The largest subsidence rate of the fault on the steep slope make Huoen area and Dongwu area, both locate on the northern abrupt slope to be sustained depocenters.
北部陡坡断层沉降速率大，使得该区霍恩和冬屋地区成为持续发育的沉积中心。
The largest subsidence rate of the fault on the steep slope make Huoen area and Dongwu area, both locate on the northern abrupt slope to be sustained depocenters.
北部陡坡断层沉降速率大，使得该区霍恩和冬屋地区成为持续发育的沉积中心。
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