摘要
对江苏下古生界动物化石有机碎屑 (笔石、胞石和虫牙 )反射率进行系统研究的结果表明 ,它们与镜质组反射率有着极为相似的光性特征和变化规律 ,即随埋深的增加而增高 ,因而它们均可作为有机质成熟度指标 ;并进而以牙形刺色变指标 (CAI)为纽带 ,分别建立它们与镜质组反射率之间的良好对应关系 ,提出它们的成熟度划分标准 ,为它们的实际应用奠定基础。
The reflectances of zoolite organic debris(including graptolites,chitinozoans and scolecodonts) from Lower Paleozoic in Jiangsu are well studied in this paper.The results show that they have extremely similar optical properties and variational regularities with vitrinite reflectances,that is,their reflectances increase with increasing of depth,thus,they all can be served as good indexes of organic maturity.Furthermore,the correlations between them and vitrinite reflectances are established respectively by using conodont CAI as a link,therefore,the criteria of their maturity are given,which has laid the foundations for their actual application.
出处
《古生物学报》
CAS
CSCD
北大核心
2000年第4期548-552,共5页
Acta Palaeontologica Sinica
基金
中国科学院古生物与古人类学特别支持费
国家自然科学基金委特殊学科点人才基金
关键词
古生物
化石碎屑
有机质成熟度
下古生界
烃源岩
conodont CAI, zoolite organic debris, reflectance, organic maturity, Lower Paleozoic, Jian8
