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泥页岩中有机质-黏土复合体微结构研究进展
Research Advance on Microstructures of the Organic-Clay Composite in Mud Shale

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李晓霞 1   谷渊涛 1 *   万泉 2   杨曙光 2  
文摘 黏土矿物和有机质是泥页岩的两大重要组成部分,二者在沉积演化过程中形成的有机质-黏土复合体是油气生成的天然母质,对泥页岩中有机质的富集和保存有重要作用。目前关于泥页岩中有机质-黏土复合体的研究主要集中于有机质与黏土矿物的结合关系及黏土矿物对有机质生烃的催化作用。本文综述了有关泥页岩中有机质和黏土矿物的相互关系及黏土矿物对有机质生烃的催化作用和原理的研究成果,剖析了有机质-黏土复合体在热演化过程中的组成和结构特征。在此基础上,本文提出了目前尚待解决的科学问题,并就该研究未来的发展方向进行了展望。
其他语种文摘 Clay minerals and organic matters,two important components of mud shale,could form the organic-clay composite in mud shale during the sedimentary evolution. The organic-clay composite plays an important role in the hydrocarbon generation and the enrichment and preservation of organic matters in mud shale. Presently,studies about the organicclay composite in mud shale focused mainly on the relationship between organic matters and clay minerals,as well as the catalysis effect of clay minerals on the hydrocarbon generation from organic matters. By summarized previous studies,this paper briefly reviewed the relationship between organic matters and clay minerals in mud shale,discussed the catalysis effect of clay minerals on hydrocarbon generation from organic matters,and analyzed compositional and structural characteristics of the organic-clay composite during the thermal evolution. On this basis,several scientific problems,which are still to be solved,are put forward. In addition,we provide some suggestions for future researches in this research field.
来源 矿物岩石地球化学通报 ,2020,39(3):663-670 【核心库】
DOI 10.19658/j.issn.1007-2802.2020.39.029
关键词 泥页岩 ; 有机质-黏土复合体 ; 相互关系 ; 催化作用 ; 热演化
地址

1. 河南工程学院资源与环境学院, 郑州, 451191  

2. 中国科学院地球化学研究所, 矿床地球化学国家重点实验室, 贵阳, 550081

语种 中文
文献类型 综述型
ISSN 1007-2802
学科 地质学
基金 国家自然科学基金资助项目
文献收藏号 CSCD:6750515

参考文献 共 71 共4页

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