中国台湾龟山岛热液自然硫中微观包体的元素富集特征

陈雪刚; 邱中炎; 段威; 李小虎; 叶瑛; 陈镇东

doi:10.3799/dqkx.2018.413

Volume 43 Issue 5

May 2018

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Chen Xuegang, Qiu Zhongyan, Duan Wei, Li Xiaohu, Ye Ying, Chentung Arthur, 2018. Elemental Enrichment in the Microscopic Inclusions of the Native Sulfur from Kueishantao Hydrothermal System, Taiwan, China. Earth Science, 43(5): 1549-1561. doi: 10.3799/dqkx.2018.413

Citation:

Chen Xuegang, Qiu Zhongyan, Duan Wei, Li Xiaohu, Ye Ying, Chentung Arthur, 2018. Elemental Enrichment in the Microscopic Inclusions of the Native Sulfur from Kueishantao Hydrothermal System, Taiwan, China. Earth Science, 43(5): 1549-1561. doi: 10.3799/dqkx.2018.413

Citation:

Chen Xuegang, Qiu Zhongyan, Duan Wei, Li Xiaohu, Ye Ying, Chentung Arthur, 2018. Elemental Enrichment in the Microscopic Inclusions of the Native Sulfur from Kueishantao Hydrothermal System, Taiwan, China. Earth Science, 43(5): 1549-1561. doi: 10.3799/dqkx.2018.413

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Elemental Enrichment in the Microscopic Inclusions of the Native Sulfur from Kueishantao Hydrothermal System, Taiwan, China

doi: 10.3799/dqkx.2018.413

1.
Ocean College, Zhejiang University, Zhoushan 316021, China
2.
Key Laboratory of Submarine Geoscience, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
3.
Department of Oceanography, National Sun Yat-Sen University, Kaohsiung 80424, China

Received Date: 2017-08-16
Publish Date: 2018-05-15

Abstract

Abstract

The Kueishantao shallow-water hydrothermal system, offshore northeast Taiwan, discharges large amounts of native sulfur. In order to unveil the distribution of trace elements in the native sulfur, we analyzed the elemental contents of sulfur matrix and microscopic inclusions in the KST native sulfur by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS). The results indicate that the sulfur matrix only contains volatile chalcophile elements such as As, Se, and Te, which are mainly originated from magma degassing. The siderophile elements including Fe, Mn, Co, and Ni are mainly contributed by the andesite host rock of the KST system. These elements are enriched in the Fe-rich and/or Si-bearing inclusions as various sulfides. Al, Zn, Ba, Pb, La, Ce, Au, and Ag were significantly enriched in Si-bearing inclusions, suggesting that the occurrence of these elements was mainly controlled by silicate particles.The Cu-rich inclusions contain higher per unit chalcophile elements (Hg, Pb, and Zn) than Fe-rich inclusions. The distribution of trace elements is analyzed in-situ in the KST native sulfur for the first time. This study will help to better understand the geochemical behaviors of trace elements during hydrothermal processes.
- seafloor hydrothermal system,
- chalcophile elements,
- microscopic inclusions,
- enrichment mechanism,
- sulfide,
- geochemistry

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References(55)

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Elemental Enrichment in the Microscopic Inclusions of the Native Sulfur from Kueishantao Hydrothermal System, Taiwan, China

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