摘要
Boron isotopic geochemistry is a new research field, which began to be developed in the mid-late 1980s. It deals with many aspects, such as seawater and oceanic crust, marine and non-marine evaporate borates, lavas, massive sulfide deposits, thermal-water system, and the recent saline lakes. We began to carry out the geochemical research on boron isotopes in those lakes at that time as well. However, such an investigation on boron isotopic geochemistry for the common lakes like the Qinghai
基金
Project supported by the National Natural Science Foundation of China