packstones with intraclasts and bioclasts, or bioturbation structure. That builds Ashima’s breast. The top is made of high energy shoal facies of grey thick bedded grainstones with intraclasts and bioclasts. That builds Ashima’s head. The carbonates contained amount of bioclasts, like foraminifera, trilobite, alga, Ostracoda, brachiopod, bryozoansea moss, Fusulinida, crinoid, bivalve. The sedimentary environments are high energy shoal and middle energy shallow subtidal.