Crustal deformation in the northeastern Tibetan Plateau: the roles of northward indentation of the Qaidam basin and southward underthrusting of the North China Craton

Chuang Sun*, Zhigang Li, Wenjun Zheng, Dong Jia, Shuang Yang *Corresponding author: Chuang Sun ([e-mail] and [e-mail]) All the presented kinematical data were measured from modelled thrust wedges in our sandbox experiments which illustrating how brittle upper crust response differently to distinct boundary conditions, like that of indentation or underthrusting of certain plate/block mantle lithosphere in the northern Tibetan Plateau. This supporting information includes the supplementary 5 tables. Table S1. The measured elevations of each structures in Exp.030 and Exp.031 and their uplift rates. Table S2. The measured elevations of each structures in Exp.026 and their uplift rates. Table S3. The measured elevations of each structures in Exp.020 and Exp.022 and their uplift rates. Table S4. Dynamic surface slope angles measured from all the five experiments. Table S5. Dynamic width of the growing thrust wedges measured from all the five experiments.孙闯*，李志刚，郑文军，贾栋，杨双 通讯作者：孙闯（[e-mail]、[e-mail]） 本研究呈现的全部运动学数据均取自我们砂箱实验中的模拟逆冲楔体（thrust wedges），用以阐明脆性上地壳对不同边界条件的差异化响应，例如青藏高原北部特定板块/地块岩石圈地幔的压入或下插过程。本补充材料包含5张附表： 表S1：Exp.030与Exp.031实验中各构造的实测高程及其隆升速率 表S2：Exp.026实验中各构造的实测高程及其隆升速率 表S3：Exp.020与Exp.022实验中各构造的实测高程及其隆升速率 表S4：全部5组实验测得的动态地表坡角 表S5：全部5组实验测得的生长中逆冲楔体的动态宽度