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基于年代学约束的白马雪山晚第四纪冰川作用

DOI: 10.11928/j.issn.1001-7410.2015.01.03, PP. 29-37

Keywords: 白马雪山,ESR测年,冰期系列,冰川地貌

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Abstract:

白马雪山(5429m)地处横断山脉腹地,海拔3800m以上保存着确切的第四纪冰川遗迹,对其进行深入研究,可以为重建西南季风影响区的环境演变历史以及区域冰期-间冰期系列对比提供依据。本文采用野外地貌调查与电子自旋共振测年(ESR)相结合的方法,查明白马雪山第四纪冰川发育的地貌特点,并对研究区的冰期系列进行划分。结果显示,白马雪山晚第四纪以来至少发生5次冰川作用,分别为中梁赣冰期(475±62ka,MIS12);倒数第二次冰期(MIS6),年代分别为166±22ka、142±17ka、209±23ka、153±15ka、120±16ka和180±20ka;末次冰期早期(MIS4),年代分别为57±6.8ka、67±8.7ka、81±11ka、77±11ka和64±7.7ka;末次盛冰期(19±2.5ka,LGM,MIS2)以及全新世新冰期/小冰期(MIS1)。研究区的冰川作用与青藏高原的脉动式抬升具有一定的对应关系。

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