The Cenozoic Himalayan leucogranite-pegmatite belt has been a hotspot for rare metal exploration in recent years.To determine the genesis of the pegmatite in the Himalayan region and its relationship with the Greater ...The Cenozoic Himalayan leucogranite-pegmatite belt has been a hotspot for rare metal exploration in recent years.To determine the genesis of the pegmatite in the Himalayan region and its relationship with the Greater Himalayan Crystalline Complex(GHC),the Gyirong pegmatite in southern Tibet was chosen for geochronological and geochemical studies.The dating analyses indicate that the U-Th-Pb ages of zircon,monazite,and xenotime exhibit large variations(38.6‒16.1 Ma),with the weighted average value of the four youngest points is 16.5±0.3 Ma,which indicates that the final stage of crystallization of the melt occurred in the Miocene.The age of the muscovite Ar-Ar inverse isochron is 15.2±0.4 Ma,which is slightly later than the intrusion age,showing that a cooling process associated with rapid denudation occurred at 16‒15 Ma.TheεHf(t)values of the Cenozoic anatectic zircons cluster between−12 and−9 with an average of−11.4.The Gyirong pegmatite shows high contents of Si,Al,and K,a high Al saturation index,and low contents of Na,Ca,Fe,Mn,P,Mg,and Ti.Overall,the Gyirong pegmatite is enriched in Rb,Cs,U,K,Th and Pb and depleted in Nb,Ta,Zr,Ti,Eu,Sr,and Ba.The samples show a high 87Sr/86Sr(16 Ma)ratio of ca.0.762 and a lowεNd(16 Ma)value of−16.0.The calculated average initial values of 208Pb/204Pb(16 Ma),207Pb/204Pb(16 Ma)and 206Pb/204Pb(16 Ma)of the whole rock are 39.72,15.79 and 19.56,respectively.The Sr-Nd-Pb-Hf isotopic characteristics of the Gyirong pegmatite are consistent with those of the GHC.This study concludes that the Gyirong pegmatite represents a typical crustal‒derived anatectic pegmatite with low metallogenic potential for rare metals.The Gyirong pegmatite records the long‒term metamorphism and partial melting process of the GHC,and reflects the crustal thickening caused by thrust compression at 39‒29 Ma and the crustal thinning induced by extensional decompression during 28‒15 Ma.展开更多
介绍了激光诱导击穿光谱(laser induced breakdown spectroscopy,LIBS)技术、主元分析(principal component an alysis,PCA)法和偏最小二乘(partial least squares,PLS)法的基本原理。对Pb元素特征谱线附近的36个维度进行主成分信息提取...介绍了激光诱导击穿光谱(laser induced breakdown spectroscopy,LIBS)技术、主元分析(principal component an alysis,PCA)法和偏最小二乘(partial least squares,PLS)法的基本原理。对Pb元素特征谱线附近的36个维度进行主成分信息提取,对36维波长数据压缩到2维后,采用每个样品的20个脉冲的主元分数进行偏最小二乘拟合,对数据进行平均处理后,拟合结果质量较高,拟合系数平方的值从0.49810提高到0.97000;残差平方和从0.72529下降到1.36366*10^(-4)。PCA法可以有效的缩减具有一定相关性的样本数据空间,对于数据维度较大的数据处理能显著提升效率,再结合PLS法拟合压缩后的主元,实验结论得出PLS适合用于LIBS定量分析。展开更多
在 n 维的 Sr-Nd-Pb 同位素空间中,几乎所有的大洋中脊玄武岩(MORB)和洋岛玄武岩(OIB)都落在一个虚拟平面上,被称为"地幔面(mantle plane)"。"地幔面"描述了大部分玄武岩的同位素地球化学特征,是最重要的、也是最...在 n 维的 Sr-Nd-Pb 同位素空间中,几乎所有的大洋中脊玄武岩(MORB)和洋岛玄武岩(OIB)都落在一个虚拟平面上,被称为"地幔面(mantle plane)"。"地幔面"描述了大部分玄武岩的同位素地球化学特征,是最重要的、也是最早提出的地幔动力学演化特征之一,但是长期以来关于"地幔面"的内涵和意义并不清楚。本文通过一个综合模型,反演受岩浆作用控制的地幔微量元素(包括各种同位素母体元素)分异、Sr-Nd-Pb同位素演化,并推导出地幔 Sr-Nd-Pb 同位素演化的二元参数方程形式。模型表明,通过部分熔融向地壳输出相对富硅、富碱的物质成分,是地幔长期演化的主要特点,这个过程受到两个参数—部分融融程度(F)和岩浆分离的时间(t)—的控制,即 n 维参数可化为2维,因此在 n 维同位素空间出现"地幔面"的特征。壳源物资循环,能够使局部地幔偏离"地幔面",就地幔总体统计特征而言,地壳混染的比例很低,不同的统计数据显示大约1%～6%的系统偏差,即可能的地壳混染程度;进一步模拟,可能作出更加精确的估算。展开更多
基金sponsored by the National Key R&D Programme of China(2021YFC2901803)National Natural Science Foundation of China(92055314 and 41802095)+2 种基金the China Geological Survey(DD20230049 and DD20220983)is a contribution to the International Geoscience Programme(IGCP-741)Academician Bao-jun Liu Foundation of Southwest Geological Science and Technology Innovation Center.
文摘The Cenozoic Himalayan leucogranite-pegmatite belt has been a hotspot for rare metal exploration in recent years.To determine the genesis of the pegmatite in the Himalayan region and its relationship with the Greater Himalayan Crystalline Complex(GHC),the Gyirong pegmatite in southern Tibet was chosen for geochronological and geochemical studies.The dating analyses indicate that the U-Th-Pb ages of zircon,monazite,and xenotime exhibit large variations(38.6‒16.1 Ma),with the weighted average value of the four youngest points is 16.5±0.3 Ma,which indicates that the final stage of crystallization of the melt occurred in the Miocene.The age of the muscovite Ar-Ar inverse isochron is 15.2±0.4 Ma,which is slightly later than the intrusion age,showing that a cooling process associated with rapid denudation occurred at 16‒15 Ma.TheεHf(t)values of the Cenozoic anatectic zircons cluster between−12 and−9 with an average of−11.4.The Gyirong pegmatite shows high contents of Si,Al,and K,a high Al saturation index,and low contents of Na,Ca,Fe,Mn,P,Mg,and Ti.Overall,the Gyirong pegmatite is enriched in Rb,Cs,U,K,Th and Pb and depleted in Nb,Ta,Zr,Ti,Eu,Sr,and Ba.The samples show a high 87Sr/86Sr(16 Ma)ratio of ca.0.762 and a lowεNd(16 Ma)value of−16.0.The calculated average initial values of 208Pb/204Pb(16 Ma),207Pb/204Pb(16 Ma)and 206Pb/204Pb(16 Ma)of the whole rock are 39.72,15.79 and 19.56,respectively.The Sr-Nd-Pb-Hf isotopic characteristics of the Gyirong pegmatite are consistent with those of the GHC.This study concludes that the Gyirong pegmatite represents a typical crustal‒derived anatectic pegmatite with low metallogenic potential for rare metals.The Gyirong pegmatite records the long‒term metamorphism and partial melting process of the GHC,and reflects the crustal thickening caused by thrust compression at 39‒29 Ma and the crustal thinning induced by extensional decompression during 28‒15 Ma.
文摘介绍了激光诱导击穿光谱(laser induced breakdown spectroscopy,LIBS)技术、主元分析(principal component an alysis,PCA)法和偏最小二乘(partial least squares,PLS)法的基本原理。对Pb元素特征谱线附近的36个维度进行主成分信息提取,对36维波长数据压缩到2维后,采用每个样品的20个脉冲的主元分数进行偏最小二乘拟合,对数据进行平均处理后,拟合结果质量较高,拟合系数平方的值从0.49810提高到0.97000;残差平方和从0.72529下降到1.36366*10^(-4)。PCA法可以有效的缩减具有一定相关性的样本数据空间,对于数据维度较大的数据处理能显著提升效率,再结合PLS法拟合压缩后的主元,实验结论得出PLS适合用于LIBS定量分析。
文摘在 n 维的 Sr-Nd-Pb 同位素空间中,几乎所有的大洋中脊玄武岩(MORB)和洋岛玄武岩(OIB)都落在一个虚拟平面上,被称为"地幔面(mantle plane)"。"地幔面"描述了大部分玄武岩的同位素地球化学特征,是最重要的、也是最早提出的地幔动力学演化特征之一,但是长期以来关于"地幔面"的内涵和意义并不清楚。本文通过一个综合模型,反演受岩浆作用控制的地幔微量元素(包括各种同位素母体元素)分异、Sr-Nd-Pb同位素演化,并推导出地幔 Sr-Nd-Pb 同位素演化的二元参数方程形式。模型表明,通过部分熔融向地壳输出相对富硅、富碱的物质成分,是地幔长期演化的主要特点,这个过程受到两个参数—部分融融程度(F)和岩浆分离的时间(t)—的控制,即 n 维参数可化为2维,因此在 n 维同位素空间出现"地幔面"的特征。壳源物资循环,能够使局部地幔偏离"地幔面",就地幔总体统计特征而言,地壳混染的比例很低,不同的统计数据显示大约1%～6%的系统偏差,即可能的地壳混染程度;进一步模拟,可能作出更加精确的估算。
