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地球学报  2006 

西天山山脉多期次隆升-剥露的裂变径迹证据

DOI: 10.3975/cagsb.2006.02.01

Keywords: 西天山,裂变径迹,隆升与剥露

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Abstract:

磷灰石的裂变径迹法已经广泛地应用于限定山脉的隆升剥露历史研究。天山山脉的隆升历史一直存在争议,西天山山脉的构造隆升研究则相对更为缺乏。野外系统采集三个横穿西天山察汗乌苏山剖面的花岗岩、火山岩等样品,挑选磷灰石开展了裂变径迹测试分析工作。测试结果表明,西天山可能存在多期次的构造隆升事件;进一步利用实测的磷灰石裂变径迹年龄数据和径迹长度,开展了磷灰石的温度时间反演模拟研究。模拟结果结合区域性的地质资料分析推断,西天山山脉自中生代以来存在4个阶段构造隆升剥露事件,分别为:三叠纪末—早侏罗纪(220~180Ma)、侏罗纪中期(170~140Ma)、白垩纪中期(110~80Ma)和晚新生代(24Ma以来)。

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