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地质学报  2003 

燕山及邻区晚白垩世以来山脉隆升历史的低温热年代学证据

, PP. 399-406

Keywords: 燕山晚白垩世山脉隆升低温热年代学裂变径迹夷平面地壳均衡

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Abstract:

本文根据以裂变径迹测年为主的低温热年代学方法,认为燕山及邻区在晚白垩世进入区域性伸展构造环境以来经历了造山带伸展裂解引发的6次强烈差异升降运动,分别发生在120~105Ma、95~85Ma、60~50Ma、38Ma左右、25~20Ma和10~5Ma,造成燕山及邻区约7~8km的剥蚀量。而在相邻两次强烈差异升降运动期之间的相对构造稳定期,则形成了燕山―太行山地5期夷平面以及周缘盆地多期沉积间断。燕山与邻区盆地之间晚中新世以来的快速差异升降运动导致燕山及邻区现今盆―山构造―地貌格局。

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