The Sr–He–Ar isotopic and elemental evidence constraints on the ore genesis of the Zhaxikang Sb–Pb–Zn–Ag deposit in southern Tibet

Abstract

The genesis of Zhaxikang deposit is still debated, and three main geological environments have been proposed to model the mineralization: hot spring, magmatic hydrothermal fluid, and sedimentary exhalative (SEDEX) overprinted by hydrothermal fluid. This study presents elemental and Sr–He–Ar isotopic data of minerals from different mineralization stages to support the genetic model of earlier submarine hydrothermal sedimentation (metasomatism) metallogenesis superimposed by a later magmatic‐hydrothermal fluid. The linear relations between 1/Sr and 87Sr/86Sr ratios, Sr isotopic two‐component mixing model and elemental characteristics for Mn–Fe carbonate (87Sr/86Sr ratios: 0.713135–0.720277, Sr concentrations: 0.72–6.05 ppm) and calcite (87Sr/86Sr ratios: 0.707953–0.716116, Sr concentrations: 177–1,194 ppm) imply that the first episode of mineralization relates to a seafloor hydrothermal fluid and the second episode of mineralization is associated with a magmatic hydrothermal fluid. Furthermore, noticeable different He–Ar isotopic characteristics of the two episodes of mineralization (the first episode: 40Ar/4He: 0.06–0.27, 40Ar/36Ar: 288.9–1483.4, 38Ar/36Ar: 0.16–0.22, 3He/4He: 0.04–0.08Ra; the second episode: 40Ar/4He: 0.23–211.76, 40Ar/36Ar: 831.5–10047, 38Ar/36Ar: 0.17–0.25, 3He/4He: 0.04–1.31Ra) indicate that both these two episodes of ore‐forming fluids are mainly crustal‐derived with a more possibly magmatic hydrothermal origin for the second episode. Overall, the elemental and Sr–He–Ar isotopic data demonstrate the existence of two episodes of mineralization in which the initial submarine hydrothermal sedimentation (metasomatism) metallogenesis was overprinted by a later magmatic hydrothermal fluid.

Genesis of the Abunabu antimony deposits in the Tethys Himalayan metallogenic belt: Evidence from He–Ar and S isotopes of stibnite

“…The Tethys Himalayan lead-zinc-antimony polymetallic metallogenic belt is located in southern Tibet and consists of various types of Cenozoic polymetallic deposit, such as antimony, antimony-gold, gold, lead-zinc, and lead-zinc-antimony deposits. Major deposits include the Cheqiongzhuobu antimony, Abunabu antimony, Mazhala antimony-gold, Chapula gold, Jisong lead-zinc, and Zhaxikang lead-zinc-antimony polymetallic deposits (Yang et al, 2006;Zheng et al, 2014;Sun et al, 2016;Sun et al, 2018;Zhai et al, 2018;Cao et al, 2019;Wang et al, 2020;. Although no copper or molybdenum deposits have been discovered in this metallogenic belt, rare-metal (such as tungsten, tin, beryllium, and rubidium) ore deposits have been discovered (Li et al, 2017;Liang et al, 2018;Cao et al, 2021).…”