Supplementary figure 1, sample location with Maximum depositional age, and Zircon U-Pb analyses : Evidence for Late Triassic crustal suturing of the Central and Southern Pamir

Sup Fig. 1. Calculated R2 crossplot statistical comparison values between the Lokzun Group flysch, Darbasatash Group, and Northern Pamirs’ Karakul-Mazar using Saylor and Sundell’s (2016) DZstats. An R2 crossplot value greater than 0.70±0.10 suggest that the samples are related and have a common source. Note that sample DV 8-08-16_3, which has a distinct late Proterozoic-early Paleozoic population, is associated with R2 crossplot values that lie below this range. Table 1 DR1-Sample Location and MDA contains the location and maximum depositional age for samples in the manuscript:Evidence for Late Triassic crustal suturing of the Central and Southern Pamir Table 2 DR2-Zircon U-Pb analyses contains data collected from the samples used in the manuscript: Evidence for Late Triassic crustal suturing of the Central and Southern Pamir

补充图1 展示了基于Saylor与Sundell（2016）开发的DZstats工具，计算得到的洛祖恩群复理石、达尔巴沙塔什群以及北帕米尔喀拉库勒-马扎尔地区样品的R²交会图统计对比值。当R²交会图数值大于0.70±0.10时，表明样品间存在成因关联且具有共同物源。需注意，样品DV 8-08-16_3具有显著的新元古代-早古生代锆石群体特征，其R²交会图数值落在该阈值范围之外。表1 DR1-样品位置与最大沉积年龄（MDA）收录了论文《中帕米尔与南帕米尔晚三叠世地壳缝合作用证据》（Evidence for Late Triassic crustal suturing of the Central and Southern Pamir）中所有样品的采样位置与最大沉积年龄数据。表2 DR2-锆石U-Pb分析数据收录了该研究论文中所用样品的相关测试数据。