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本文研究和应用我国现有的海绿石资料,叙述了海绿石在时代上与平面上的分布特点;讨论了现代与古代海绿石矿物学特征的变化,并探讨自生海绿石在其形成后晶体结构有着从无序向有序转化的过程,也是海绿石埋藏后逐渐成熟的过程;在总结现代和古代海绿石形成环境的基础上,指出海绿石含量,形态及其伴生矿物组合的变化,可作为判别沉积相的依据之一.而海绿石含量上的规律递增,又可能指示海侵过程.
This paper researches and applies the existing information of glauconite in our country, narrates the distribution characteristics of glauconite in time and in the plane, discusses the mineralogical characteristics of modern and ancient glauconite, After the formation of the crystal structure from disorder to orderly transformation process, but also the gradual maturity of the process of burial of glauconite; summarize the formation of modern and ancient glauconit on the basis of that the content of glauconite, morphology and its associated The change of mineral assemblage can be used as one of the evidences for determining sedimentary facies, while the regularity of the content of glauconite increases, which may indicate the transgression process.