Clay mineralogy of sdiment core PS2161-1 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...通过运用比斯凯（Biscaye）1965年提出的因子，将表征黏土矿物族的峰面积转换为相对黏土矿物百分含量，该转换以黏土[原文未完整表述的假设条件]为前提。