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笔者通过云南罗茨年青褐煤(实为泥炭向褐煤的过渡)多样的凝胶化和丝炭化现象研究提出了以下的新观点以丰富经典理论:1)笔者认为凝胶化作用的最终产物在适当条件下均向炭丝化方向转化;2)把“凝胶化作用”概念广义化,认为只要存在着凝胶化和炭丝化组分的差异,凝胶化作用将一直进行下去,为此笔者把凝胶化作用划分为:初激,定凝和老化三个阶段;3)笔者认为在复水浅或流水状态下进行的“丝炭化作用”的概念值得商榷,一般地所谓氧化丝炭都要先经过一定程度的凝胶化作用,而后由于条件改变转化成丝炭化物质;4)由于气侯和环境的转变,致使在中新生代陆相煤系形成大量火焚丝炭。
The author puts forward the following new ideas to enrich the classical theory through the diversification of gelation and silk charcoalization of young lignite in Yunnan Roots (actually, the transition from peat to lignite): 1) The author believes that the final product of gelation is the appropriate Under the conditions of carbonization into the direction of transformation; 2) the concept of “gelation” generalized, that as long as there is a difference between gelation and carbonization components, gelation will continue, for which The author divides the gelation into three phases: primary shock, fixed coagulation and aging. 3) The author thinks that the concept of “silk charring” under shallow water or flowing water is worth discussing. Generally, the so-called oxidized charcoal All undergoes a certain degree of gelatinization before being converted into silk-charred material due to changes in conditions; 4) a large amount of fire-burning charcoal is formed in Meso-Cenozoic continental facies due to climate and environmental changes.