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地质论评  2009 

鲁西古生代碳酸盐岩中的垂直缝合线及其在华北板块构造演化中的意义

Keywords: 华北东部,碳酸盐岩,垂直缝合线,水平挤压,构造演化

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Abstract:

笔者在山东省淄博市博山区中奥陶统马家沟群白云岩和上石炭统本溪组石灰岩中识别出垂直缝合线。垂直缝合线都借助于平面X剪节理发育,缝合面上的“牙齿”与缝合面本身多呈斜交状态,其延伸方向代表着变形期最大主压应力轴(σ1)方向。根据垂直缝合面“牙齿”的突出方向判别:以山东博山地区为代表的华北东部地区在古生代中期和末期先后两次受到NNE―SSW方向的水平挤压作用。其中第一次挤压事件与遍布华北东部的中奥陶统―上石炭统(C2―O2)平行不整合抬升相关,而第二次则与华北东部古生代末期的褶皱隆起相联系。本文的研究为垂直缝合线在盆地构造演化研究中的应用提供了良好的研究实例。

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