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地质论评  2001 

地质事件、序列和事件群

Keywords: 地质事件事件序列事件年代格架事件群造山带构造事件变质岩

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Abstract:

在前寒武纪变质基底和造山带中,由于多期热-构造事件的影响,以及透入性片理和构造岩的发育,造成变质深成侵入体,构造岩和表壳岩鉴别的困难,。即使表壳岩系统也因强烈的变形而不能够完全运用叠置地层学的方法进行地层划分和对比,因而事件地质学的思路和方法的应用颇为广泛。地质事件是地史演化过程中,不同于正常地质历史发展的突发性,或灾变性,或具有特殊意义的地质记录,在正确识别地质事件的性质和特征的基础上,需建立地质事件的序列,事件序列的建立包括两个步骤,首先要在野外翔实的工作基础上建立地质事件的相对序列,然后在此基础上运用多元同位素测年方法标定主要或特征地质事件的时代,建立地质事件的年代格架。地质事件群或组合则是成因上有联系,空间上相匹配,时间上有先后的一组地质事件,它比单独的一个事件更深刻地反映地质历史演化的过程和特点,正确归并和界定地质事件群在研究区域地质演化特征或进行大区域间的地质对比时具有十分重要意义。

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