The exhumation history of the Central Asian Orogenic Belt reveals preserved paleotopography since ~160 Ma

Attached is the single-grain apatite and zircon data obtained for the Karatau-Talas Terrane, Kazakhstan-Kyrgyzstan. In addition to modelling parameters used and raw outputs for transparency.Figure S1. Radial plots for apatite fission-track calculating central ages.Figure S2. Observed vs Predicted mean track length Distribution and Observed Ages vs Predicted Ages for thermal modelling using QTQt 5.7.0.Figure S3. Tera-Wasserburg (T-W) concordia diagrams of apatite U-Pb data from samples A16-34, B15204, and 06-TN-12. Ellipses are plotted at 2 sigma uncertainties. The dashed lines correspond to linear regressions through the apatite U-Pb data that were used to obtain an estimate of the initial 207Pb/206Pb ratio (upper intersect of the concordia curve) and the apatite U-Pb (AUPb) date (lower intercept with the concordia curve).Table S1. Apatite fission track age and chemical data: ρs is the density of spontaneous tracks within the region of interest and is expressed as 10^5 tracks/cm2. Ns is the total number of counted spontaneous tracks per sample. 238U is the concentration in ppm of uranium 238 measured in each grain. 35Cl is the concentration in ppm of chlorine 35 measured in each grain. BLOD is below limits of detection, and thus could not provide a concentration value and was not used in calculating sample concentration averages. Dpar is the average length of spontaneous track etch pits in μm. t is the age of the grain age in Ma.Table S2. Zircon fission track age and chemical data: Ns and Ni is the number of spontaneous and induced fission-tracks respectively. Area is the region of interest counted. RhoS is the density of spontaneous tracks, RhoD is the density of dosimeter tracks, RhoI is the density of induced tracks.Table S3. Thermal history model input table for simulations of the Karatau-Talas, Kazakhstan and Kyrgyzstan, based on framework established by Flowers et al. (2015).Table S4. 238U/206Pb and 207Pb/206Pb ratios and their associated standard deviation, as well at their individual error corrections.For inquiries regarding the contents of this dataset, please contact the Corresponding Author listed in the README.txt file. Administrative inquiries (e.g., removal requests, trouble downloading, etc.) can be directed to [e-mail]

附为此数据集的是哈萨克斯坦-吉尔吉斯斯坦卡拉套-塔拉斯地体的单颗粒磷灰石和锆石数据。此外，还包括建模参数的使用和原始输出，以确保透明度。图S1展示了磷灰石裂变径迹计算中心年龄的径向图。图S2展示了使用QTQt 5.7.0进行热力学建模时，观测值与预测值的平均径迹长度分布，以及观测年龄与预测年龄的比较。图S3展示了来自样品A16-34、B15204和06-TN-12的磷灰石U-Pb数据的Tera-Wasserburg（T-W）一致线图。椭圆表示2倍标准差的不确定性。虚线对应于通过磷灰石U-Pb数据进行的线性回归，用以获取初始207Pb/206Pb比率的估计（一致线曲线的上交点）和磷灰石U-Pb（AUPb）年龄（与一致线曲线的下截距）。表S1提供了磷灰石裂变径迹年龄和化学数据：ρs是在感兴趣区域内的自发径迹密度，以10^5条/cm^2表示。Ns是每个样品中计数的自发径迹总数。238U是每个颗粒中238U浓度的ppm值。35Cl是每个颗粒中35Cl浓度的ppm值。BLOD低于检测限，因此无法提供浓度值，且未用于计算样品浓度平均值。Dpar是自发径迹蚀坑的平均长度，以μm为单位。t是颗粒年龄，以Ma为单位。表S2提供了锆石裂变径迹年龄和化学数据：Ns和Ni分别是自发和诱导裂变径迹的数量。Area是计数的感兴趣区域。RhoS是自发径迹的密度，RhoD是剂量计径迹的密度，RhoI是诱导径迹的密度。表S3是基于Flowers等人（2015年）建立的框架，为哈萨克斯坦和吉尔吉斯斯坦的卡拉套-塔拉斯地体的热历史模型模拟提供的输入表。表S4提供了238U/206Pb和207Pb/206Pb比率及其相关标准偏差，以及各自的误差校正。有关此数据集内容的查询，请联系README.txt文件中列出的通讯作者。行政查询（例如，删除请求、下载问题等）可发送至[e-mail]。