Clay mineralogy of sdiment core PS2185-4 in the Arctic Ocean

Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay...

将代表各类黏土矿物组的峰面积，借助比斯开（Biscaye）于1965年提出的因子转换为相对黏土矿物百分含量，转换过程中采用了黏土……的假设前提。