supported by the National Natural Science Foundation of China (40925008 and 91128206);the National Basic Research Program of China(2007CB815906)
Variability of clay mineral assemblages in the Western Pacific Warm Pool(WPWP) over the past 370 ka shows the prominent glacial-interglacial cyclicity.Smectite(62%-91%) is the dominant clay mineral,with decreased cont...
supported by the National Natural Science Foundation of China (40925008, 40876024 and 40776027);the National Basic Research Program of China (2007CB815906);the Program of Shanghai Subject Chief Scientist (10XD1406300)
High-resolution grain size and major element geochemical measurements were performed on the marine sediments of Core MD05-2895 to help understand the formation of turbidite sequences. Grain-size results show that thes...
supported by National Natural Science Foundation of China (Grant Nos. 40925008,40876024,and 40776027);National Basic Research Program of China (Grant No. 2007CB815906);Shanghai Shuguang Program (Grant No. 07SG23);Shanghai Subject Chief Scientist Program (Grant No. 10XD1406300)
Weathering products of silicate rocks are particularly useful for evaluating the continental chemical weathering on the Earth's surface and its mechanism.Clay mineralogy and major-element geochemistry of surface sedim...
supported by the National Natural Science Foundation of China (40925008,40876024 and 40776027);the National Basic Research Program of China (2007CB815906);the Shanghai Shuguang Program (07SG23);the Shanghai Subject Chief Scientist Program (10XD1406300)
High-resolution clay mineralogical analysis of Core MD05-2904 in the northern South China Sea(SCS) covering the period since the Last Glacial Maximum shows that illite(29%-48%),smectite(14%-45%),chlorite(17%-28%),and ...