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硼的地球化学研究已有四十年的历史。这项研究工作的首倡者是B.库尼茨(Куниц),因为在他的卓越的综合报告中,在全面分析地壳中各种硼矿成矿作用的基础上,定性地论述了硼在自然界演化过程中的行为特征,确定了导致不同成分硼矿物形成及其沉积序列的基本因素,正确认识了岩浆活动对硼的分散、迁移所起的作用。В.М.戈尔德施密特和克尔-别捷尔斯(Кл-Петерс)则从定量方面研究了硼在自然界的行为,并确定了硼在各种地质形成物中的分布特点。他们的研究成果得到了А.Е.费尔斯曼院土的充分肯定,并把这些成果列为硼的地球化学基本原理。
The geochemical study of boron has a history of forty years. The initiator of this research was B. Куниц, because in his excellent synthesis report, on the basis of a comprehensive analysis of various mineralization of boron in the earth’s crust, the qualitative description of boron in nature The behavioral characteristics of the evolution process determine the basic factors leading to the formation and deposition sequence of boron minerals of different compositions and correctly understand the role of magma activity in the dispersion and migration of boron. В.М. Golderschmidt and Кл-Петерс studied the behavior of boron in nature quantitatively and determined the distribution of boron in various geological formations. Their research results have been fully affirmed by А.Е. Felssman’s court, and these achievements are listed as basic principles of boron geochemistry.