Supp Figure 1: Revisiting Ediacaran to early Cambrian depositional history of the western North China: Did it remain passive until mid-Paleozoic?

Appendix Figure 1. Representative photomicrographs (cross-polarized light) for sampled selected for detrital zircon U-Pb analyses. Sample locations are shown in Figure 2. (a) Sample S002 from the Hangqikou Formation at the Huating Section. (b) Sample QLSLQ from the Luoqan Formation at the Qinglongshan Section. (c) Sample YSX-1 from the Luoqan Formation at the Yinshixia Section. (d) Sample QLSHW from the Suyukou Formation at the Qinglongshan Section. (e) Sample YSX-3 from the Suyukou Formation at the Yinshixia Section. (f) Sample SYSX-7 from the Mantou Formation at the Yinshixia Section. Qtz, quartz grain; Kfs, K-feldspar; Lv, Volcanic lithic fragement; Ls, Sedimentary lithic fragment

Supp Table 1: Revisiting Ediacaran to early Cambrian depositional history of the western North China: Did it remain passive until mid-Paleozoic?

Supplementary Table 1. Laser ablation inductively coupled plasma spectrometry (LA-ICP-MS) data for detrital zircons of Statherian and Cambrian sandstones from the western North China Block

Supp Table 1: Revisiting Ediacaran to early Cambrian depositional history of the western North China: Did it remain passive until mid-Paleozoic?

Supplementary Table 1. Laser ablation inductively coupled plasma spectrometry (LA-ICP-MS) data for detrital zircons of Statherian and Cambrian sandstones from the western North China Block

Supp Table 2: Revisiting Ediacaran to early Cambrian depositional history of the western North China: Did it remain passive until mid-Paleozoic?

Supplementary Table 2. In-situ Lu-Hf isotope data of detrital zircons with U-Pb ages of c. 1600–500 Ma from Ediacaran and Cambrian sandstones from the western North China Block

Supp Table 2: Revisiting Ediacaran to early Cambrian depositional history of the western North China: Did it remain passive until mid-Paleozoic?

Supplementary Table 2. In-situ Lu-Hf isotope data of detrital zircons with U-Pb ages of c. 1600–500 Ma from Ediacaran and Cambrian sandstones from the western North China Block

Supp Figure 2: Revisiting Ediacaran to early Cambrian depositional history of the western North China: Did it remain passive until mid-Paleozoic?

Appendix Figure 2. Representative cathodoluminescence images of analyzed zircons from Statherian to Cambrian samples from the western North China Block, with red circles showing analytical spots and yellow and white numbers displaying corresponding U-Pb ages and Th/U ratios, respectively. (a) S002, (b) QLSLQ, (c) YSX-1, (d) QLSHW, (e) YSX-3, (f) SYSX-7