Clay mineralogy of sdiment core PS2172-1 in the Arctic Ocean
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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...
表征黏土矿物组的峰面积,采用Biscaye(1965)提出的校正因子,并基于黏土相关假设(原文未完整呈现该假设的具体内容),转换为相对黏土矿物百分比。



