“…The crystalline structure of natural clay minerals and the corresponding hybrid pigments (Clay-IORs) were studied by XRD analyses (see Figure 1 ). The main crystal phase information of natural clay minerals, including IS [ 25 ], REC [ 26 ], KAO [ 27 ], MMT [ 28 ], VMT [ 29 , 30 ], SEP [ 9 ], HYS [ 31 ] and ILL was listed in Table S1 (see Supplementary Materials ). As can be seen from Figure 1 and Table S1 , the associated minerals, such as quartz (at 2 θ = 20.86°, 26.67°, 36.55°, 42.45°, 50.12°, 59.94° and 68.15°) [ 32 ], muscovite (at 2 θ = 8.81°, 17.78°, and 27.96°) [ 33 ], talc (at 2 θ = 9.49°, 18.66° and 28.65°) [ 30 ], biotite (at 2 θ = 10.56°) [ 29 ], dolomite (at 2 θ = 30.94°, 33.54°, 41.13°, 44.95°, and 50.53°), and calcite (at 2 θ = 23.05°, 29.39°, 35.98°, 39.42°, 47.50°, 48.50°, 56.58°, 57.42°and 60.99°) are present in the natural clay minerals.…”