Yu, JunyuJunyuYuTao, ChunhuiChunhuiTaoLiao, ShiliShiliLiaoDias, ÁgataÁgataDiasLiang, JinJinLiangYang, WeifangWeifangYangZhu, ChuanweiChuanweiZhu2024-04-022024-04-0220210169-1368https://dspace.usj.edu.mo/handle/123456789/491510.1016/j.oregeorev.2021.104169Seafloor massive sulfide (SMS) deposits are important deep-sea mineral resources expected to occur predominantly on slow- and ultraslow-spreading mid-ocean ridges. Resource estimates are already available for some of the largest SMS deposits on slow-spreading ridges but not on ultraslow-spreading ridges. Based on geological mapping and sampling, this study investigates the distribution and content of sulfide-rich deposits in the Yuhuang-1 hydrothermal field (YHF), located on the ultraslow-spreading Southwest Indian Ridge. The sulfide-rich deposits in the YHF are composed of two areas _500 m apart: the southwest sulfide area (SWS) and the northeast sulfide area (NES). We calculated the volume of sulfide-rich mounds in the YHF and arrived at a total accumulation of _10.6 _ 106 tons, including at least _7.5 _ 105 tons of copper and zinc and _18 tons of gold. Furthermore, considering the coverage of layered hydrothermal sediment mixed with sulfide-rich breccias, which may have underlying massive sulfide deposits, the maximum total mass was estimated at _45.1 _ 106 tons. This suggests that the YHF is one of the largest SMS deposits worldwide and confirm that ultraslow-spreading ridges have the greatest potential to form large-scale SMS deposits.enResource estimateSeafloor massive sulfide depositsSouthwest Indian RidgeYuhuang-1 hydrothermal fieldtext::journal::journal article