《Table 3 LA–ICP–MS Zircon U–Pb Ages of the Granitoids in Jiangla’angzong》

《Table 3 LA–ICP–MS Zircon U–Pb Ages of the Granitoids in Jiangla’angzong》   提示：宽带有限、当前游客访问压缩模式
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《"Petrogenesis of Late Cretaceous Jiangla'angzong I-Type Granite in Central Lhasa Terrane, Tibet, China: Constraints from Whole-Rock Geochemistry, Zircon U-Pb Geochronology, and Sr-Nd-Pb-Hf Isotopes"》


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Jiangla’angzong syenogranite and adamellite Rb-Sr，Sm-Nd，and Pb isotopic compositions are listed in Table 6and Fig.6.The 87Rb/86Sr ratios ranged from1.8780 to4.6441，the 87Sr/86Sr ratios ranged from 0.7106 to 0.7180，the 147Sm/144Nd ratios ranged from 0.1015 to 0.1086，the143Nd/144Nd ratios ranged from 0.5121 to 0.5123，the206Pb/204Pb ratios ranged from 18.758 to 18.828，the207Pb/204Pb ratios ranged from 15.698 to 15.709，and the208Pb/204Pb ratios ranged from 39.218 to 38.280.Analytical results show that these mineral grains have homogenous Rb-Sr，Sm-Nd，and Pb isotopic compositions.The（87Sr/86Sr）t ratios ranged from 0.7106 to 0.7179，the（143Nd/144Nd）t ratios ranged from 0.5121 to 0.5123，the（206Pb/204Pb）t ratios ranged from 18.683 to 18.746，the（207Pb/204Pb）t ratios ranged from 15.695 to 15.702，（208Pb/204Pb） t ratios ranged from from 39.012 to 39.071，and theεNd（t）ranged from，-10.17 to-6.10.

图表编号XD0017176100    严禁用于非法目的
绘制时间2018.08.01
作者LIU Hong、LI Guangming、HUANG Hanxiao、CAO Huawen、YUAN Qian、LI Yingxu、OUYANG Yuan、LAN Shuangshuang、Lü Menghong、YAN Guoqiang
绘制单位Chengdu Center,China Geological Survey、Chengdu Center,China Geological Survey、Chengdu Center,China Geological Survey、Chengdu Center,China Geological Survey、Faculty of Earth Resources, China University of Geosciences、Chengdu Center,China Geological Survey、
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