因此,可以通过联合地貌面的级数确定断块隆升的期次,并通过阶地的年代推断断块隆升的起始时间。
Therefore the fault-block uplifting stages can be determined from the steps of unified geomorphic surfaces, and the starting time of uplifting can be deduced from the age of terraces.
因此,可以通过联合地貌面的级数确定断块隆升的期次,并通过阶地的年代推断断块隆升的起始时间。
Therefore the fault-block uplifting stages can be determined from the steps of unified geomorphic surfaces, and the starting time of uplifting can be deduced from the age of terraces.
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