New results of field investigations show that the eastern Liupanshan piedmond fault is an active reverse fault zone since late Quaternary.
新的野外调查研究结果表明，六盘山东麓断裂是一条第四纪以来的活动逆断裂构造带。
New results of field investigations show that the eastern Liupanshan piedmond fault is an active reverse fault zone since late Quaternary.
新的野外调查研究结果表明，六盘山东麓断裂是一条第四纪以来的活动逆断裂构造带。
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