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“还原环境”是鉴别生油岩的主要指标之一;研究生油岩的氧化还原程度,就成为现今实验研究的任务。应用“高鉄,低鉄”此值或其某些系数如K_(Fe)、Kc划分原始沉积环境氧化还原程度,是石油地貭中常用的指标之一;但由于目前在选择溶矿用的盐酸浓度问题上,存在着极大的混乱,使得“高鉄、低鉄”实验分析成果的地貭解释及应用,可以呈现出错误的推断
“Reducing environment” is one of the main indexes to discriminate the source rock. The degree of redox of graduate oil rock becomes the task of present experimental research. It is one of the most commonly used indicators in petroleum geology to apply this value of “high 鉄 and low 鉄” or some of its coefficients such as K_ (Fe) and Kc to classify the redox status of the original sedimentary environment. However, Hydrochloric acid concentration problem, there is a great deal of chaos, making the “high 鉄, low 鉄” experimental analysis of the interpretation and application of ground 可 can show a wrong conclusion