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自1827年法国地质学家布朗尼尔特(Brangn-iart)提出“细碧岩”这一名称以来,围绕有关细碧岩的问题(如矿物成分、岩石化学特征、成岩地质环境及岩浆性质等)展开了长期的研究和争论。通过一百多年来各国地质学家的研究,上述问题已基本上得到解决,绝大多数的研究人员都认为细碧岩是玄武岩类的变种,它是在特定的地质环境(海底喷发)下形成的,常常与拉斑玄武岩共生,或成相互过渡关系,
Since the French geologist Brangn-iart proposed the name “small boulder” in 1827, the problems surrounding fine bijins (such as mineral composition, petrochemical characteristics, diagenetic geology, magmatic properties, etc.) ) Launched a long-term research and debate. The problems mentioned above have been basically solved by more than one hundred years of geologists’ studies. Most researchers consider that the diagenetic bimodal is a variant of basaltic rocks that is under certain geological conditions (submarine eruptions) Formed, often symbiotic with tholei basalt, or into a mutual transitional relationship,