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一、南京台场地概况南京台位于南京市中山陵风景区,属于紫金山南麓的丘陵地貌。地质构造处于南京一自来桥大断裂(NW向)东侧,长江破碎带(近EW向)南侧,茅山东侧大断裂(NE向)西侧。位于中山陵西沟断裂和老虎山西洼村断裂围成的断块上(图1)。现有体应变、短水准测量、地磁、地电、大地电场、ELF、测震等观测手段。
First, the Nanjing station site overview Nanjing station is located in Zhongshan City, Nanjing Sun Yat-sen scenic area, belonging to the southern foot of Purple Mountain landscape. The geological structure is located on the east side of the NW strike of the Bailan Bridge in Nanjing, south of the fault zone in the Yangtze River (near EW direction) and west of the large fault in the east of Maoshan (NE direction). It is located on the fault block enclosed by the Xiling fault in Zhongshanling and the Xiwacun fault in Tiger Mountain (Figure 1). The existing body strain, short leveling, geomagnetic, geoelectric, earth electric field, ELF, seismic measurements and other means of observation.