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	Origin of native sulfur ball from the Kueishantao hydrothermal field offshore northeast Taiwan: Evidence from trace and rare earth element composition
	Zeng, Zhigang1; Chen, Chen-Tung A.3; Yin, Xuebo1; Zhang, Xueying1; Wang, Xiaoyuan1; Zhang, Guoliang1,2; Wang, Xiaomei1,2; Chen, Daigeng1,2; Zeng, ZG (reprint author), Chinese Acad Sci, Inst Oceanol, Seafloor Hydrothermal Activ Lab, Key Lab Marine Geol & Environm, 7 Nanhai Rd, Qingdao 266071, Peoples R China
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	2011-01-20
卷号	40期号:2页码:661-671
关键词	Trace Elements Rare Earth Elements Native Sulfur Ball Kueishantao Hydrothermal Field Northeast Taiwan
ISSN号	1367-9120
DOI	10.1016/j.jseaes.2010.10.019
文献子类	Article
英文摘要	We first report the trace and rare earth element compositions of native sulfur ball with sulfur contents varying from 97.08 wt.% to 99.85 wt.% from the Kueishantao hydrothermal field, off NE Taiwan. We then discuss the sources of trace and rare earth elements incorporated into the native sulfur ball during formation. Comparison of our results with native sulfur from crater lakes and other volcanic areas shows the sulfur content of native sulfur ball from the Kueishantao hydrothermal field is very high, and that the rare earth element (REE) and trace element constituents of the native sulfur balls are very low (Sigma REE < 35 ppb). In the native sulfur ball, V, Cr, Co, Ni, Nb, Rb, Cs, Ba, Pb, Th, U. Al, Ti and REE are mostly derived from andesite; Mg, K and Mn are mostly derived from seawater; and Fe, Cu, Zn and Ni are partly derived from magma. Based on the sulfur contents, trace and rare earth element compositions, and local environment, we suggest that the growth of the native sulfur ball is significantly slower than that of native sulfur chimneys, which results in the relatively higher contents of trace and rare earth element contents in the native sulfur ball than in the native sulfur chimneys from the Kueishantao hydrothermal field. Finally, we suggest a "glue pudding" growth model for understanding the origin of the native sulfur ball in the Kueishantao hydrothermal field, whereby the native sulfur ball forms from a mixture of oxygenated seawater and acidic, low-temperature hydrothermal fluid with H(2)S and SO(2) gases, and is subsequently shaped by tidal and/or bottom currents. (C) 2010 Elsevier Ltd. All rights reserved.; We first report the trace and rare earth element compositions of native sulfur ball with sulfur contents varying from 97.08 wt.% to 99.85 wt.% from the Kueishantao hydrothermal field, off NE Taiwan. We then discuss the sources of trace and rare earth elements incorporated into the native sulfur ball during formation. Comparison of our results with native sulfur from crater lakes and other volcanic areas shows the sulfur content of native sulfur ball from the Kueishantao hydrothermal field is very high, and that the rare earth element (REE) and trace element constituents of the native sulfur balls are very low (Sigma REE < 35 ppb). In the native sulfur ball, V, Cr, Co, Ni, Nb, Rb, Cs, Ba, Pb, Th, U. Al, Ti and REE are mostly derived from andesite; Mg, K and Mn are mostly derived from seawater; and Fe, Cu, Zn and Ni are partly derived from magma. Based on the sulfur contents, trace and rare earth element compositions, and local environment, we suggest that the growth of the native sulfur ball is significantly slower than that of native sulfur chimneys, which results in the relatively higher contents of trace and rare earth element contents in the native sulfur ball than in the native sulfur chimneys from the Kueishantao hydrothermal field. Finally, we suggest a "glue pudding" growth model for understanding the origin of the native sulfur ball in the Kueishantao hydrothermal field, whereby the native sulfur ball forms from a mixture of oxygenated seawater and acidic, low-temperature hydrothermal fluid with H(2)S and SO(2) gases, and is subsequently shaped by tidal and/or bottom currents. (C) 2010 Elsevier Ltd. All rights reserved.
学科主题	Geology
URL标识	查看原文
语种	英语
WOS记录号	WOS:000286846400017
公开日期	2012-07-03
内容类型	期刊论文
源URL	[http://ir.qdio.ac.cn/handle/337002/11508]
专题	海洋研究所_海洋地质与环境重点实验室
通讯作者	Zeng, ZG (reprint author), Chinese Acad Sci, Inst Oceanol, Seafloor Hydrothermal Activ Lab, Key Lab Marine Geol & Environm, 7 Nanhai Rd, Qingdao 266071, Peoples R China
作者单位	1.Chinese Acad Sci, Inst Oceanol, Seafloor Hydrothermal Activ Lab, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China 3.Natl Sun Yat Sen Univ, Inst Marine Geol & Chem, Kaohsiung 804, Taiwan
推荐引用方式 GB/T 7714	Zeng, Zhigang,Chen, Chen-Tung A.,Yin, Xuebo,et al. Origin of native sulfur ball from the Kueishantao hydrothermal field offshore northeast Taiwan: Evidence from trace and rare earth element composition[J]. JOURNAL OF ASIAN EARTH SCIENCES,2011,40(2):661-671.
APA	Zeng, Zhigang.,Chen, Chen-Tung A..,Yin, Xuebo.,Zhang, Xueying.,Wang, Xiaoyuan.,...&Zeng, ZG .(2011).Origin of native sulfur ball from the Kueishantao hydrothermal field offshore northeast Taiwan: Evidence from trace and rare earth element composition.JOURNAL OF ASIAN EARTH SCIENCES,40(2),661-671.
MLA	Zeng, Zhigang,et al."Origin of native sulfur ball from the Kueishantao hydrothermal field offshore northeast Taiwan: Evidence from trace and rare earth element composition".JOURNAL OF ASIAN EARTH SCIENCES 40.2(2011):661-671.

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