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地质学报  2004 

新疆北部中二叠统烃源岩地球化学特征与沉积环境

, PP. 534-541

Keywords: 烃源岩,地球化学,中二叠统,新疆北部

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Abstract:

首次对新疆北部准噶尔、吐哈及伊犁盆地中二叠统碳酸盐岩类、泥岩类烃源岩的微量元素、稀土元素和有机地球化学丰度进行了系统分析,其主要特征是微量元素含量与同类岩石的克拉克值相比,有的较高,有的偏低;轻稀土富集程度较高,重稀土相对较低,Ce/Ce*具有较明显的正异常,反映出烃源岩沉积环境总体为还原环境。有机地球化学分析证实,烃源岩中微量元素含量对沉积水体中生物的分布有一定的影响,部分微量元素丰度与有机质含量呈明显的正相关关系。还原程度强的沉积相带是原始有机质沉积的良好场所,沉积有机质能及时沉积、保存,烃源岩大多有机质丰度高;反之,则明显变差

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