Clay mineralogy of sdiment core PS2177-3 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 fraction consists only of clay minerals. Smectite, illite, kaolinite and chlorite by area, kaolinite/chlorite by intensity
创建时间：
2025-11-18
