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拓木岩溶塌陷分布在漓江Ⅰ级阶地与河漫滩的结合部位,受NW向和NE向断裂控制,岩溶塌陷成因以振动致塌和冲爆致塌为主,直接的诱发原因是炸礁爆破的振动作用。
The extension of Tuokou karst collapse is located at the junction of grade Ⅰ terraces and river floodplains in the Lijiang River and is controlled by the NW and NE faults. The causes of karst collapse are dominated by vibration and impulse explosion, and the direct cause is the vibration of the reef explosion effect.