Geochemistry, sulfur and lead isotopic composition of hydrothermal sulfide from the Duanqiao hydrothermal field on the Southwest Indian Ridge: implications for ore genesis

• Published in: International geology review Vol. 65; no. 6; pp. 883 - 899
• Main Authors: Yang, Weifang, Liao, Shili, Alveirinho Dias, Ágata, Liang, Jin, Li, Wei, Ding, Teng, Tao, Chunhui
• Format: Journal Article
• Language: English
• Published: Philadelphia Taylor & Francis 26.03.2023; Taylor & Francis Ltd
• Subjects: Basalt; Chalcopyrite; Chemical composition; Composition; Copper; Geochemistry; Heavy metals; Hydrothermal activity; Hydrothermal fields; Hydrothermal sulfide; Lava; Lead; Magma; Magma chambers; Metallogenesis; Metals; Mid-ocean ridges; Mineral deposits; Oceanic crust; Pyrite; Ridges; Sediment; southwest Indian ridge; Sphalerite; Spreading; Spreading centres; Sulfide; Sulfides; Sulfur; sulfur isotope; Sulphides; Sulphur; Zincblende; Zonation; Zone melting; zone refining
• ISSN: 0020-6814; 1938-2839
• DOI: 10.1080/00206814.2022.2081937

Hydrothermal activities on ultraslow-spreading ridges exhibit diverse characteristics, long histories with multiple participants, and might form large-scale, high-grade sulfide deposits. The Duanqiao hydrothermal field (DHF) is located at the segment with the thickest oceanic crust and a large axial magma chamber on the Southwest Indian Ridge, providing unique perspective of sulfide metallogenesis on ultraslow-spreading ridges. Previous studies revealed that DHF sulfide exhibits distinct features of enrichment of ore-forming elements in comparison with those of hydrothermal fields on sediment-starved mid-ocean ridges. However, the genesis and processes responsible for such differences remain poorly constrained. In this study, mineralogical, geochemical and S and Pb isotopic analyses were performed on relict sulfide mound samples to characterize DHF formation. The samples show clear concentric mineral zonation from the interior to the exterior wall. Assemblages of chalcopyrite, sphalerite, and pyrite are distributed mainly in the interior wall, whereas pyrite and marcasite are distributed mainly in the exterior wall. The low Cu content and Pb isotopic composition of the sulfide indicate that the metals are derived mainly from basement basalts. The δ 34 S values exhibit positive values distributed over a reasonably narrow range (2.42‰-7.97‰), which suggests approximately 62.1%-88.5% of S with basaltic origin. Compared with most hydrothermal fields along the sediment starved mid-ocean ridges, the DHF sulfide shows particularly high contents of Pb (263-2630 ppm), As (234-726 ppm), Sb (7.32-44.3 ppm), and Ag (35.2 to >100 ppm). The δ 34 S values exhibit an increasing tendency from the sample exterior to the interior. We propose that these features probably reflect the existence of a subsurface zone refining process. Our results provide new insight into the sulfide formation process and contribute to understanding the metallogenic mechanism of hydrothermal sulfides on ultraslow-spreading ridges.