Characteristics and in situ U-Pb dating of hydrothermal titanite by LA-ICPMS of the Jingshandian iron skarn deposit, Hubei Province | |
Zhu QiaoQiao5; Xie GuiQing1; Jiang ZhongSheng; Sun JinFeng2; Li Wei3 | |
刊名 | ACTA PETROLOGICA SINICA
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2014 | |
卷号 | 30期号:5页码:1322-1338 |
关键词 | Hydrothermal titanite In situ U-Pb dating Skarn iron deposit Southeastern Hubei Province |
ISSN号 | 1000-0569 |
英文摘要 | U-Pb ages and trace element compositions of two types of hydrothermal titanite from the Jinshandian iron skarn deposit, southeastern Hubei Province, have been successfully analyzed by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS). Compared to titanite from diopside and scapolite skarn, hydrothermal titanite from albite altered quartz diorite are characterized by lower REE, delta Eu values, Th/U, Lu/Hf ratios and higher Hf component and LREE/HREE, suggesting they formed under different environment. The amount of Ti in the hydrothermal titanite probably resulted from the decomposition of Ti-bearing accessory minerals such as titanite, ilmenite and rutile from magma during the alteration. In situ U-Pb dating of titanite by LA-ICPMS shows that titanite from diopside + anhydrite + magnenite and scapolite + anhydrite + magnenite skarn sample yield a weighted mean Pb-206/U-238 ages of 129.5 +/- 1Ma and 130.4 +/- 1. 2Ma, respectively, while that of albite altered quartz diorite give 127 +/- 12Ma. These ages might be considered to be the age of mineralization, consistent with crystallization age of phlogopite got by previous researcher, suggesting that Jinshandian iron skarn deposit formed associate with lithospheric thinning, similar to other skarn Cu-Fe deposits in the southeastern Hubei Province. Our study shows that in situ U-Pb dating of hydrothermal titanite by LA-ICPMS is a robust method for getting precise formation age of skarn iron deposit. |
学科主题 | 地质年代学 |
WOS关键词 | MIDDLE-LOWER REACHES ; HF ISOTOPIC CONSTRAINTS ; YANGTZE-RIVER VALLEY ; LATE MESOZOIC MAGMATISM ; NING-WU BASIN ; CU-AU-MO ; EASTERN CHINA ; SOUTHEASTERN HUBEI ; GOLD DEPOSIT ; GEOLOGICAL SIGNIFICANCE |
WOS研究方向 | Geology |
语种 | 中文 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000337205700010 |
内容类型 | 期刊论文 |
源URL | [http://119.78.100.197/handle/2HKVOGP0/40387] ![]() |
专题 | 中国地质科学院矿产资源研究所 |
作者单位 | 1.Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China 2.MRL Key Lab Metallogeny & Mineral Assessment, Beijing 100037, Peoples R China 3.Univ Chinese Acad Sci, Fac Earth Sci, Beijing 100049, Peoples R China 4.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China 5.中国地质科学院矿产资源研究所 |
推荐引用方式 GB/T 7714 | Zhu QiaoQiao,Xie GuiQing,Jiang ZhongSheng,et al. Characteristics and in situ U-Pb dating of hydrothermal titanite by LA-ICPMS of the Jingshandian iron skarn deposit, Hubei Province[J]. ACTA PETROLOGICA SINICA,2014,30(5):1322-1338. |
APA | Zhu QiaoQiao,Xie GuiQing,Jiang ZhongSheng,Sun JinFeng,&Li Wei.(2014).Characteristics and in situ U-Pb dating of hydrothermal titanite by LA-ICPMS of the Jingshandian iron skarn deposit, Hubei Province.ACTA PETROLOGICA SINICA,30(5),1322-1338. |
MLA | Zhu QiaoQiao,et al."Characteristics and in situ U-Pb dating of hydrothermal titanite by LA-ICPMS of the Jingshandian iron skarn deposit, Hubei Province".ACTA PETROLOGICA SINICA 30.5(2014):1322-1338. |
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