檢視交错层理的原始碼

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中文名: 交错层理

外文名: Cross bedding

形成原因: 由沉积介质的流动造成的

分 类: 板状，楔状，槽状

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'''交错层理'''通常也称为斜[[层理]]。它是由一系列斜交于层系界面的纹层组成，斜层系可以彼此重叠、交错、切割的方式组合。其特点是细层理大致规则地与层间的分隔面（主层理）呈斜交的关系，上部与主层理截交，下部与主层理相切。可以利用斜层理的倾向了解[[沉积]]物的来源方向。<ref>[https://wenku.baidu.com/view/7ab3868650e2524de4187e0c.html 交错层理  ],百度 , 2014-09-01</ref>