On Tectonic Genesis of Daobeiling in Jingxi Long'en Temple
The Daobeiling of Jingxi Long'en Temple in the Beijing Xiaoxishan Mountain is a small mountain range that runs northeast and is as steep as a wall.This paper explores the structural genesis of Daobeiling through geological structure,regional stratigraphy,lithology comparison,and geomorphologic trend.The study shows,in the late stage of the Yanshan Movement,underground magma intruded near the surface along the structural fissures of the Yanshan Movement,forming flow plastic bodies and squeezing towards the ground to form rock walls.Due to its relatively new formation age,the rock wall has a hard lithology and strong resistance to weathering,forming the ridge of Daobeiling.The study on the genesis of the Daobeiling structure hopes to provide useful references for the research on the formation reasons of similar terrain and landforms.
tectonic genesisgeological structureregional stratigraphygeomorphologic trendlithology correlationterrain and landform
万方数据
维普
