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本文通过对东秦岭地区古生代以来断裂带活动特征的分析,阐明该构造带是属于地中海型断裂式多期构造活动带的基本观点。
Based on the analysis of the activity characteristics of the fault zone since the Paleozoic in the East Qinling Mountains, this paper clarifies that the tectonic belt belongs to the basic view of the Mediterranean type fault multi-stage tectonic activity belt.