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一、前言笔者在分析我国某一盆地的一个钻井剖面的样品中;以及在第三纪、三叠纪、二叠纪、奥陶纪、寒武纪和震旦纪碳酸盐岩和其它地层中,发现了一种新的有机色素。它主要存在于含氧、氮和硫的非烃馏分中。纯化合物呈橙红色。在硅胶薄板上很稳定,长期暴露于空气中其颜色仍清晰不变,是普遍存在于天然地质样品中的一种色素物质,在石油勘探上有着实际和理论意义。因此,引起笔者的注意。对它进行了多种测试和研究。
I. INTRODUCTION The author is analyzing samples of a well section in a certain basin in China; and in the third, Triassic, Permian, Ordovician, Cambrian and Sinian carbonate and other strata In the discovery of a new organic pigment. It is mainly found in non-hydrocarbon oxygen, nitrogen and sulfur fractions. The pure compound is orange-red. Silicone sheet is very stable, long-term exposure to the air its color is still clear, is common in natural geological samples of a pigment material, the oil exploration has practical and theoretical significance. Therefore, the author’s attention. It conducted a variety of tests and research.