Fig. 4From: Spatiotemporal patterns of sediment deposition on the northern slope of the South China Sea in the last 150,000 yearsVariations in clay mineral assemblage, illite chemical index, illite crystallinity, smectite/(illite + chlorite) and kaolinite/(illite + chlorite) from site DLW3101. The pink bar highlights the deglacial period. MIS: Marine isotope stageBack to article page