Clay mineralogy of sdiment core PS2187-5 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...代表黏土矿物组的峰面积，借助Biscaye于1965年提出的校正因子，并基于黏土相关假设（原文未完整阐述该假设的具体内容），转换为相对黏土矿物百分含量