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1962年8月,作者等开始研究龙門山抝陷泥盆紀沉积岩的有机地球化学問題,其目的在于探討生物和有机貭对沉积岩地球化学过程的作用。本文根据工作第一阶段的部分結果,初步討論有机碳、氮和磷等生物元素分布的岩相地球化学規律及有关的成因問題。工作中承叶連俊教授热心指导和鼓励并审閱文稿,乐森璕教授和张守信同志代为鉴定化石,叶继蓀、潘均、王文琳、裴洁等同志分析样品,史书麟同志給以帮助,四川省地貭局地貭队热心协助,在此謹向他們表示感謝。
In August 1962, the author started to study the organic geochemistry of Devonian sedimentary rocks in the Longmen Shan depression. The purpose of this study was to explore the role of biological and organic rocks in the geochemical processes of sedimentary rocks. Based on some results of the first phase of the work, the paper discussed the laws of lithofacies geochemistry and the related genesis problems of the distribution of biological elements such as organic carbon, nitrogen and phosphorus. In the course of his work, Professor YE Lian-Jun was enthusiastic in guiding, encouraging and reviewing manuscripts. Professor Leshengwan and Comrade Zhang Shouxin took samples on behalf of fossils, Ye Jisun, Pan Jun, Wang Wenlin, Pei Jie and other comrades for analysis, and Shi Shulin comrades helped Sichuan Province The local team is very helpful and I hereby extend my thanks to them.