Origin of the Permian high silica A-type granites in Halajun, South Tienshan, NW China: Implications for crystal-liquid segregation and rare metal fertilization
文献类型：期刊论文
| 作者 | Chen, Tian-Chu4,5,6; Ling, Ming-Xing1; Liu, Yu-Long3,4; Jiang, Xiao-Yan2; Wei, Ying1; Chen, Jia-Jie1 |
| 刊名 | LITHOS
 |
| 出版日期 | 2024-03-01 |
| 卷号 | 468页码:16 |
| 关键词 | High Silica A-type granite (HSAG) Crystal-liquid segregation Rare metal Fertilization Tarim Large Igneous Provinve (TLIP) |
| ISSN号 | 0024-4937 |
| DOI | 10.1016/j.lithos.2024.107490 |
| 英文摘要 | High silica A-type granites (HSAGs) are important carriers of rare metal elements. Formation of HSAGs by crystal-liquid segregation would facilitate fertilization of rare metals and rare earth elements (REE). In this work, we present detailed petrology, whole-rock geochemistry, and in-situ zircon UPb ages and HfO isotopic compositions of the Halajun HSAGs in the South Tienshan Orogenic Belt (STOB). In combination with the previous study of the Halajun syenite and monzonite, we unravel the genetic connection of these granitoids and further explore the metallogenetic potentiality of HSAGs along the STOB in China. The Halajun granites have geochemical affinities of HSAGs with high SiO2 contents (> 70 wt%), whole-rock zirconium saturation thermometry (680-860 degrees C), high Ga/Al ratios and high field strength elements (HFSE) contents. The HSAGs (273-279 Ma), monzonite (280 Ma) and syenite (283 Ma) have similar formation ages, identical mineral assemblages, and consistent variations in major elements, implying a common magma reservoir of their parental magma. The Tamu and Huoshibulake HSAGs have high SiO2 (74.5-78.1 wt%) contents, low Sr (5-28 ppm) and Ba (7-60 ppm) contents, high Rb/Sr ratios (11.6-87.5), and strong negative Eu anomalies (0.01-0.08). Combined with the petrographic features, these geochemical variations suggest that they are the extracted melt. Conversely, the geochemical (high Sr and Ba concentrations, and Eu/Eu* near unity) and petrographic features of monzonite and syenite represent the residual silicic cumulate (crystals +/- trapped melt). The Kezi'ertuo and Halajun II HSAGs have SiO2 (71.9-76.5 wt%) contents, Sr (35-101 ppm) and Ba (60-541 ppm) contents, Rb/Sr ratios (1.9-8.9), and negative Eu anomalies (0.04-0.43), indicating the intermediate component (extracted melt + fractional crystals) in the consecutive system of crystal-liquid segregation. In-situ zircon HfO isotopes for the Halajun granitoids indicate a complex trans-crustal magmatic process involving crystal-liquid segregation and wall-rock assimilation. The long-time span of Tarim Large Igneous Province (TLIP) sustained injection of mantle-derived magma and/or advective heat to the magma chamber (> 1 Ma). Owing to the prolonged magma evolution, the highly fractionated silicic magma with high incompatible elements and F contents was extracted from the magma mush, and formed the HSAGs. |
| WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
| 语种 | 英语 |
| WOS记录号 | WOS:001159257400001 |
| 源URL | [http://ir.gig.ac.cn/handle/344008/76261]  |
| 专题 | 同位素地球化学国家重点实验室 |
| 通讯作者 | Ling, Ming-Xing; Liu, Yu-Long |
| 作者单位 | 1.East China Univ Technol, State Key Lab Nucl Resources & Environm, Nanchang 330013, Peoples R China 2.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550081, Peoples R China 3.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Mineral & Metallogeny, Guangzhou 510640, Peoples R China 4.CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China 5.Univ Chinese Acad Sci, Beijing 100094, Peoples R China 6.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China |
| 推荐引用方式 GB/T 7714 | Chen, Tian-Chu,Ling, Ming-Xing,Liu, Yu-Long,et al. Origin of the Permian high silica A-type granites in Halajun, South Tienshan, NW China: Implications for crystal-liquid segregation and rare metal fertilization[J]. LITHOS,2024,468:16. |
| APA | Chen, Tian-Chu,Ling, Ming-Xing,Liu, Yu-Long,Jiang, Xiao-Yan,Wei, Ying,&Chen, Jia-Jie.(2024).Origin of the Permian high silica A-type granites in Halajun, South Tienshan, NW China: Implications for crystal-liquid segregation and rare metal fertilization.LITHOS,468,16. |
| MLA | Chen, Tian-Chu,et al."Origin of the Permian high silica A-type granites in Halajun, South Tienshan, NW China: Implications for crystal-liquid segregation and rare metal fertilization".LITHOS 468(2024):16. |
入库方式： OAI收割
来源：广州地球化学研究所
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