Source and nature of ore-forming fluids of the Edmond hydrothermal field, Central Indian Ridge: evidence from He-Ar isotope composition and fluid inclusion study
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- 作者：Yejian Wang ; Xiqiu Han ; Zhongyan Qiu
- 关键词：Key wordsfluid inclusion ; helium and argon isotopes ; phase separation ; massive sulfides ; Central Indian Ridge
- 刊名：Acta Oceanologica Sinica
- 出版年：2017
- 出版时间：January 2017
- 年：2017
- 卷：36
- 期：1
- 页码：101-108
- 全文大小：
- 刊物主题：Oceanography; Climatology; Ecology; Engineering Fluid Dynamics; Marine & Freshwater Sciences; Environmental Chemistry;
- 出版者：The Chinese Society of Oceanography
- ISSN：1869-1099
- 卷排序：36
文摘
To understand the source and nature of the ore-forming fluids of the Edmond hydrothermal field on the Central Indian Ridge, we studied the He-Ar isotope composition and fluid inclusions of the hydrothermal precipitates. Our results show that the sulfide samples contain noble gases He, Ne, Kr, and Xe with their abundances in between those of air-saturated water (ASW) and mid-ocean ridge basalt (MORB). The 3He/4He ratio varies from 1.3 to 8.7 Ra (n=10, average: 5.1 Ra), whereas the 40Ar/36Ar ratio is from 285.3 to 314.7 (n=10, average: 294.8). These results suggest that the He was derived from a mixture of MORB with variable amounts of seawater, but the Ar in the ore-forming fluids trapped in the sulfides is predominantly derived from seawater. The fluid inclusions of barite have a wide range of homogenization temperatures and salinities varying from 163°C to 260°C and 2.6 wt% to 8.5 wt% NaCl equiv., respectively. It is suggested that the ore-forming fluids were produced by phase separation, which agreed with the present-day vent fluid study.