碳酸盐岩烃源岩有机岩石学特点和有机组分分类

ORGANIC PETROLOGICAL CHARACTERISTICAS AND ORGANIC CONSTITUENTS CLASSIFICATION OF CARBONATE SOURCE ROCKS

采用反光、透光、荧光和透射电镜相结合，全岩光片和干酪根光片相对比的有机岩石学方法，对我国不同时代碳酸盐烃源岩有机岩石学特点和有机组分特征进行了分析，并提出碳酸盐烃源岩有机组分分类。

A series of Chinese carbonate source rock in different geologic periods fromTarim basin,Ordos basin,the east part of North China and Shichuan basin were anal yzed todocument their organic petrological character and organic constituents composition. Theorganic petrological analysis procedures include that microscopy in incident light,transmittedlight and fluorescence mode may be combined with transmitted electron microscopy,and thepolished section of whole rock be co-ordinated with polished pellet of kerogen concentrate.The maceral, submaceral and submicromaceral in the whole rock and in kerogen concentratesare described and classified.