Source and nature of ore-forming fluids of the Edmond hydro thermal field, Central Indian Ridge: evidence from He-Ar isotope composition and fluid inclusion study

作者：Wang Yejian; Han Xiqiu^*; Qiu Zhongyan

来源：Acta Oceanologica Sinica, 2017, 36(1): 101-108.

DOI：10.1007/s13131-016-0963-1

• fluid inclusion
• helium and argon isotopes
• phase separation
• massive sulfides
• Central Indian Ridge

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 He-3/He-4 ratio varies from 1.3 to 8.7 R-a (n=10, average: 5.1 R-a), whereas the Ar-40/Ar-36 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 degrees C to 260 degrees 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.

• 出版日期2017-1
• 单位国家海洋局第二海洋研究所