Clay mineralogy of sdiment core PS2186-3 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...
通过采用比斯开(Biscaye)1965年提出的因子,并基于黏土……的假设,将表征黏土矿物组的峰面积转换为相对黏土矿物百分含量。



