Clay mineralogy of sdiment core PS2179-3 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 fraction consists only of clay minerals采用Biscaye于1965年提出的校正因子，将代表黏土矿物组的峰面积转换为相对黏土矿物（clay mineral）百分含量，其假设前提为黏土级组分（clay fraction）仅由黏土矿物构成。