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应用构造地貌的观点 ,把太原盆地及其边缘地貌分为 :外围断块抬升山地、抬升轻微的丘陵台地、山前堆积的洪积倾斜平原和沉降堆积的冲积平原 4种地貌单元。通过对边缘地貌形态、地震活动特点、水系演变规律以及古河道发育、新生代沉积厚度等特征分析 ,太原盆地新构造运动的特点为 :(1)盆地西部上升强烈、东部隆起较弱。 (2 )在整体上升过程中 ,构成两个隆起中心。盆地西部以石千峰为隆起中心 ,向南隆起幅度减小 ;盆地东部以绵山为隆起中心 ,向北隆起幅度减小。 (3)整个盆地新构造运动具有中心对称性。此外还论述了边缘地貌、新构造断裂及古河道的控水作用及其在水文地质方面的应用
From the viewpoint of tectonic landform, the Taiyuan Basin and its marginal landform are divided into four types: alluvial plain alluvial plain with peripheral fault block uplifting, slightly uplifting hilly platform, alluvial plain piedmont and alluvial plain. Based on the characteristics of marginal landforms, seismogenic activities, evolution of water system, paleokaryo development and Cenozoic sedimentary thickness, the characteristics of neotectonic movement in Taiyuan basin are as follows: (1) The western part of the basin rises strongly and the eastern part rises slightly. (2) During the whole ascending process, two bulge centers are formed. The western part of the basin takes Shiqianfeng as the uplift center and the south uplift amplitude decreases. In the eastern part of the basin, the Mianshan uplift center decreases toward the north. (3) Cenozoic symmetry of neotectonic movement in the whole basin. In addition, it discusses the marginal landform, the neotectonic rupture and the water control action of ancient rivers and their application in hydrogeology