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New insights into the evolution of Mississippi Valley-Type hydrothermal system: A case study of the Wusihe Pb-Zn deposit, South China, using quartz in-situ trace elements and sulfides in situ S-Pb isotopes

  • Kai Luo , Jia-Xi Zhou EMAIL logo , Zhi-Long Huang , John Caulfield , Jian-Xin Zhao , Yue-Xing Feng and Hegen Ouyang
Published/Copyright: December 30, 2019
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Abstract

Unraveling the evolution of Mississippi Valley-type (MVT) hydrothermal system is crucial for understanding ore genesis and exploration. In this paper, we take the Wusihe Pb-Zn deposit in the western Yangtze Block (South China) as a case study, using detailed ore deposit geology, quartz in situ trace elements, and sulfides in situ S-Pb isotopes, to propose a new integrated model for the evolution of MVT hydrothermal system. Four hydrothermal stages were identified in the Wusihe ore district: (I) lamellar pyrite-sphalerite; (II) disseminated, stock-work, and brecciated sphalerite-galena; (III) massive galena, and (IV) veined calcite-bitumen. Within the most representative stage (stage II), Al concentrations in quartz (Q) increase from 8.46–354 ppm (mean 134 ppm) of Q1 to 171–3049 ppm (mean 1062 ppm) of Q2, and then decrease to 3.18–149 ppm (mean 25.4 ppm) of Q3. This trend indicates the role of acid-producing processes that resulted from sulfide precipitation and acid consumption by carbonate buffering. The occurrence of authigenic non-altered K-feldspar provides further evidence that the ore-forming fluids were weakly acidic with pH values of > ~5.5. Moreover, new bulk δ34S values of sulfides (+1.8 to +14.3‰) are overall lower than those previously reported (+7.1 to +20.9‰), implying that in addition to thermochemical sulfate reduction (TSR), bacterial sulfate reduction (BSR) may play an important role in the formation of S2–. In situ δ34S values show a larger range (–4.3 to +26.6‰), and significantly, varies within single grains (up to +12.3‰), suggesting mixing of two isotopically distinct S2– end-members produced by TSR and BSR. The diagenetic and hydrothermal early phase (stage I) sulfides were formed within a nearly closed system of BSR, whereas the formation of late phase (stage II and stage III) sulfides was caused by the input of hydrothermal fluids that promoted TSR. New galena in situ Pb isotopic ratios (206Pb/204Pb = 18.02–18.19, 207Pb/204Pb = 15.66–15.69, and 208Pb/204Pb = 38.14–38.39) suggest that the sources of mineralizing metals in the Wusihe deposit are mainly Proterozoic basement rocks. Hence, a multi-process model (i.e., basin-mountain coupling, fluid mixing, local sulfate reduction, in situ acid-producing and involvement of black shales and carbonate sequences) was responsible for the formation of the Wusihe deposit, while S2– was produced by both TSR and BSR, providing new insights into the evolution of MVT hydrothermal system.

Acknowledgments

We thank Wei Zhou, Gang Xia (The University of Queensland, Australia), En-Tao Liu (China University of Geosciences, Wuhan, China), Tai-Yi Luo, Jun Chen, and Zhen-li Li (Institute of Geochemistry, Chinese Academy of Sciences, China) for fruitful discussions. Comments and suggestions from Fang-Zhen Teng (Associate Editor), Martin Appold, David Huston, and an anonymous reviewer greatly improved the quality of the paper.

  1. Funding

    This research was financially supported by National Natural Science Foundation of China (41872095 and 41430315), the National Key R&D Program of China (2017YFC0602502), and the Research Start-up Project for Introduced Talent of Yunnan University (YJRC4201804) and the Cultivation Project for Excellent Youth of National Natural Science Foundation of Yunnan University (2018YDJQ009) to J.-X. Zhou.

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Received: 2019-05-01
Accepted: 2019-08-25
Published Online: 2019-12-30
Published in Print: 2020-01-28

© 2020 Walter de Gruyter GmbH, Berlin/Boston

Articles in the same Issue

  1. Highlights and Breakthroughs
  2. Regolith-hosted rare-earth elements: The phyllosilicate connection
  3. MSA Centennial Review Paper
  4. Heirs of the revolution: X-ray diffraction and the birth of the Mineralogical Society of America
  5. Deep Earth carbon reactions through time and space
  6. Magmatic carbon outgassing and uptake of CO2 by alkaline waters
  7. New insights into the evolution of Mississippi Valley-Type hydrothermal system: A case study of the Wusihe Pb-Zn deposit, South China, using quartz in-situ trace elements and sulfides in situ S-Pb isotopes
  8. Celestine discovered in Hawaiian basalts
  9. Microstructural controls on the chemical heterogeneity of cassiterite revealed by cathodoluminescence and elemental X-ray mapping
  10. Hornblende as a tool for assessing mineral-melt equilibrium and recognition of crystal accumulation
  11. The role of clay minerals in formation of the regolith-hosted heavy rare earth element deposits
  12. The tetrahedrite group: Nomenclature and classification
  13. Caseyite, a new mineral containing a variant of the flat-Al13 polyoxometalate cation
  14. Incorporation of Mg in phase Egg, AlSiO3OH: Toward a new polymorph of phase H, MgSiH2O4, a carrier of water in the deep mantle
  15. Imaging trace-element zoning in pyroxenes using synchrotron XRF mapping with the Maia detector array: Benefit of low-incident energy
  16. Discussion
  17. “Kamchatite” diamond aggregate from northern Kamchatka, Russia: New find of diamond formed by gas phase condensation or chemical vapor deposition—Discussion
  18. Reply
  19. On “Kamchatite” diamond aggregate from northern Kamchatka, Russia: New find of CVD-formed diamond in nature—Reply to K.D. Litasov, T.B. Bekker, and H. Kagi
  20. Memorial of Enver Murad 1941–2019
  21. Errata
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