Abstract: The correlation between lithostratigraphy and marker beds of the East Hill and West Hills, Taiyuan,Shanxi has been proposed by the authors according to the tripartite method. The formerly named "Luotuobozi Sandstones" now has been renamed as the "East Hill Sandstones" （K₈）.
The regressive palaeogeographic evolution has been recorded in the coal-bearing strata over 200 m thick. The Benxi Formation composed dominantly of black shales, lenticular limestones and thin coal beds with higher sulfur contents is interpreted as the littoral lacustrine sediments and tidally influenced lagoonal and bay sediments. From the Jinci Sandstones （K₁） upwards, there are gradations from lagoon and bay to fluvial-dominated shallow-water deltaic environments. In the Taiyuan Formation and the lower part of the Shanxi Formation, there are five deltaic cycles, each of which, about 20-30 m in thickness, was deposited in the order from bottom to top: limestones, black shales, siltstones, tabular cross-bedded sandstones, rhizoliths and coal seams,whereas in the Shanxi Formation, only abundant plant remains have been recognized. The channel sandstone facies are found to be interspersed with the lacustrine and flood-basin facies.
The estimates of hydrologic parameters such as flow velocity and flow amount of river water and the analysis of palaeogeomorphology were also made by the authors on the basis of the current theory on sedimentology and the data from measured sections. They may be well-concurred with the geological information. It is concluded that the quantitative geological analysis will be a stimulation to the study of sedimentary facies and palaeogeography.