论文部分内容阅读
本文对4块标样和4块现代生物及自然刻面作品的可溶有机物进行显微荧光光谱的测量分析表明：标样的荧光，随着苦环数的增多，λmax向长波移动；浮游植物、石孔莼等水生生物光谱峰在兰区，马尾范藻、柽柳叶等陆生植物光谱峰在红区；利用物质原始有机质的差异，用氯仿A的Amax与干酪极腐泥组关系图，可以进行生油岩类型的划分。
In this paper, four standard samples and four modern biological and natural faceted soluble organic matter measured by microscopic fluorescence spectroscopy showed that: the standard fluorescence, with the increase of bitter ring, λmax shift to the long wave; phytoplankton , Shikongsang and other aquatic biological peaks in Lan, Pseudostellaria, Tamarisk and other terrestrial plant spectral peaks in the red zone; the use of differences in the original organic matter, with chloroform A Amax and cheese polar saprolite group diagram, The type of source rock can be divided.