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The Mineral and Geochemical Features of Sulfides in the Jade Hydrothermal Field of the Okinawa Trough in Off-Shore China
Wang, Yujie1,2; Zeng, Zhigang1,2,3
2023-09-01
发表期刊JOURNAL OF MARINE SCIENCE AND ENGINEERING
卷号11期号:9页码:13
通讯作者Zeng, Zhigang(zgzeng@ms.qdio.ac.cn)
摘要In this study, mineralogical and elemental geochemical characteristics of massive sulfide samples collected from the Jade hydrothermal field, located in the Izena depression in the central graben of the Okinawa Trough, were analyzed by means of optical microscopy, scanning electron microscopy, and electron probe microanalysis (EPMA). The results show that the mineralization in the Jade hydrothermal field can be divided into Zn-Cu-Pb-rich massive sulfides and Zn-Fe-rich massive sulfides. The former is composed of sphalerite, galena, chalcopyrite, pyrite, and anglesite, which is the product of the low-temperature alteration of galena. The latter is mainly composed of sphalerite, pyrite, marcasite, and traces of galena. Cu and Zn in pyrite may exist in the form of microinclusions, while Ag and Pb may exist in pyrite in the form of fine galena inclusions containing Ag. Fe and Cu may enter sphalerite in the form of ion replacement. Zn may enter chalcopyrite in the form of ion replacement. Consistent with the previous understanding, the metal elements in the hydrothermal liquid system in the Jade hydrothermal field mostly migrated as sulfur complexes, and when the hydrothermal fluid mixes with seawater, the physical and chemical conditions of the fluid change, resulting in sulfide mineral precipitation. However, the chemical structure of chalcopyrite is still controversial, which restricts the understanding of the substitution mechanism of trace elements during chalcopyrite precipitation.
关键词massive sulfide mineralization stage Jade hydrothermal field Okinawa Trough
DOI10.3390/jmse11091772
收录类别SCI
语种英语
资助项目We are grateful for the valuable comments and suggestions from the anonymous reviewers and editors. This work was supported by the National Natural Science Foundation of China (Grant Nos. 91958213, 42221005), Strategic Priority Research Program (B) of the[91958213] ; We are grateful for the valuable comments and suggestions from the anonymous reviewers and editors. This work was supported by the National Natural Science Foundation of China (Grant Nos. 91958213, 42221005), Strategic Priority Research Program (B) of the[42221005] ; National Natural Science Foundation of China[XDB42020402] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[ts201511061] ; Special Fund for the Taishan Scholar Program of Shandong Province
WOS研究方向Engineering ; Oceanography
WOS类目Engineering, Marine ; Engineering, Ocean ; Oceanography
WOS记录号WOS:001071746500001
出版者MDPI
WOS关键词TRACE-ELEMENT SYSTEMATICS ; SEA-FLOOR ; MASSIVE SULFIDES ; ISOTOPIC CHARACTERISTICS ; DEPOSITS EVIDENCE ; MINOR ELEMENTS ; VOLCANIC-ROCKS ; BACKARC BASIN ; SPHALERITE ; CHALCOPYRITE
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文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/181799
专题海洋地质与环境重点实验室
通讯作者Zeng, Zhigang
作者单位1.Chinese Acad Sci, Inst Oceanol, Seafloor Hydrothermal Act Lab, CAS Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Laoshan Lab, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China
第一作者单位中国科学院海洋研究所
通讯作者单位中国科学院海洋研究所
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Wang, Yujie,Zeng, Zhigang. The Mineral and Geochemical Features of Sulfides in the Jade Hydrothermal Field of the Okinawa Trough in Off-Shore China[J]. JOURNAL OF MARINE SCIENCE AND ENGINEERING,2023,11(9):13.
APA Wang, Yujie,&Zeng, Zhigang.(2023).The Mineral and Geochemical Features of Sulfides in the Jade Hydrothermal Field of the Okinawa Trough in Off-Shore China.JOURNAL OF MARINE SCIENCE AND ENGINEERING,11(9),13.
MLA Wang, Yujie,et al."The Mineral and Geochemical Features of Sulfides in the Jade Hydrothermal Field of the Okinawa Trough in Off-Shore China".JOURNAL OF MARINE SCIENCE AND ENGINEERING 11.9(2023):13.
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