Geochemistry, geochronology and fluid inclusion studies of the Dongji epithermal gold deposit in Fujian province, south-east China
文献类型:期刊论文
作者 | Huang, Liang-Liang3,4; Fan, Hong-Rui2,3,4; Ma, Feng-Shan3,4; Liu, Ri-Fu1; Wang, Hui-Sheng1; Zheng, Guang-Shi1; Zhang, Zhi-Cheng1 |
刊名 | GEOLOGICAL JOURNAL |
出版日期 | 2022-08-25 |
页码 | 18 |
ISSN号 | 0072-1050 |
关键词 | Dongji gold deposit epithermal Au mineralization fluid inclusion South-east China Zircon U-Pb geochronology |
DOI | 10.1002/gj.4573 |
英文摘要 | The Dongji epithermal Au deposit formed in the Early Cretaceous is located in the Dongkeng volcanic Basin of the South China Block. The orebodies of the deposit are mainly hosted in the Jurassic volcanic-subvolcanic rocks. Here, detailed zircon U-Pb geochronology, major-trace elements, and fluid inclusion data of the Dongji deposit are reported. At least two epochs of magmatic activity were identified at Dongji, including the Late Jurassic rhyolitic crystal tuff lava (165.3 +/- 1.8 Ma to 162.8 +/- 2.6 Ma) and quartz porphyry (156.0 +/- 1.9 Ma), and the Early Cretaceous dacitic crystal tuff lava (108.4 +/- 5.7 Ma) and purplish-red crystal tuff lava (98.1 +/- 0.8 Ma). The Late Jurassic volcanic-subvolcanic rocks are characterized by high SiO2 content, enriched LILE (large ion lithophile element) elements, depleted HFSE (high field strength element) elements, and obvious P, Ti and Eu anomalies. These geochemical characteristics suggest that the volcanic-subvolcanic rocks were generated by partial melting of the lower crust and controlled by fractional crystallization of Ti-bearing phases, apatite, and plagioclase. In comparison, the Early Cretaceous volcanic-subvolcanic rocks are characterized by high K contents, and arc-like signatures (e.g., enriched Rb, Th, K, and depleted Nb, Ta, Ti), indicating a partial melting of crust-mantle interaction under an extensional tectonic setting. The ore-bearing dacitic crystal tuff lava and the caprock of purplish-red tuff lava constrain the timing of gold mineralization in the range of 108-98 Ma. The Au mineralization at Dongji is divided into the early stage of quartz-pyrite association and the late main mineralization stage of quartz-polymetallic sulfide association. The fluid inclusion microthermometry results show that the ore-forming fluids at the early mineralization are characterized by enrichment of liquid-rich two-phase inclusions and CO2-bearing aqueous inclusions. The fluids with moderate homogenization temperatures (292-382 degrees C) and low salinities (5.4-10.0 wt% NaClequiv) were possibly exsolved from magmatic rocks. Nevertheless, fluid inclusions in the late-stage contain liquid-rich two-phase inclusions and pure liquid phase inclusions. The homogenization temperatures (222-309 degrees C) and salinities (2.4-8.3 wt% NaClequiv) of the late-stage fluid inclusions are relatively lower than those of the early stage, probably indicating a fluid mixing of magmatic and meteoric fluids. Based on the above, we propose that fluid mixing is the key factor facilitating Au precipitation in the Dongji deposit, probably applicable to other Au deposits in the Dongkeng volcanic Basin. |
WOS关键词 | SE CHINA ; VOLCANIC-ROCKS ; U-PB ; STABLE-ISOTOPE ; TRACE-ELEMENT ; NANLING RANGE ; COASTAL AREA ; MAFIC ROCKS ; CU DEPOSIT ; PETROGENESIS |
资助项目 | Zhenghe Yuanxin Mining Corporation Limited |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | WILEY |
WOS记录号 | WOS:000844065900001 |
资助机构 | Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited ; Zhenghe Yuanxin Mining Corporation Limited |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/108402] |
专题 | 地质与地球物理研究所_中国科学院矿产资源研究重点实验室 |
通讯作者 | Fan, Hong-Rui |
作者单位 | 1.Zhenghe Yuanxin Min Corp Ltd, Nanping, Fujian, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing, Peoples R China 3.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Huang, Liang-Liang,Fan, Hong-Rui,Ma, Feng-Shan,et al. Geochemistry, geochronology and fluid inclusion studies of the Dongji epithermal gold deposit in Fujian province, south-east China[J]. GEOLOGICAL JOURNAL,2022:18. |
APA | Huang, Liang-Liang.,Fan, Hong-Rui.,Ma, Feng-Shan.,Liu, Ri-Fu.,Wang, Hui-Sheng.,...&Zhang, Zhi-Cheng.(2022).Geochemistry, geochronology and fluid inclusion studies of the Dongji epithermal gold deposit in Fujian province, south-east China.GEOLOGICAL JOURNAL,18. |
MLA | Huang, Liang-Liang,et al."Geochemistry, geochronology and fluid inclusion studies of the Dongji epithermal gold deposit in Fujian province, south-east China".GEOLOGICAL JOURNAL (2022):18. |
入库方式: OAI收割
来源:地质与地球物理研究所
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