TY - JOUR TI - Geochemistry, sulfur and lead isotopic composition of hydrothermal sulfide from the Duanqiao hydrothermal field on the Southwest Indian Ridge: implications for ore genesis AU - Yang, Weifang AU - Liao, Shili AU - Alveirinho Dias, Ágata AU - Liang, Jin AU - Li, Wei AU - Ding, Teng AU - Tao, Chunhui T2 - International Geology Review AB - 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 δ34S 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 δ34S 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. DA - 2022/05/31/ PY - 2022 DO - 10.1080/00206814.2022.2081937 DP - Taylor and Francis+NEJM VL - 0 IS - 0 SP - 1 EP - 17 SN - 0020-6814 ST - Geochemistry, sulfur and lead isotopic composition of hydrothermal sulfide from the Duanqiao hydrothermal field on the Southwest Indian Ridge UR - https://doi.org/10.1080/00206814.2022.2081937 Y2 - 2022/09/21/13:41:13 KW - Hydrothermal sulfide KW - geochemistry KW - southwest Indian ridge KW - sulfur isotope KW - zone refining ER - TY - JOUR TI - Occurrence and precipitation mechanism of silver in pyrite from chimney fragments in the Edmond hydrothermal field, Central Indian Ridge AU - Zhang, Huichao AU - Chen, Kean AU - Tao, Chunhui AU - Alveirinho Dias, Ágata AU - Liang, Jin AU - Yang, Weifang AU - Liao, Shili AU - An, Fang AU - Yin, Bohao AU - Sun, Chuanqiang T2 - Ore Geology Reviews DA - 2023/05// PY - 2023 DO - 10.1016/j.oregeorev.2023.105471 DP - DOI.org (Crossref) SP - 105471 J2 - Ore Geology Reviews LA - en SN - 01691368 UR - https://linkinghub.elsevier.com/retrieve/pii/S0169136823001865 Y2 - 2023/05/10/03:57:57 ER -