论文部分内容阅读
对湖泊沉积物磁性矿物的来源及其鉴别方法进行了较为深入系统的分析, 发现不同湖泊沉积物的磁学参数具有不同的气候响应过程. 提出为了恢复古气候和古环境的变化过程, 详细的岩石磁学和土壤磁学研究是认识湖泊沉积物磁学性质及其环境意义的基础.
The origin and identification methods of magnetic minerals in lacustrine sediments are systematically analyzed in depth and it is found that the magnetic parameters of sediments in different lakes have different climate response processes.It is proposed that in order to restore the paleoclimate and paleoenvironmental changes, Rock magnetism and soil magnetism research are the basis for understanding the magnetic properties of lake sediments and their environmental significance.